eighth & ninth year assessment report on...

EIGHTH & NINTH YEAR ASSESSMENT REPORT ON MINERAL EXPLORATION ON THE ROCKY BROOK JOINT VENTURE, MINERAL

LICENSES 007897M & 016221M, DEER LAKE AREA, WESTERN NEWFOUNDLAND, NTS SHEETS 12H06.

for

Altius Resources Inc. Suite 202, 66 Kenmount Road,

St. John’s, NL, A1B 3V7

&

JNR Resources Inc. Suite 204, 315 - 22nd Street East, Saskatoon, SK, S7K OG6

by

Andrea Devereaux, Dale O’Reilly & Rod Churchill, P.Geo.

ALTIUS RESOURCES INC. &

J. Geoffrey Thurlow, P.Geo. VMS CONSULTANTS INC.

JANUARY 2010

…i

SUMMARY This report presents the technical results from the 2009 “Rocky Brook Project”, an earn-in/joint venture mineral exploration project being conducted in the Deer Lake Basin in western Newfoundland by JNR Resources Inc. and Altius Resources Inc. The 2009 field season marked the fifth year of exploration under this joint venture agreement. The purpose of the program was to locate the bedrock source(s) of high-grade uranium-silver-bearing boulders discovered by Westfield Minerals in 1978 – 1980. The 2009 exploration program included a diamond drilling campaign that consisted of 1,958.2 metres of drilling in 38 new drill holes and an environmental assessment that included the backfilling of the 2007 Wigwam Brook trench. The drill program was designed to test geological and IP/Resistivity targets highlighted during the 2008 exploration program. Digital borehole radiometric data was collected upon completion of all drill holes with the exception of one (a result of down-hole obstruction). In addition, lithogeochemical and assay samples were collected and shipped to the Saskatchewan Research Council for analyses. JNR Resources also completed PIMA analyses on the samples prior to being sent for assay. The purpose of the environmental assessment was to determine the amount of natural regeneration since the previous drilling campaign (2007) and to determine where future reclamation will be required. While the 2009 exploration program identified new areas of uranium mineralization, the source of the high-grade boulders has not yet been defined. Detailed correlations of the 2009 drill holes will be completed in the near future at which point they will be incorporated into the ongoing 3D Gocad model. This will undoubtedly further the understanding of the structure and stratigraphy of the geology at the Rocky Brook property.

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TABLE OF CONTENTS

SUMMARY ...................................................................................................................................... I

1.0 INTRODUCTION ........................................................................................................................ 1 1.1 Mineral Holdings ............................................................................................................................ 1 1.2 Location, Access, Infrastructure & Physiography .......................................................................... 4 1.3 History & Previous Work ............................................................................................................... 4

2.0 GEOLOGY .................................................................................................................................. 8

2.1 Regional Geology ........................................................................................................................... 8 2.2 Property Geology ........................................................................................................................... 9

2.2.1 Deer Lake Group ..................................................................................................................................... 9 2.2.1.1 North Brook Formation ..................................................................................................................................... 9 2.2.1.2 Rocky Brook Formation ..................................................................................................................................... 9 2.2.1.3 Humber Falls Formation .................................................................................................................................... 9

2.2.2 Structure of the Deer Lake Group ........................................................................................................ 13 2.2.3 Stratigraphy of the Humber Falls Formation ........................................................................................ 13

2.2.3.1 Lower Sandstone (Sl) ....................................................................................................................................... 14 2.2.3.2 Lower Mudstone (Ml) ...................................................................................................................................... 14 2.2.3.3 Middle Sandstone (Sm).................................................................................................................................... 14 2.2.3.4 Middle Mudstone (Mm) .................................................................................................................................. 15 2.2.3.5 Trashy Sandstone (St) ...................................................................................................................................... 15 2.2.3.6 Upper Mudstone (Mu) ..................................................................................................................................... 16 2.2.3.7 Upper Sandstone (Su) ...................................................................................................................................... 16

3.0 2009 EXPLORATION PROGRAM .............................................................................................. 16 3.1 Work Completed & Methodology ............................................................................................... 16 3.2 Diamond Drilling .......................................................................................................................... 17

3.2.1 Introduction .......................................................................................................................................... 17 3.2.2 Drill Core Sampling ............................................................................................................................... 18 3.2.3 Observations on Field Aspects of the Diamond Drill Program ............................................................. 19 3.2.4 Drilling Results ...................................................................................................................................... 19

3.2.4.1 Wigwam Brook Area ........................................................................................................................................ 19 3.2.4.2 Goose Anomaly Area ....................................................................................................................................... 22 3.2.4.3 Birchy Hill Brook Area ...................................................................................................................................... 23

3.3 Environmental Assessment Program ........................................................................................... 26

4.0 CONCLUSIONS & RECOMMENDATIONS .................................................................................. 26

5.0 ACKNOWLEDGEMENTS ........................................................................................................... 27

6.0 BIBLIOGRAPHY & REFERENCES ............................................................................................... 28

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APPENDIX 1. LIST OF CONTRACTORS & PERSONNEL; STATEMENT OF EXPENDITURES .................... 1 APPENDIX 2. DIAMOND DRILL HOLE DATABASE ............................................................................. 2 APPENDIX 3. DIAMOND DRILL LOGS ............................................................................................... 3 APPENDIX 4. BOREHOLE RADIOMETRIC PROBE SPECIFICATIONS .................................................... 4 APPENDIX 5: CROSS-SECTIONS ....................................................................................................... 5 APPENDIX 6: 2009 FIVE-METRE SYSTEMATIC DRILL CORE SAMPLING ............................................. 6 APPENDIX 7: 2009 DRILL CORE INTERVAL SAMPLING ..................................................................... 7 APPENDIX 8: 2009 LABORATORY ASSAY CERTIFICATES ................................................................... 8 APPENDIX 9: 2009 PORTABLE INFRARED MINERAL ANALYSER (PIMA) RESULTS ............................. 9 APPENDIX 10: ENVIRONMENTAL ASSESSMENT REPORT ............................................................... 10

LIST OF TABLES Table 1. Listing of Current Mineral License Details, Rocky Brook Property .................................................. 1 Table 2. Selected Boulder Assays, Westfield Trenches ................................................................................. 5 Table 3. Anomalous Assay and Probe Results from RB-09-229, Wigwam Brook Area .............................. 20 Table 4. Anomalous Assay and Probe Results for Drillholes RB-09-232 and 245, Goose Anomaly Area .. 23 Table 5. Uranium Assay Results for Drillholes RB-09-248, 251 and 256 – 258 .......................................... 25

LIST OF FIGURES Figure 1. Tectonostratigraphic Setting .......................................................................................................................... 2 Figure 2. Claims Location map ....................................................................................................................................... 3 Figure 3. Regional Geological Setting .......................................................................................................................... 10 Figure 4. Geology of the Humber Falls Formation ....................................................................................................... 11 Figure 5. Schematic Stratigraphy of the Deer Lake Basin (after Hyde et al., 1988) ..................................................... 12

MAP POCKET

Map No. Description

Scale

01 Wigwam & Goose Areas; Drill Collar Locations 1:2,000 02 Birchy Hill Brook Area; Drill Collar Locations 1:1,250

This report and the information presented/described herein is also submitted in digital format and found on the disk located in the front of this report.

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1.0 INTRODUCTION This report presents the results from the 2009 field season, the fifth year of a joint venture agreement between Altius Resources Inc. and JNR Resources Inc. The program included a diamond drilling campaign consisting of 1,958.2 metres of drilling in 38 new diamond drill holes and an environmental assessment which included the backfilling of a trench that was excavated in 2007. Exploration in the Deer Lake Basin has been ongoing since the mid 1970’s and has largely been for uranium, although base metals have also been targeted intermittently. Altius - JNR exploration programs are largely based on discovering the source(s) of high-grade uranium-silver-bearing boulders discovered by Westfield Minerals in 1978 – 1980. The purpose of the 2009 exploration program was to test areas highlighted by the 2008 exploration program in particular geochemical (water), geophysical (chargeability/resistivity) and geological targets.

1.1 Mineral Holdings Altius negotiated an option to acquire the rights to mineral license 007897M from prospector Paul Crocker in 2001 and have since added to the land position by staking additional, contiguous claims. Altius, in turn, reached an agreement with JNR whereby JNR could earn an interest in all of these claims (collectively the “Rocky Brook Project”) by conducting mineral exploration and making payments to Altius. As of 2009, JNR have successfully completed their earn-in requirements and are the majority owners of the property. In May 2009, Altius and JNR completed a series of reductions and groupings on the Rocky Brook property resulting in the current property configuration of two licenses, totalling 258 claims, covering the most prospective geology. Former licenses 010141M (90 claims) and 016050M (108 claims) were grouped and issued the new mineral license number of 016221M. In addition, licenses 016051M (31 claims) and 016052M (8 claims) were surrendered to the Crown. The following table provides the details pertaining to the mineral holdings and the location of the claims is shown on Figures 1 and 2.

Table 1. Listing of Current Mineral License Details, Rocky Brook Property

License Number

Issuance Date Number of

Claims Work Due Date Work Required ($)

007897M 19-Feb-2001 60 19-Feb-2019 72,000.00

016221M 21-Sept-2001 198 21-Sept-2011 47,787.16

TOTALS 258 119,787.16

Notre Dame Bay

CornerBrookCornerBrookCornerBrook

St. John'sSt. John's

BaieVerteBaieVerteBaieVerte

GanderGanderD

over

Fault

Cape Ray Fault

Long

Range

Fault

BaieVerteLine

GR

UB

Lin

e

GR

UB

Lin

e

Hermitage Bay Fault

LineLine

India

n

India

n

RedRedBuchansBuchans

AVALONZONE

AVALONZONE

AVALONZONE

DUNNAGE ZONE

BOTWOOD BASIN

BOTWOOD BASIN

GANDERZONE

NotreDam

eSubzo

ne

NotreDam

eSubzo

neExplo

its S

ubzone

Exploits

Subzo

ne

Meelpaeg Subzone

Meelpaeg Subzone

Mt. C

orm

ack

Subzo

ne

Mt. C

orm

ack

Subzo

ne

Mt. C

orm

ack

Subzo

ne G

ander

Lak

eSubzo

ne

Gan

der

Lak

eSubzo

ne

HUMBERZONE

HUMBERZONE

HUMBERZONE

Precambrian crystalline, Laurentian basement overlain by youngershelf-facies rocks and allochthonous oceanic sedimentary/ophioliticrocks.

NOTRE DAME SUBZONE: dominantly Cambrian to MiddleOrdovician submarine volcanic rocks and ophiolitic suitesunconformably overlain by non-marine Silurian overlap sequences.

EXPLOITS SUBZONE: dominantly Cambrian to Mid-Ordovicianoceanic sedimentary rocks with intercalated volcanic rocks overlainby Mid- to Late Ordovician black shales that pass conformablyinto turbidite deposits that in turn pass into shallow marine andnon-marine Silurian strata.

Cambro-Ordovician, variably metamorphosed, quartz-richsiliciclastic rocks of continental slope origin (GANDER LAKESUBZONE) and inferred structral windows through the DunnageZone (MOUNT CORMACK AND MEELPAEG SUBZONES).

Late Proterozoic submarine and terrestrial volcanic rocks andturbiditic, deltaic and fluviatile sedimentary rocks unconformablyoverlain by a younger shallow marine succession having distinctiveAcado-Baltic faunal assemblages.

HUMBER ZONE

TECTONOSTRATIGRAPHIC ZONATIONS

DUNNAGE ZONE

GANDER ZONE

AVALON ZONE

Rocks of ophiolitic affinity - may include mafic intrusiveand extrusive rocks as well as ultramafic lithologies

Post-Ordovician intrusive rocks including felsic and maficintrusive lithologies

Post-Ordovician overlap sequences including shallowmarine and non-marine sedimentary and volcanic rocks

Regional scale fault and shear systems that delineateboundaries between adjacent tectonostratigraphic zones

MAJOR GEOLOGICAL ELEMENTS

48

°00

'N5

0°0

0'N

59°00'W 57°00'W 55°00'W 53°00'W

0 25 50

Kilometers

75 100

ROCKYBROOKROCKYBROOKROCKYBROOK

ROCKY BROOK PROPERTYTectonostratigraphic Setting

Date Printed:

Revised By:

Drawn By:

15-Jan-2010

A. Devereaux

R. Churchill

NTS:

UTM:

Scale:

Figure No:

NAD 27, Zone 21

As Shown

1

Filename: Figure_01.cdr

12H/06, 07, 10, 11

License(s)

007897M & 016221M

500000mE495000mE

5465000m

N5470000m

N5475000m

N

490000mE

5480000m

N5485000m

N5490000m

N

016221M

007897M

Sandy

Lake

Birchy

Lake

Upp

er

Hum

ber

River

Adi

es

Riv

er

Alder

Pond

LEGEND

Streams

Woods Roads and Trails

Contours

Trans Canada Highway

Altius Claims

Wetlands

ROCKY BROOK PROPERTYClaims Location Map

Date Printed:

Revised By:

Drawn By:

D. O’Reilly

R. Churchill

NTS:

UTM:

Scale:

Figure No:

NAD 27, Zone 21

As Shown

2


12H/06, 07, 10, 11

0 1 2 3 4

kilometres

5

15-Jan-2010

License(s)007897M &

016221M

…4

1.2 Location, Access, Infrastructure & Physiography The property is located in western Newfoundland (Figure 1), generally between the towns of Deer Lake (pop. approx. 5,000) and Hampden. The claims are 5 to 10 kilometres northwest of the Trans-Canada Highway (TCH) and are accessible by a number of secondary woods roads emanating from the TCH. The Town of Deer Lake is at the juncture of the Viking Trail and the TCH and has a modern airport. Topographically, the claim group can be divided into two areas separated by the Wigwam Fault; (a) a low, flat, boggy, prospective terrane, and (b) an “upland” area along the eastern margin of the claim group. Vegetation within the prospective area consists of abundant alders and patches of stunted black spruce, birch and fir within larger areas of open bog with scattered ponds whereas the upland area is characterized by denser forest with local harvested areas. The Humber River, a major western Newfoundland watercourse, flows southwest through the area. Outcrop is rare within the prospective low country.

1.3 History & Previous Work Several companies have explored the property extensively since the mid 1970’s and this work has been documented on several occasions, including by Giggie, (1991) from which parts of this account are paraphrased directly. The focus of the mineral exploration effort has changed from base metals in the early days (1974 – 1976) to uranium (1976 – 1982) to precious metals (1983, 1988) and recently to uranium again. The property was originally staked in 1974 by Westfield Minerals Ltd. as part of a regional base metal exploration program in the Deer Lake Basin. Knight, (1976) reported above background scintillometer readings from Carboniferous rocks of the St. George’s Basin. Urangesellschaft, apparently acting on the Knight report, investigated the Deer Lake Basin in 1976 but found only minor radioactive occurrences (Curtis, 1976). Westfield conducted reconnaissance geochemical and radiometric surveys in 1978 on parts of both the St. George’s and Deer Lake Basins that resulted in the discovery of radioactive sandstone boulders in the bed of Wigwam Brook. A hand-dug pit on the bank of the brook exposed boulders with assays of up to 11.5% U3O8. “Subsequent trenching revealed highly radioactive zones in the bedrock” (Byrne, 1978) and though channel sampling revealed only trace mineralization, one grab sample returned an assay of 1.28% U3O8. Twenty-one diamond drill holes were drilled and “although no anomalously radioactive core was recovered, radiometric borehole logging showed that the drill passed through or close to moderately radioactive zones in the 5 to 15 ft. depth range where core recovery was generally poor” (Byrne, 1979). Westfield apparently sought joint venture partners for the property at this time. Northgate Exploration Ltd. and Shell Canada Resources Ltd. joined forces with Westfield during 1980 and 1981 and a massive exploration program was executed at which time approximately $6,000,000 was expended. Work included extensive prospecting, till and soil geochemistry, geology, trenching and more than 150 diamond drill holes, most with downhole radiometric

…5

surveys and assays. Several consultants were engaged for advice on various aspects of the exploration program; among these, Dr. R. Rogerson was especially influential in proposing glacial transport from the southeast to the northwest. Shell withdrew from the joint venture at the end of 1981 with the demise of their minerals division. However, Westfield attracted Chutine Resources and carried on in 1982 with the focus shifted to silver, a result of “very high silver values found in uraniferous boulders late in the preceding year” (Wilkinson, 1983). A small amount of basal till sampling was carried out which also failed to locate the source of the U-Ag boulders and Westfield dropped the claims in 1984. Government geologist Richard Hyde conducted regional geological mapping of the Deer Lake Basin during the Westfield campaigns and his 1982 map (Map 82-7) at 1:100,000 scale remains to this day as the most authoritative regional map. The property remained open for staking until 1988 when INCO conducted reconnaissance sampling of some of the Westfield boulder fields and obtained the following assays:

Table 2. Selected Boulder Assays, Westfield Trenches

Boulder Field g/T Au g/T Ag

Birchy Hill Brook 17.8 788.4

Wigwam Brook -- 1953.5

Goose -- 240.0

INCO staked 452 claims in 1988, re-assayed Westfield core, cut four small grids and drilled 24 short diamond drill holes around the Birchy Hill Brook trenches. Drilling was largely conducted in what was believed to be an up-ice (southwest) direction from the boulder field. No anomalous core was recovered and the best assays returned from boulders at the Birchy Hill Brook trenches were 3.05 g/T Au, 209.1 g/T Ag and 630 ppm Pb (Vidito, 1989). INCO apparently assayed a uraniferous boulder, which ran 17.8 g/T Au, however, this was not reported by INCO, but by Giggie, (1991). During 1990, NovaGold Resources Inc. focused efforts on the relatively less explored area of the Wigwam Fault, southeast of the Wigwam and Goose boulder fields (Giggie, 1991). Linecutting, soil geochemistry (n = 268), fourteen test pits dug on soil anomalies, 15 basal till samples and 11 boulders were assayed. Further work was not recommended and the claims were allowed to lapse.

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Plains Exploration conducted exploration on claims registered to A.B. Baldwin, again with emphasis on the Wigwam Fault (Baldwin, 1996, 1997). Linecutting, VLF-EM, magnetics and induced polarization were carried out during 1996 and 6 BQ diamond drill holes totaling 1,123.2 metres were drilled in 1997. No new mineralization was encountered. Interestingly, Baldwin reports an assay of 11.76 oz./t Au from a mineralized boulder assayed (but not reported?) during the Shell era. Batterson and Taylor, (1994) conducted till mapping in the Deer Lake Basin and concluded, contrary to most previous workers, that glacial transport in the vicinity of the boulder fields was from northeast to southwest. This observation was a key factor in piquing Altius’ interest in the property. Altius Resources conducted minor prospecting, trenching, sampling and compilation of data (Churchill et al., 2002) prior to the formation of a joint venture with Cameco Corporation in 2002. Altius and Cameco conducted an exploration program in 2002 which included a three-axis gradient airborne magnetic survey and related interpretation, acquisition and interpretation of existing radar and radiometric data sets, a program of lithogeochemical and PIMA analysis of existing diamond drill core, stratigraphic definition and correlation within the Humber Falls Formation, prospecting, orientation till pitting with geochemical analyses and petrographic work on mineralized boulder samples (Thurlow, 2003). During 2003, Altius and Cameco cut 60 kilometres of line and conducted ground magnetics and VLF-EM surveys, ground prospecting of airborne radiometric anomalies and completed a 96-hole sonic drilling program. Eight of the sonic holes were converted to diamond drill holes upon reaching bedrock. Borehole radiometric surveys conducted within the newly drilled holes suggested that the Birchy Hill Brook boulder field forms part of a much larger train of radioactive till which does not emanate from the immediate vicinity of the anomalous trenches. Cameco abandoned their interest in the property in 2004 and JNR Resources were attracted to the project late in the same year. An extensive diamond drilling program was completed on the Rocky Brook Project in 2005 by Altius and JNR. The exploration program comprised 3,265.1 metres of drilling in 78 new BTW (BQTK) diamond drill holes. Digital borehole radiometric data was collected upon completion of all holes with the exception of one. In addition, lithogeochemical, assay and PIMA samples were collected and analysed. Drilling in the south was mainly designed to test the contact between hematitized and reduced sandstone members however some drill holes did test up-ice of the Wigwam Brook boulder field. Drilling in the vicinity of the Birchy Hill Brook boulder field was designed to test the northern extents of the dispersal train of radioactive till that was proposed after the 2003 sonic drilling program.

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Altius and JNR continued to explore the Deer Lake Basin in 2006. The exploration program included an airborne radiometric, magnetic and electromagnetic survey, radiometric prospecting of airborne anomalies and additional diamond drilling. The airborne survey, which was completed in the early summer of 2006, consisted of 1,250.3 line kilometres that were flown at 100 metre spacings. Several radiometric anomalies were generated from the survey and required further examination. A two-man crew, equipped with hand-held scintillometers and/or spectrometers, was employed to investigate the anomalies. The results from the prospecting program were less than encouraging, in part due to a lack of outcrop but mainly due to the majority of the anomalies being the result of radioactive till and/or boulders exposed at surface. A total of 65 new BTW (BQTK) diamond drill holes were completed in 2006, comprising 2,882.9 metres of drilling. Digital borehole radiometric data was collected upon completion of all holes and as well, in several historic drill holes completed by Westfield (O’Reilly et al., 2007). Drilling was largely designed to follow-up geophysical anomalies although minor geochemical anomalies, identified during previous programs, were further evaluated. Lithogeochemical, assay and PIMA samples (core, outcrop and float) were also collected and analysed. The 2007 exploration program on the Rocky Brook Project consisted of a high-resolution satellite imagery (Quickbird) survey, a differential GPS survey, trenching, petrography and a diamond drilling program. In addition to this work, consultation with respect to geochemical sampling in boggy terrain was also completed. A single trench was excavated in the Wigwam Brook area, and although radioactive bedrock was not encountered, historical reports of northwest striking bedding was confirmed. However, a review of geological cross-sections in area illustrate flat-lying geology suggesting the anomalous bedding angle is the result of cross-bedding. Four polished thin sections were prepared in order to describe and classify an unknown alteration species and a tectonized(?) mudstone (which closely resembles the high-grade boulders) encountered in drill core. A total of 2,482.2 metres of drilling in 82 new BTW (BQTK) diamond drill holes was also completed in 2007. The focus of the drill program was to follow-up geochemical and geophysical results from the 2005 and 2006 programs. Additional drilling in the Goose boulder field and the prospective Anomaly “H” areas was also completed as both areas had been insufficiently drilled (due to time constraints) during previous programs. Digital borehole radiometric data was collected upon completion of all but four holes (a result of both down-hole and technical difficulties) (O’Reilly et al., 2008). Lithogeochemical, assay and PIMA samples of core were also collected and analysed. JNR and Altius took a different approach for the 2008 exploration program in that the focus was on generating new targets for future drill programs. There has been an extensive volume of data collected over the previous programs (drilling, geochemistry and geophysics), but a thorough interpretation has always been lacking. As a result, a program consisting of a detailed geological re-evaluation was conducted. Detailed stratigraphic correlations were completed and a new model for the structure of the upper lobe of the Humber Falls Formation was

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proposed. High angle reverse faults, (subsidiary faulting related to the Wigwam Fault or Cabot Fault System), were introduced and several of these structures were recommended for drill testing. In addition to the geological re-evaluation, a regional water geochemical survey and an IP/Resistivity survey were also completed. The water sampling survey identified a total of ten exploration targets, three of which (Birchy Hill, Wigwam Brook and the Goose Anomaly) had been the focus of previous drilling campaigns. Seven new multi-element anomalies were also identified and were recommended for follow-up exploration. The induced polarization/resistivity survey was conducted in areas of known mineralization on the basis of delineating “chargeable” zones that had not been drill tested. Several areas of high chargeability (mineralization?) and/or high resistivity (alteration?) were identified and proposed as drill targets.

2.0 GEOLOGY 2.1 Regional Geology

The island of Newfoundland presents a cross-section through the northern portion of the Appalachian Orogen. Four major tectonostratigraphic zones, based upon pre-Carboniferous geology, have been identified and termed from west to east as the Humber, Dunnage, Gander and Avalon zones (Figure 1). These zones record the opening and closing of the Iapetus Ocean in the late Precambrian and early Paleozoic (Williams, 1979). The Humber Zone represents the continental margin of Laurentia and consists of Precambrian crystalline rocks overlain by Paleozoic shelf facies rocks while the Avalon Zone represents part of Gondwana and consists of late Precambrian plutonic, volcanic and sedimentary rocks overlain by Paleozoic platformal sedimentary units. The Gander Zone represents mainly sedimentary rocks believed to have been deposited near the eastern continental margin of the Iapetus Ocean. The Dunnage Zone represents the vestiges of the Iapetus Ocean. Rocks within this zone consist of volcanic and sedimentary rocks of back-arc and island-arc affinity and of ophiolitic rocks created during the opening and subsequent closure of Iapetus. The Dunnage Zone also includes post-accretion molasse sedimentation largely of Silurian age and a variety of intrusive rocks, largely of Devonian age. Following assembly of the Appalachian Orogen, transtensional stresses during the Carboniferous opened the marine St. George’s Bay Basin and lacustrine Deer Lake and Red Indian Lake Basins. The Deer Lake Basin formed along the Cabot Fault system, a major strike-slip structure that transects western Newfoundland. It was infilled with clastic sediments dominated by sandstone, siltstone and conglomerate, which were deposited upon basement rocks of the Grenville Province, Cambro-Ordovician carbonates as well as Siluro-Devonian volcanic and intrusive rocks. The Carboniferous strata were folded and faulted during ongoing strike-slip movements along faults of the Cabot Fault System. A geological map of the Deer Lake Basin at 1:100,000 scale by Hyde, (1982) represents the most recent published portrayal of

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the regional geology. Hyde et al., (1988, 1994) provide good overviews of the stratigraphy and structure of the basin.

2.2 Property Geology Simplified geological maps of the area of prime interest are presented in Figures 3 and 4, and a schematic section of the Deer Lake Basin is reproduced from Hyde et al., (1988) in Figure 5. The Carboniferous Deer Lake Group includes, in ascending order, the North Brook, Rocky Brook and Humber Falls formations in the Upper Humber River area. The Deer Lake Group is interpreted to unconformably overlie the early Carboniferous Anguille Group in this area. Also exposed at surface in the northwest corner of the claim group are Grenville basement rocks and overlying Paleozoic carbonate rocks (Figure 3). Along the eastern margin of the claim group, Silurian volcanic rocks (Sops Arm Group) and Devonian granites and gabbros of the Gull Lake Intrusive Suite (Saunders and Smyth, 1990) are in presumed fault contact with the Carboniferous sediments (Figure 3).

2.2.1 Deer Lake Group 2.2.1.1 North Brook Formation

The North Brook Formation consists of grey and red, pebble to boulder conglomerate, grey, orange and red sandstone, red siltstone, thin grey limestone beds and an amygdaloidal basalt flow. It is interpreted as representing alluvial fan deposition at basin margins, and braided- and meandering-river deposition on the alluvial-fan deposits. The North Brook Formation thickens southward where it has a maximum thickness of 1,300 metres.

2.2.1.2 Rocky Brook Formation The Rocky Brook Formation gradationally overlies the North Brook Formation and consists of the following rock types: red and grey siltstone and mudstone, dominantly fine-grained red sandstone, grey calcilutite and calcarenite, and dark brown oil shale. It was deposited in a fluvial environment at its base; shallow lacustrine deposition dominates the rest of the formation. The Rocky Brook Formation thickens southward, where it has a maximum thickness of 1,500 metres.

2.2.1.3 Humber Falls Formation The Humber Falls Formation consists of grey, pink and red arkose, arkosic granule to pebble conglomerate, thin red siltstone beds and reddish to brownish mudstone, overlying the Rocky Brook Formation. It is interpreted to represent fluviatile sandstone-conglomerate sedimentation with overbank floodplain deposition of siltstone (Hiscott, 1979). The sediments are thought to have been deposited from braided rivers within an alluvial fan.

Sandy

Lake

Birchy

Lake

Upp

er

Hum

ber

River

Adi

es

Riv

er

Alder

Pond

500000mE495000mE

5465000m

N5470000m

N5475000m

N

490000mE

5480000m

N5485000m

N5490000m

N

016221M

007897M

LEGEND

Carboniferous - Westphalian A

Howley Formation

Humber Falls Formation

Rocky Brook Formation

North Brook Formation

Saltwater Cove Formation

Geological Contacts

Wigwam Brook Formation(purple units are limestone)

Wigwam Fault

Faults (unspecified)

Carboniferous - Visean

Carboniferous - Tournaisian

Carboniferous - Tournaisian and older

DEER LAKE GROUP

ANGUILLE GROUP

PRE-CARBONIFEROUS BASEMENT

Devonian - Silurian (?)

Gull Lake Intrusive Suite(Granitic and gabbroic rocks)

Devonian (?) - Silurian

Sops Arm Group (Felsic tointermediate volcanic rocks)

Pre-Cambrian

Granitoid gneiss

Streams

Trans Canada Highway

Woods Roads and Trails

Altius Claims

Contours

Wetlands

Wild Cove Pond Intrusive Suite(Granitic and gabbroic rocks)

ROCKY BROOK PROPERTYRegional Geological Setting

Date Printed:

Revised By:

Drawn By:

15-Jan-2010

A. Devereaux

R. Churchill

NTS:

UTM:

Scale:

Figure No:

NAD 27, Zone 21

As Shown

3


12H/06, 07, 10, 11

License(s)007897M &

016221M

0 1 2 3 4

kilometres

5

Mm

RB

2,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0002,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,0001,000

metresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetresmetres

0000000000000000000000000000000000000000000000000

498,000 mE

496,000 mE494,000 mE

5,4

74

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494,000 mE492,000 mE 496,000 mE

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Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook Birchy Hill Brook

Boulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder FieldBoulder Field

Wigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam BrookWigwam Brook


Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose Goose


Figure Number:

Date Revised:

Geology By:

Drafted By:

Date Drafted:Area:

NTS Sheets:

Scale:

Filename:

Projection:

April 2009

Map_04_HF_Fm.wor

A. Devereaux

J.G. Thurlow

Geology of theHumber Falls Formation

UTM Zone 21 (NAD 27)

Upper Humber River Area

1/30,000

12H/06

04

January 2010

Middle Mudstone(Mm)

Middle Sandstone(Sm)

Lower Mudstone(Ml)

Lower Sandstone(Sl)

Trashy Sandstone(St)

Upper Mudstone(Mu)

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Reverse Fault

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Granite

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Upper Humber River

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PRE-CARBONIFEROUS BASEMENT

HUMBER RIVER AREA

Howley Fm

Rocky Brook Fm

Humber Falls Fm Little Pond Brook Fm

North Brook FmDE

ER

LA

KE

GR

OU

P

Gold CoveFm

CapeRouge Fm

Thirty - fifthBk Fm

Saltwater Cove Fm

AN

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E G

RO

UP

WigwamBrook Fm

BIRCHYRIDGEBLOCK

FISHERHILLS

BLOCK

WetstonePt Fm

Forty-fiveBk Fm

Blue GulchBk Fm

Westphalian A

Visean-

Namurian (?)

Visean

Visean (?)

Tournaisian

Devonian (?) - Tournaisian

W

SN

E

ROCKY BROOK PROPERTYSchematic Stratigraphy of the Deer Lake Basin

(after Hyde et. al., 1988)

Date Printed:

Revised By:

Drawn By:

15-Jan-2010

A. Devereaux

D. O’Reilly

NTS:

UTM:

Scale:

Figure No:

n/a

n/a

05


12H10 & 12H11

License(s)

007897M & 016221M

…13

The Humber Falls Formation sandstones in the project area are composed dominantly of quartz, plagioclase and K-feldspar generally with only minor lithic material. The sandstones are commonly quite coarse grained and grade into conglomerates composed dominantly of large crystal clasts of quartz and perthitic feldspar. A coarse-grained granitic rock is implied as the source of the bulk of the sandy material of the formation and rare granitic clasts have been observed. Conglomerates at the base of the formation contain a variety of lithic clasts including foliated volcanic rocks of presumed Silurian age. Some sandstone units are characterized by the presence of abundant fine to coarse-grained coalified wood trash with associated pyrite. Varying styles of hematite and lesser chlorite alteration are locally well developed. The maximum thickness of this formation is probably no more than several hundred metres. The Altius claim group was largely designed to cover the northern lobe of the Humber Falls Formation, structures bounding the Formation and some of the minor uranium occurrences outside the Formation.

2.2.2 Structure of the Deer Lake Group The Deer Lake Group rocks were originally interpreted to be gently folded into an open synclincal structure that is truncated along its eastern margin by the Wigwam Fault, a reverse fault that juxtaposes conglomerates of the Wigwam Brook Formation (and/or possibly the North Brook Formation?) against the Deer Lake Group (Figures 3 and 4). The Birchy Ridge Fault, in turn, juxtaposes Lower Carboniferous clastic sediments of the Anguille Group against the Wigwam Brook Formation. The Wigwam and Birchy Ridge Faults are members of a swarm of north-northeast striking structures that are thought to comprise components of a positive flower structure generated during transpressional tectonics along the Cabot Fault system. The Wigwam Fault appears to join with the Doucer’s Valley Fault Complex in White Bay. The numerous high-angle, secondary reverse faults, which have only recently been recognized, are interpreted to be related to the Wigwam Fault (or Cabot Fault System) and present a much more structurally complex model for the Deer Lake Group rocks in the Upper Humber River area (Thurlow, 2009).

2.2.3 Stratigraphy of the Humber Falls Formation A relatively consistent pattern of sandstone and mudstone units exists within the Humber Falls Formation and is especially evident in the Wigwam Brook area. A stratigraphic column was proposed by Thurlow, (2002) based upon logging of drill core from this area and this stratigraphy has been correlated progressively southward and northward to the limits of the historic and recent drilling. The stratigraphic members of the Humber Falls Formation, from bottom to top, are the Lower Sandstone (Sl), Lower Mudstone (Ml), Middle Sandstone (Sm), Middle Mudstone (Mm), Trashy Member (St), Upper Mudstone (Mu) and Upper Sandstone (Su). A geological map showing their distribution is given as Figure 4 and descriptions of the various units are provided below. Furthermore, Thurlow, (2009) identified further subdivisions within these members to facilitate more detailed stratigraphic correlation in certain areas.

…14

2.2.3.1 Lower Sandstone (Sl) This member is located at the base of the Humber Falls Formation where it overlies the Rocky Brook Formation with a sharp, well-defined contact. Westfield geologists have previously described the contact as sheared and Thurlow et al., (2006) have reported an instance of a gradational contact. The contact is primarily sharp and well-defined, although instances of gradation and faulting have also been observed locally. This lowermost member consists of tan-buff to reddish to greyish coloured, fine- to very coarse-grained sandstone and granule to pebble conglomerate. The rocks are dominantly comprised of quartz and K-feldspar grains with minor lithic fragments (more common in conglomerates). Thin, silty and clayey mudstone beds are locally present as well. The member is generally massive however some of the finer intervals do exhibit bedding. In addition, some of these finer intervals tend to be very micaceous. One characteristic of the Lower Sandstone Member that appeared to be similar throughout the basin is the presence of an impervious, pyrite-bearing conglomerate at its base; however this unique marker horizon was either absent, significantly thinner or interbedded/intermixed with mudstone, possibly belonging to the underlying Rocky Brook Formation, in several drill holes completed in 2007 and 2009. The basal conglomerate often contains carbonaceous material that may also contain sulphide mineralization though this is not characteristic. The member can be variably oxidized (more common in the southern portion of the property) though an entirely reduced member is not uncommon, as mainly seen in the north, near Birchy Hill Brook. Oxidation can be of several different types and is often very intense (complete replacement of host rock by hematite).

2.2.3.2 Lower Mudstone (Ml) This member overlies the Lower Sandstone Member with a gradational to sharp contact. It consists of reddish to greenish coloured, clayey mudstone with minor fine- to medium-grained sandstone intervals. The member is generally massive however bedding is exhibited within some of the sandstone intervals. The rocks are variably to strongly oxidized, and tend to be a redder colour than the other mudstone intervals within the Humber Falls Formation. In contrast, the member can also exhibit variable or strong reduction, with only remnants of hematite alteration remaining. Hematite – calcite nodules/concretions are locally common. Non-calcareous nodules (possibly felsic and/or phosphate in composition) tend to be less common. Furthermore, the mudstones often host minute nodules, which give the member a “vesicular-looking” texture. Carbonaceous material, though rare, can be present within the member. The organics, when present, tend to be restricted to the base of the member, near the contact with the Lower Sandstone Member.

2.2.3.3 Middle Sandstone (Sm) This unit overlies the Lower Mudstone Member with a sharp, often hematitized contact. The Middle Sandstone Member of the Humber Falls Formation consists of similar (colour, composition and grain size) sandstone and conglomerate intervals as the Lower Sandstone Member, though the thickness of this member is significantly greater than that of the lower

…15

one. This member also hosts smaller intervals of silty and clayey mudstone, that tend to be more abundant in the northern portion of the basin than the southern half. Due to the thickness of this member, instances of bedding are more frequent, especially in the finer grained sandstones. However, massive beds of sandstone, mudstone and conglomerate are not uncommon and other thick units display only weak stratification. Oxidation within the rocks is almost ubiquitous throughout the basin except in an area east-southeast of Wigwam Brook where the member tends to be unoxidized. Where unoxidized, the member contains more noticeable organic material and can be difficult to distinguish from the Trashy Member. Oxidation tends to be stronger on the upper half of the member and commonly decreases with depth. The type and intensity of hematite alteration varies greatly. It can range from a weak, fine-grained, disseminated hematite to an intense, complete replacement of the host rock by an oily, fracture-related hematite or by a stratigraphically controlled-type to name a few. In addition to oxidation, this unit can be significantly reduced. Reduction can be present in the form of spots, rings, haloes or complete beds within the member. Though not as widespread as oxidation, reduced sections are very common in the Middle Sandstone Member. Organic material +/- sulphide mineralization (pyrite, oxidized Cu minerals) and hematitization is evident within this member but tends to be rare. The Middle Sandstone Member is a good candidate for the source rocks of the anomalous, uranium-bearing boulders at Anomaly “H”.

2.2.3.4 Middle Mudstone (Mm) This member of the Humber Falls Formation is not always encountered in drill core. The member is present to the north and south of Wigwam Brook but not within the immediate Wigwam area (Thurlow, 2003). It occupies a position between the underlying oxidized Sm and overlying reduced St and the contact with Sm is commonly a locus for strong hematite alteration with elevated radioactivity and uranium levels. It was encountered six times in 2009 and was described as a greenish-grey to charcoal grey, micaceous, clayey to silty mudstone that locally becomes sandy towards the base of the interval. It typically hosts variable amounts of organic trash (disseminated detritus, coal seams and organic fragments). It is variably hematitic (locally a reddish-brown colour or hosts strong, hematitic patches). Previous descriptions have made notes of containing carbonate nodules (caliche?). Correlations of the Middle Mudstone and Trashy Sandstone members between the Wigwam Brook area and the Birchy Hill Brook area are problematic.

2.2.3.5 Trashy Sandstone (St) Organic detritus, sometimes quite coarse (>10cm long), characterizes this sandstone member. The organic material commonly contains a rim and/or core of pyrite and is often associated with yellowish-brown limonitic weathering that can be pervasive. Furthermore, the organic debris can have a vitreous-looking appearance or a sooty, dull appearance and is often coalified (wood texture is partially preserved). Oxidation within this reduced member is rare and the colour is generally a uniform light grey. The Trashy member resembles all other sandstone members and consists of sandstone (fine- to very coarse) and conglomerate (granule to pebble)

…16

intervals with minor silty and clayey mudstone beds. Bedding is exhibited in most drill holes however there are instances where the member is massive. It predominantly overlies the Middle Sandstone Member with a sharp, often strongly hematitized contact however it locally overlies the Middle Mudstone Member.

2.2.3.6 Upper Mudstone (Mu) This member overlies the Trashy Sandstone Member with a sharp to gradational contact. It dominantly consists of brownish to greenish coloured, silty mudstone with minor fine- to very coarse-grained sandstone. It is usually semi-consolidated, hosts sporadic reduction (spots, rings and sections) and limonitic weathering and occasionally contains organic detritus. Nodular carbonate (caliche) is better developed (locally spectacular) in this member than elsewhere in the stratigraphy.

2.2.3.7 Upper Sandstone (Su) This member resembles the other sandstone members of the Humber Falls Formation. It overlies the Upper Mudstone Member with a sharp, often hematitized and anomalous contact. The member consists of alternating and gradating sandstone and conglomerate intervals with minor silty and clayey mudstone. The sandstones of this member are typically coarser than the other members but can be fine-grained as well. Varying styles and intensities of oxidation are present, though unoxidized rocks are not uncommon. Organic detritus can be quite coarse, minute or even missing. Limonitic weathering is locally common and is often associated with organic debris. This member tends to be massive however bedding has been observed. The Upper Sandstone Member has potential to be the source rocks of the high-grade boulders discovered at Wigwam Brook, Birchy Hill Brook and possibly the Goose Boulder Fields.

3.0 2009 EXPLORATION PROGRAM 3.1 Work Completed & Methodology

Exploration in 2009 consisted of a diamond drilling program with attendant borehole radiometric surveying, geochemistry (lithogeochemistry and assays), PIMA analyses and an environmental assessment that included the backfilling of the Wigwam Brook trench that was excavated during the 2007 program. A total of 1,958.2 metres were drilled in 38 new drill holes. An overview of the distribution of drill holes is provided on Maps 01 and 02. A Mount Sopris MGX II digital logging system was used to conduct borehole radiometric surveys of the 2009 drill holes. This is the same unit that has been used on the project since 2005. An experiment conducted in 2006, 2007 and again in 2009 showed negligible year-over-year instrument drift. One hole (RB-09-244) was not surveyed in 2009 due to a subsurface obstacle. Furthermore, four drill holes (RB09-230, 237, 241 and 257) were not surveyed to the end of hole due to downhole obstruction(s). A total of 486 core samples, including systematic and interval samples, were collected during this program. Core logging was completed at White Hills Tourist Lodge near Bonne Bay, NL. Once on site, the core was cleaned, reassembled where

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possible and photographed. Digital photographs of the 2009 core (drill holes RB-09-226 to 263) can be found on the disk located in the front pocket of this report. The core, now cross-piled and covered by tarpaulins, is being stored at the lodge, along with some of the 2006 and all of the 2007 core. Presently, the core from all Altius/JNR drill programs (2005 – 2007 & 2009) is in storage at two different sites (Big Falls Tourist Lodge, along the Humber River and White Hills Tourist Lodge near Bonne Bay). A handheld Exploranium GR-135 spectrometer/scintillometer (50 – 75 counts per second background) was used to measure the radioactivity of the core at the drill site and during core logging/sampling. The GR-135 was also used to obtain “crude assays” of potassium (%), uranium (ppm) and thorium (ppm) on all samples. In addition, an Exploranium KT-9 magnetic susceptibility meter was used to measure the magnetic susceptibility (K) of both the core and rock samples (the uraniferous boulders have moderately elevated K values in comparison to unmineralized Humber Falls Formation sandstones). A complete listing of contractors and personnel as well as a statement of expenditures is included in Appendix 1 of this report.

3.2 Diamond Drilling 3.2.1 Introduction

The 2009 diamond drilling and radiometric logging program was designed to follow up on targets identified by the 2008 exploration program (water sampling survey, IP/Restivity survey and detailed geological re-evaluation). Drilling was conducted in the Birchy Hill Brook, Wigwam Brook and Goose Anomaly areas only. There were no drilling operations at Anomaly H in 2009. A database containing all drill hole information is included as Appendix 2. All of the drill sites were located using a handheld Garmin etrex Legend C GPS unit, with an accuracy of 5 to 10 metres. Altius employees Edison Keats of Buchans, NL and Mervin Davis of Westport, NL prepared the drill sites and trails. The drill program commenced on August 26th and continued until October 29th, 2009 and was contracted to New Valley Drilling Ltd. of Springdale, NL. A Nodwell-mounted diamond drill rig was utilized for the program on a single shift basis. This rig, accompanied by a supply muskeg, allowed for quick and relatively easy access to the sites with minimal ground disturbance. Oversized BQ core was recovered using B-sized Thin Wall or BTW (BQTK) drill equipment. The drill core was boxed and secured at the drill site and brought to the base camp daily where it was logged, photographed and sampled. In addition to logging, measurements of radioactivity, magnetic susceptibility and oxidation (visual determination) were also collected. Diamond drill logs are included in this report as Appendix 3. Upon completion of a drill hole, all the BTW equipment was pulled out and replaced by a string of PVC pipe, purchased from Wellmaster of Tillsonburg, ON. This enabled the drill to be able to pull the casing and leave the site prior to the borehole radiometric survey. The PVC pipe remains in the holes. Additionally, an environmental assessment of each collar

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and water supply location was conducted. Drill sites were inspected for debris and surficial disturbance and comments regarding further clean-up and reclamation requirements were suggested if necessary. Once completed, the forms were signed by the geological technician performing the site assessment, the project geologist and the drilling supervisor. Furthermore, Edison Keats, Mervin Davis and/or Andrea Devereaux inspected and photographed each site prior to the mobilization of the drill to the site. The diamond drill holes were surveyed using a Mount Sopris MGX II radiometric logging system and 2GHF-1000 Triple Gamma/Geiger Combination Probe(s). The Mount Sopris 2GHF-1000 probe specifications are included in this report as Appendix 4. Edison Keats and Mervin Davis of Altius Resources and Richard From of JNR Resources, completed all of the surveys. The system measures borehole radiation at one-centimetre (arbitrary) intervals using a highly sensitive sodium iodide (NaI) crystal in combination with two, less sensitive Geiger Mueller (G-M) tubes. The radiometric data was output to, and recorded on, a Panasonic Toughbook laptop computer that was connected via a serial/USB cable to the logging system. The data was then incorporated into drill hole cross-sections, which are included in this report as Appendix 5. As in previous programs, all drill holes were surveyed with the joint between the cable head of the logging system and the probe at ground level in order for the drilling and probe depths to correspond (first measurement upon zeroing is 1.80 metres, which corresponds to the bottom of the probe). In 2008, it was brought to the attention of Altius and JNR that the sodium-iodide (NaI) crystal, which measures radioactivity, is actually 0.15 metres from the bottom of the probe. As a result, an additional 0.15 metres was subtracted from the probe data and thus, the first measurement of all probe data is 1.65 metres.

3.2.2 Drill Core Sampling Samples of drill core were taken for PIMA studies, lithogeochemical analyses and assays. In total, 486 samples were collected in 2009, all of which were core samples. There were two different types of core samples taken: (1) 355 lithogeochemical/PIMA samples (five-metre systematic samples). For the most part, both sandstones and mudstones were sampled. The systematic samples were collected using a hammer and chisel to extract a small (3 to 5-inches), elongate piece of core at approximately 5-metre intervals in all drill holes. The samples, once collected, are placed into 30-dram (dr) prescription vials. ‘The reasoning for the five-metre systematic samples is to provide a “scan” of the sandstone/mudstone column and to give an idea of the downhole geochemistry.’ The preceding was paraphrased from sample methodology notes belonging to Ken Wasyliuk of JNR Resources. (2) 131 assay samples of split core were taken at specific intervals in various drill holes. These samples correspond to sections of elevated borehole radioactivity (as recorded by the down-hole probe) or anomalous features (eg. alteration and/or mineralization). Samples were shipped in secured, 5-gallon buckets via Day and Ross (ground transport) to JNR Resources of Saskatoon, SK for PIMA analyses and then to the Saskatchewan Research Council (SRC) in Saskatoon, SK for

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geochemical analyses. Complete sample listings, geochemistry and PIMA results are included in this report as Appendices 6, 7, 8 and 9.

3.2.3 Observations on Field Aspects of the Diamond Drill Program A Nodwell-mounted drill rig was used for the 2009 program. The nodwell was slightly larger than the muskegs used in previous programs, but was able to manoeuvre the boggy terrain more easily and with less ground disturbance. The drill was accompanied by a second supply nodwell which was comparable in size to the drill. The size of these machines allow for quick and easy access to the drill sites with minimal ground disturbance as the tracks are slightly longer and wider than those on the muskegs. As stated in previous assessment reports, a common issue with the drill is with core recovery. Although this was encountered again in 2009, it was discovered that using less pressure when drilling made it easier to remove the core from the inner tube. There were, however, still instances where a hammer was needed to retrieve the core from the tube, resulting in broken and disaggregated core. Overall, core recovery was much better in 2009 than it had been in previous years. A series of technical issues with the down-hole radiometric equipment were encountered approximately half way through the program. It was discovered there was a problem with the MGX II logging console. A replacement logging console was supplied by JNR for the remainder of the program.

3.2.4 Drilling Results The following sections provide the geochemical and geological highlights from the 2009 program. Assay results were received a week prior to the due date of this report. As a result, the observations presented within are preliminary in nature. A more detailed and thorough program of interpretation will be conducted in the upcoming months. All down-hole information will be incorporated into the 3D Gocad model at this time as well. The analytical data listed in the following discussion is reported from the partial digestion analyses with the exception of thorium, which is reported from the total digestion analyses.

3.2.4.1 Wigwam Brook Area A total of 710.0 metres were drilled in fourteen holes (RB-09-226 to 231 and RB-09-237 to 244) in the Wigwam Brook area in 2009. The first six drill holes were designed to test shallow anomalies identified by the 2008 IP/Resistivity survey. The remainder of the drilling was designed to follow up on anomalous stratigraphy encountered in RB-09-227. Drill holes RB-09-226 to 231 were drilled to test IP/Restivity anomalies in the Wigwam Brook area. While the targets highlighted by the survey were only weakly anomalous, they appeared to be shallow and within the Su and Mu Members, both of which host low-grade uranium mineralization in the Wigwam Brook area (O’Reilly et al., 2007). Drill holes were designed with input from consulting geophysicist, Ken Sweet of Littleton, Colorado who supervised the 2009

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IP/Restivity program. In most cases, the drilling results suggest that the anomalous readings were associated with pyrite mineralization within the coalified wood-bearing St Member and not uranium mineralization. One drill hole, RB-09-229 however, did intersect numerous narrow zones with anomalous radiometrics. The most significant was a 1.62m intersection (from 8.47 – 10.09m) that had an average of 230 CPS and a peak of 788 CPS. Another notable intersection from this drill hole was a 2.31m zone (from 14.34 – 16.65m) with an average of 83 CPS and a peak of 230 CPS. RB-09-229 intersected numerous, smaller (0.50 – 1.20m) zones throughout with averages of 63 – 94 CPS. This drill hole extended the zone of anomalous bedrock radioactivity outlined previously (O’Reilly et al., 2007) further to the east by approximately 60 metres. The best radiometric and geochemical results obtained from this drill hole are provided in the following table.

Table 3. Anomalous Assay and Probe Results from RB-09-229, Wigwam Brook Area

Sample No.

Depth (m) Peak/

Average (NaI)

Lithology Description Assays (ppm)

RB-09-229-008

40.10 -- St cg sst-cgl, py surrounding

clast, micaceous 0.6 Ag, 418 Cu, 10.7 Mo,

26 Th

R2945 8.47 – 9.01 210/115 Su tan-buff cg-vcg sst,

intermixed green mud 13.4 U

R2947 9.55 – 10.09 788/430 Su cg-vcg sst, wk-mod hm alt 11.6 U

R2948 10.96 – 11.70 120/63 Su tan-buff cg sst, minor green

intermixed mud 112 U, 230 Cu, 48.9 Zn

R2951 15.26 – 15.72 158/107 Mu greenish slty mst – slt 25 Th, 39.9 Zn

R2952 15.72 – 16.18 115/69 Mu fg-mg sst and mud, spotty

green ‘chl’ alt 61 Th

R2953 16.18 – 16.65 96/53 Mu fg-mg sst, spotty, green ‘chl’

alt 49 Th

* Assay results are from partial digestion ICP-OES analyses. Drill holes RB-09-230 and 231 were also designed to test anomalous IP/Resistivity zones, however, these anomalies appear to be larger, broader and deeper than those previously tested. While neither drill hole exhibited elevated radioactivity, RB-09-230 was only probed to a depth of 39.35m (due to a down-hole obstruction). As suspected, the anomalies were associated with lithological variations and not the result of uranium mineralization. Both drill holes exhibit a distinct, bright red oxidation that is typical of sandstones and mudstones west of the PML in the Birchy Hill Brook area. While the degree of oxidation varies throughout both drill holes, it is possible that this difference in oxidation may be the cause of the elevated

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chargeability responses. Furthermore, a bright white alteration (gypsum?) and drusy calcite associated with strongly hematitized fractures and veins were observed locally throughout both drill holes and could be the cause of the increased resistivity. Prior to this drilling, there had been no indication of the PML in the Wigwam Brook area. Interestingly, the zone of low-grade mineralization at Birchy Hill Brook exists just east of this feature and it is possible that the low-grade zone at Wigwam Brook has a similar association. Further to the PML, an oxidation front within the St Member is also postulated to exist, east of these two drill holes, as neither exhibits the distinctive, reduced, organic trash-bearing sandstone typical of the Wigwam Brook area. Drill holes RB-09-237 – 244 followed up on anomalous stratigraphy encountered in RB-09-227. It was anticipated that this drill hole would collar in Su, however it collared in, what appears to be, St instead. The original geology (Thurlow, 2002) of the area suggested an ‘S’ shaped geometry to the sedimentary strata, however further discussions brought forward the idea of a cross-structure in the area, to allow for the St Member to be at surface. Previously drilled holes in the vicinity of this new drill hole also document similar, anomalous stratigraphy. The presence of a cross-cutting fault, located between RB-09-227 and the drill holes to the north, would likely explain the anomalous stratigraphy. As a result, a series of holes were drilled in order to define and test the structure both at surface and at depth. Drill holes RB-09-237 to 239 were drilled north of RB-09-227 and are believed to have intersected a shallowly dipping structure or a “zone of movement” near the basal contact of the Upper Mudstone. In previous years, broken and disaggregated mudstone was thought to be the result of removing the core from the inner-tube. However, improved core recovery in 2009 suggests the broken core is a structural feature of the Upper Mudstone in the area. Holes drilled to the west of this series of drill holes (RB-09-240 – 243) support the presence of an additional structure as the St Member, which is often easily drilled with excellent core recovery, was locally quite broken, fractured and partially to completely disaggregated. This structure is interpreted as being a shallow-dipping, brittle structure that may be related to the “zone of movement” described previously. A lack of significant radioactivity and disappointing assay results suggest that this structure is not the source of the high-grade boulders. The best uranium assay from the entire series of drill holes (RB-09-237 – 244) was 2.92 ppm U in a greenish-grey, micaceous siltstone within the Mu Member of RB-09-243. The best probe results were also from RB-09-243 which intersected numerous small, weakly anomalous zones. The most impressive intersection was a 1.94m zone (from 9.46 – 11.40m) with an average probe reading of 103 CPS and a peak of 348 CPS. Unfortunately, the anomalous radiometrics appear to be thorium related (up to 20 ppm Th with 1.13 ppm U). A small, weak to moderate airborne anomaly (believed to be the result of uranium) near the proposed cross-structure was targeted by drill hole RB-09-244. Due to a down-hole

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obstruction, radiometric data was not collected from this hole. There was significant lost core (1.24m lost from 6.00 – 9.00m) near the top of the drill hole that may have been the cause of the obstruction. In addition, the obstacle may also suggest that the structure, intersected in RB-09-243was intersected here as well. A section of coalified wood (0.14m wide) with massive pyrite and trace chalcopyrite mineralization was sampled from RB-09-241. The sample (R2996) assayed anomalous copper (636 ppm), silver (2.7 ppm), molybdenum (8.1 ppm) nickel (60.5 ppm), lead (30.7 ppm) and cobalt (74.8 ppm). Results were significantly higher in the total digestion analyses (2,580 ppm Cu, 11.5 ppm Ag, 34 ppm Mo, 262 ppm Ni, 233 ppm Pb and 302 ppm Co). Although anomalous pathfinder mineralization was encountered, the uranium values were background (0.48 ppm U – partial digestion; 7.0 ppm U – total digestion).

3.2.4.2 Goose Anomaly Area Drilling at the Goose Anomaly was designed to test and define structures believed to host uranium mineralization causing anomalous scintillometer readings in the water saturated bog that covers the area. Thurlow (2009) proposed numerous high-angle reverse faults and a series of cross-cutting faults in the area highlighted by the 2008 water survey. Additionally, the target areas also have increased chargeability and/or resistivity. Six drill holes, totalling 325.2 metres, were drilled in three, scissor-like arrays targeting these faults (Map 01). Drill holes RB-09-232 and 245 were drilled in the centre of the 2006 airborne radiometric anomaly. This area is the juncture point of numerous faults and was recommended for follow-up exploration because of anomalous resistivity at approximately 50 – 100m depth (L3901E, stn 3050). Evidence of fault(s) (broken, fractured and disaggregated sandstones and conglomerates) were observed throughout both drill holes. While there were no significant intersections of uranium mineralization, there were weakly anomalous uranium values associated with suspect fault zones. Drill hole RB-09-232 intersected a 6.07m anomalous zone (from 38.82 – 44.89m), corresponding with the Mu and St Members, that had an average of 90 CPS and a peak of 202 CPS. This interval also returned the best uranium assay from all of the 2009 Goose Anomaly drilling with 13.1 ppm U (plus 109 ppm Cu). Additionally, RB-09-232 and 245 returned weakly anomalous uranium values with associated copper and silver locally. The following table provides the assays of the most anomalous intersections.

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Table 4. Anomalous Assay and Probe Results for Drillholes RB-09-232 and 245, Goose Anomaly Area

Sample No. Depth Peak/Average

(NaI) Lithology

Assays (ppm)

RB-09-232 008 45.00 -- Sm 11.2 U, 139 Cu

RB-09-232 R2972 42.04 - 42.52 202/120 St 10.3 U, 173 Cu, 0.7 Ag

RB-09-232 R2976 43.96 - 44.44 103/72 St 13.1 U, 109 Cu

RB-09-232 R2977 44.44 - 44.89 114/78 St 12.1 U, 218 Cu

RB-09-245 008 43.00 -- Sm 8.16 U, 172 Cu, 14 Th

* Assay results are from partial digestion ICP-OES analyses. Drill holes RB-09-233 - 236 are located further east and were completed on the basis of defining the cross-structure depicted by Thurlow (2009). Drill holes RB-09-233 and 236 were drilled in the vicinity of Westfield’s historic drill hole (79-29) which, when re-surveyed by Altius, displayed anomalous radiometrics for most of the drill hole, including the overburden. Drill hole RB-09-233 intersected two zones with weakly anomalous overburden (average radiometrics of ~60 CPS over 0.60 – 0.73m) and RB-09-236 intersected a 4.06 metre thick (from 1.64 – 5.70m) overburden zone with an average of 245 CPS and a peak of 1006 CPS. Interestingly, there was no anomalous bedrock in either drill hole. Drill holes RB-09-234 and 235 intersected a weakly anomalous Su member (average of 53-63 CPS with peaks of 85 – 108 CPS) described as a coarse-grained sandstone and conglomerate that is locally blocky, broken and disaggregated with weak to moderate, reddish hematite alteration and local strongly hematitized fractures. The best uranium assay from this series of drill holes was from RB-09-235 which returned background uranium (up to 2.34 ppm) values.

3.2.4.3 Birchy Hill Brook Area Most of the drilling at Birchy Hill Brook was designed to target areas of anomalous chargeability and resistivity. While previous drilling campaigns were successful in outlining areas of weakly anomalous bedrock and mineralized structures, the 2009 survey highlighted additional targets outside these previously tested areas. A total of 923.0 metres were drilled in 18 new holes during 2009. Drill holes RB-09-246 – 247, 252 – 254 and 260 - 261 were designed to test areas with weak to moderate chargeability and/or resistivity. Drill holes RB-09-252 – 254 are also in an area with anomalous water chemistry and no previous drilling. The best down-hole radiometric

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measurement was a 1.94m zone (25.49 – 27.43m) with an average of 138 CPS and a peak of 412 CPS in drill hole RB-09-253. This zone corresponds to a reddish-brown mudstone with limonite alteration (24.30 – 26.83m) which was followed (down-hole) by a grey, fine- to medium-grained, micaceous sandstone with abundant stratified organic material resembling the St Member. The best assay for this intersection, however, is 4.01 ppm U associated with the St-like sandstone. Drill holes RB-09-248 – 251 and 255 – 258 were designed to test anomalous “breaks” in chargeability and resistivity profiles on the pseudosections. These breaks are considered anomalous and may indicate mineralized structures. Targeting these features involved drilling a vertical (-90) hole the entire depth of the Humber Falls Formation and 2 to 5 metres of the Rocky Brook Formation, followed by collaring a second, angled (-45) drill hole, located an appropriate distance back to undercut the previous one. This approach was performed four times on two anomalous pseudosection areas. Drill holes RB-09-248, 251, 257 and 258 tested a “break” on L9500N and L9450N near L4260E. Each of the drill holes intersected variably anomalous overburden. Drill hole RB-09-248 displayed the best overburden radiometrics with an average of 88 CPS and a peak of 148 CPS over 3.13m. This series of drill holes was also successful in identifying another area of weakly mineralized Su Member. Anomalous radiometrics associated with strongly hematitized fractures, veins and patches were intersected in RB-09-251; however the best assay from this section was only 7.43 ppm U. An anomalous yellow, limonite(?)-altered, coarse-grained sandstone was intersected in drill hole RB-09-258 which assayed up to 7.14 ppm U. The handheld scintillometer suggests the anomalous radiometrics are associated with larger, coalified wood fragments within this Su. Indications of structure(s) (lost, broken and disaggregated core) both near surface (6.5 – 13.2 m depth) and at depth (48.0 – 50.8m) were supported by very difficult drilling in RB-09-257 and 258. In both instances, the drillers reported the holes as being very tight. In RB-09-257, a core barrel and bit were lost in the hole and in RB-09-258, the rods became stuck and had to be broken in order to free the drillstring. The following table provides the best down-hole results from this series of drill holes, along with the best uranium assay from the associated interval.

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Table 5. Uranium Assay Results for Drillholes RB-09-248, 251 and 256 – 258

Drill hole Depth (m) Peak/Average

(NaI) U (ppm) Description

RB-09-248 1.64 – 4.77 148/88 n/a Overburden

RB-09-248 29.01 – 30.42 180/70 0.96 reddish-brn clayey-silty mst, micaceous

RB-09-251 2.10 – 5.72 123/63 n/a Overburden

RB-09-251 7.25 – 9.75 287/110 7.43 reddish-brown to tan-buff cg sst with local, strongly

hematitized fractures/veins

RB-09-251 52.68 – 53.42 140/77 0.37 dark greenish, cg sst, pervasive and stratified

reduction

RB-09-257 3.81 – 5.08 110/66 n/a Overburden

RB-09-251 3.77 – 4.77 111/61 n/a overburden

RB-09-258 5.04 – 6.91 124/66 7.14 beige-yellow, limonite(?) altered sst, clay alt on

fracture surfaces, minor organic detritus

* Assay results are from partial digestion ICP-OES analyses. Drill holes RB-09-249 - 250 and 255 – 256 targeted a “break” in the chargeability and resistivity profiles on L9500N and L9450N near L4050E. The best radiometrics from this series of drill holes come from a greyish, fine- to medium-grained sandstone that hosts abundant fine-grained organic detritus throughout. The best probe results were from a 1.04m zone in drill hole RB-09-256 that had an average of 256 CPS and a peak of 656 CPS. An assay from just below this interval (from 38.00 – 38.50m) sampled the same St-like sandstone and also hosted a strong, reddish-brown hematite blotch. This sample (R3944) returned the best assay for all of the Birchy Hill Brook area with 91.5 ppm U, 1070 ppm Cu, 308 ppm V, 55.8 ppm Zn, 26.2 ppm Co, 22.6 ppm Pb and 0.8 ppm Ag. Unfortunately, the remaining samples from this series of drill holes did not return anomalous results with respect to uranium (<7.23 ppm U). Drill hole RB-09-259 was designed to test an area of anomalous chargeability that is outlined on L9400N and L9500N. This area coincides with the PML, a cross-structure and a “tectonite”/regolith horizon that was sampled and described (both in core and through petrography) during the 2007 program (O’Reilly et al., 2008). This drill hole also tested the northern extents of the zone of low-grade bedrock mineralization outlined by O’Reilly et al., (2007). Unfortunately, there were no significant radiometric anomalies associated with this drill hole. The best assay (R3949) returned 5.61 ppm U with 436 ppm Cu from a greenish, coarse-grained sandstone with spotty, green chlorite-like alteration.

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Drill holes RB-09-262 and 263 were designed to test an IP anomaly within the Wigwam Fault zone (L9400N, station 4725E). As the structure was interpreted to be near vertical, an angled hole was drilled with the anticipation of drilling through the structure or zone of higher chargeability and possibly into the Humber Falls Formation. Unfortunately, drilling was very slow and difficult, with the hole caving in frequently. As a result, RB-09-262 was terminated at a final depth of 20.33m to avoid losing drilling materials down-hole. A second attempt was made in this area, by setting up directly above the zone and drilling a vertical drill hole to an anticipated depth of 100m. Again, drilling was slow and difficult and was terminated at a depth of 18.80m. In both instances, the drill holes collared in Rocky Brook Formation and the core was badly broken. Radiometrics and assay results from both drill holes were not significant and no significant alteration was visible in the core.

3.3 Environmental Assessment Program During the summer of 2009, a total of five days were spent assessing the ground disturbance on most of the drill trails and sites at the project. The assessment was conducted by Altius geologist, Dale O’Reilly, who has been the project geologist and supervising geologist on the project since 2005. Two student geologists, Jessica Ivany and Jason Flight, were also present to help with the assessment and photography. The purpose of the assessment was to further address the concerns, raised in 2008, by the Forestry Division of the Newfoundland and Labrador Department of Natural Resources and to assess the current ground disturbance, natural re-vegetation and areas that will require reclamation. A copy of the report is included as Appendix 10.

4.0 CONCLUSIONS & RECOMMENDATIONS The following points can be highlighted from the exploration program in 2009:

• The Nodwell-mounted drill, while larger than the muskeg-mounted ones used in previous years, appears to manoeuvre the boggy terrain more easily, resulting in quicker moves between drill holes with less ground disturbance. As a result, this type of equipment is recommended for this project in the future.

• While the IP/Resistivity survey was successful in identifying zones of low-grade mineralization, it is uncertain what exactly caused the weak chargeability anomalies in some drill holes. Overall, the presence of pyrite associated with organic material correlates well with the chargeability anomalies.

• Differential GPS surveying, as was completed in 2007, is recommended for all the 2007 and 2009 drill holes. Accurate drill hole location data is essential for detailed geological correlations.

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• Additional drilling is recommended to truly test the Wigwam Brook anomaly. Although significant uranium mineralization has been intersected in the area, infill drilling in the anomalous bedrock zone is required to adequately test the zone, both at surface and at depth.

• On-going data synthesis and interpretation should be continued. Detailed correlations, as were completed in 2008, are recommended in order to link the new drill holes with the existing stratigraphic interpretation. At that point, the revised geology should be incorporated into the ongoing 3D Gocad model. Compilation of a ‘Common Earth Model’ may also be valuable in choosing future drill targets with such an immense amount of information available.

5.0 ACKNOWLEDGEMENTS Altius is pleased to acknowledge the contributions of David Billard, Dr. Irvine Annesley and Ken Wasyliuk of JNR Resources. JNR personnel have a wealth of uranium exploration experience and their input on many matters continues to be invaluable. Additionally, Ken Sweet of Kenco Minerals is acknowledged for his time and expertise with respect to recommending drill targets designed to test IP/Resistivity anomalies and providing prompt advice when needed most. Respectfully submitted this 25th day of January 2010 by,

Andrea Devereaux, B.Sc. (Hons) Geologist

Dale O’Reilly, B.Sc (Hons). Geologist

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6.0 BIBLIOGRAPHY & REFERENCES Devereaux, A., O’Reilly, D., Churchill, R. and Thurlow, J.G., 2009. Sixth, seventh & eighth year assessment report on mineral exploration on the Rocky Brook Joint Venture, Mineral Licenses 007897M, 010141M, 016050M, 016051M and 016052M, Deer Lake Area, western Newfoundland, NTS Sheets 12H06. 28 pages plus 8 appendices, O’Reilly, D., Devereaux, A., Churchill, R. and Thurlow, J.G., 2008. Sixth and seventh year assessment report on mineral exploration on the Rocky Brook Joint Venture, Mineral Licenses 7897M, 8647M, 10141M and 10727M, Deer Lake Area, western Newfoundland, NTS 12H/06, 07, 10 and 11. 35 pages plus 14 appendices and 3 maps. O’Reilly, D., Mercer, P., Churchill, R. and Thurlow, J.G., 2007. Fourth, fifth and sixth year assessment report on mineral exploration on the Rocky Brook Joint Venture, Mineral Licenses 7897M, 8647M, 10141M and 10727M, Deer Lake Area, western Newfoundland, NTS 12H/06, 07, 10 and 11. 33 pages plus 12 appendices and 2 maps. Thurlow, J.G. and Churchill, R., 2007. Assessment report on an airborne geophysical survey covering Mineral Licenses 7897M, 8647M, 10141M, 10727M (Rocky Brook property); 8878M, 9287M and 10935M (Viking and Wizard properties); 8193M and Mining Lease 60, western Newfoundland, NTS 12H/06, 10, 11 and 15. 5 pages plus 1 appendix. Thurlow, J.G., 2006. Personal Communication. Sweet, K., 2006. Personal Communication. Sparrow, B., 2006. Lithogeochemical and petrographic study of uranium mineralization in relation to hematite deposition in the Deer Lake Basin, western Newfoundland. Unpublished B.Sc. Honours Thesis, Memorial University of Newfoundland, 98 pages. Thurlow, J.G., O’Reilly, D., Graves, M., Mercer, P. and Churchill, R., 2006. Third, fourth and fifth year assessment report on mineral exploration on the Rocky Brook Joint Venture, Mineral Licenses 7897M, 8647M, 10141M and 10727M, Deer Lake Area, western Newfoundland, NTS 12H/06, 07, 10 and 11. 28 pages plus 6 appendices and 1 map. Thurlow, J.G., Barrett, S., Mercer, P. and Churchill, R., 2004. Second and third year assessment report on mineral exploration on the Rocky Brook Joint Venture (Mineral Licenses 7897M, 8198M, 8199M, 8200M, 8647M, 8648M and 8649M). 43 pages plus 7 appendices.

…29

Chester, F.M., Chester, J.S., Kirschner, D.L., Schulz, S.E. and Evans, J.P., 2004. Structure of large-displacement, strike-slip fault zones in the brittle continental crust. In: Rheology and Deformation in the Lithosphere at Continental Margins, Edited by Karner, G.D., Taylor, B., Driscoll, N.W. and Kohlstedt, D.L., Columbia University Press, New York, 2004, 42 pages. Thurlow, J.G., 2003. Report on mineral exploration on the Rocky Brook Joint Venture (Mineral Licenses 7897M, 8198M, 8199M, 8200M, 8647M, 8648M and 649M), Deer Lake Basin, western Newfoundland, NTS 12H/06, 07, 10 and 11. 25 pages plus 10 appendices. Churchill, R., Butler, R.W., Barbour, D.M. and Barrett, S., 2002. First year assessment report on prospecting, trenching, sampling and compilation, map-staked licenses 7897M, 8198M, 8199M, 8200M, 8649M, 8648M and 8647M, Rocky Brook Property, Deer Lake Region, western Newfoundland, NTS 12H/06. 23 pages plus 4 appendices. Madore, C and Annesley, I.R., 2001. Petrography of unmineralized and mineralized arkose. Saskatchewan Research Council Report No. 10401-14C01, July 2001, 2 pages with photomicrographs. Batterson, M.J., 2000. Open File 12H/06/1490, Map 2000-16. Landforms and surficial geology of the Cormack map sheet (NTS 12H/06), Newfoundland. (coloured digitally plotted map). Baldwin, A.B., 1998. Second year assessment report on diamond drilling exploration for license 4546M on claims in the Birchy Ridge area, near Deer Lake, western Newfoundland / Report on a Diamond Drilling Program on the Birch Ridge Claims Deer Lake Area, Newfoundland; Newfoundland and Labrador Geological Survey, Assessment File 12H/06/1391, 33 pages. Baldwin, A.B., Plains Exploration LLC, and Chemex Labs. Hamblin, A.P., Fowler, M.G., Utting, J., Landon, G.S. and Hawkins, D., 1997. Stratigraphy, palynology and source rock potential of lacustrine deposits of the Lower Carboniferous (Visean) Rocky Brook Formation, Deer Lake Subbasin, Newfoundland. Bulletin of Canadian Petroleum Geology, Vol. 45, No. 1, pp. 25–53. Paterson, N.R. and Scott, W.J., 1997. First year supplementary assessment report on geophysical exploration for license 4546M on claims in the Birchy Hill Brook area, near Humber River, Newfoundland / REPORT ON GROUND GEOPHYSICAL SURVEYS BIRCHY RIDGE PROPERTY DEER LAKE AREA NEWFOUNDLAND LIC 4546M; Newfoundland and Labrador Geological Survey, Assessment File 12H/06/1534, 1997; 16 pages. Plains Exploration LLC, Paterson, Grant and Watson Limited, Maritec Limited, Geoscott Exploration Consultants Incorporated, and Baldwin, A. B. Wright, J.A., Hoffe, B.H., Langdon, G.S., Quinlan, G.M., 1996: The Deer Lake Basin, Newfoundland: structural constraints from new seismic data. Bulletin of Canadian Petroleum Geology, Vol. 44, no.4 (December 1996), pp. 674–682.

…30

Baldwin, A.B., 1996. First year assessment report on geological and geochemical exploration for license 4399 on claim block 16076 and license 4546M on claims in the Wigwam Brook area, west-central Newfoundland / REPORT ON THE EXPLORATION POTENTIAL OF A PROPERTY IN THE DEER LAKE BASIN, NEWFOUNDLAND N.T.S. 12H/6 Newfoundland and Labrador Geological Survey, Assessment File 12H/06/1449; 44 pages. Baldwin, A.B., Smith, M., and Rocky Mountain Geochemical Corporation. Hyde, R.S., Langdon, G.S., Tuach, J. and Wilton, D.H.C., 1994. The last frontier – a field conference to the Deer Lake Basin, Newfoundland, September 30 – October 2, 1994; Geological Summary and Field Trip Guidebook. Centre for Earth Resources Research, Report No. 1, 74 pages. Batterson, M.J. and Taylor, R.C., 1994. Quaternary geology of the upper Humber River area, western Newfoundland. In Current Research, Newfoundland Department of Mines and Energy, Geological Survey Branch, Report 94-1, pp. 1-9. Owen, J V., 1991. Geology of the Long Range Inlier, Newfoundland; Geological Survey of Canada, Bulletin, no. 00395, 1991; 89 pages. Geofile No. NFLD/2563. Giggie, K V., 1991. Third year assessment report on geological, geochemical and trenching exploration for the Humber River and Deer Lake projects for license 3436 on claim blocks 6085 and 6087-6088 in the Goose Pond and Wigwam Brook areas, northwestern Newfoundland; Newfoundland and Labrador Geological Survey, Assessment File 12H/06/1231, 1991; 60 pages. Inco Gold Company, NovaGold Resources Incorporated, Bondar-Clegg and Company Limited, and Eastern Analytical Limited. Saunders, C.M. and Smyth, W.R., 1990. Geochemical characteristics of the Gull Lake Intrusive Suite and Devil’s Room Granite, Western White Bay, Newfoundland. In Current Research, Newfoundland Department of Mines and Energy, Report 90-1, pp. 183-199. Vidito, S., 1989. First year assessment report on geological, geochemical, geophysical and diamond drilling exploration for the Humber project for license 3436 on claim blocks 6082-6089 in the Upper Humber River, Birchy Hill Brook and Wigwam Brook areas, western Newfoundland, 2 reports; Vidito, S; Sizgoric, M. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/1114, 1989; 187 pages. Inco Exploration and Technical Services Incorporated, Eastern Analytical Limited, Inco Gold Company, and Bondar-Clegg and Company Limited. Williams, H., Coleman-Sadd, S.P. and Swinden, H.S., 1988. Tectonic-stratigraphic subdivisions of central Newfoundland. In Current Research, Part B, Geological Survey of Canada, Paper 88 1B, pp. 91-98.

…31

Hyde, R.S., Miller, H.G., Hiscott, R.S., and Wright, J.A., 1988: Basin architecture and thermal maturation in the strike-slip Deer Lake Basin, Carboniferous of Newfoundland. Basin Research, v.1, pp. 85-105. Harris, A., 1988. Drill core reduction – a pilot study. Newfoundland Department of Mines, Mineral Development Division, Report 88-1, pp. 437-445. Gall, Q. and Hiscott, R.N., 1986: Diagenesis of Locally Uraniferous Sandstones of the Deer Lake Group and Sandstones of the Howley Formation, Carboniferous Deer Lake Subbasin, western Newfoundland. Bulletin of Canadian Petroleum Geology Vol.34, No.1 (Mar. 1986); pp.17-29. Bradley, D.C. and Bradley, L.M., 1986. Tectonic significance of the Carboniferous Big Pond Basin, Cape Breton Island, Nova Scotia. Canadian Journal of Earth Sciences, Vol. 23, 1986, pp. 2000-2011. Hyde, R.S., 1983. Geology of the Carboniferous Deer Lake Basin, Newfoundland Department of Mines and Energy, Map 82-7, NFLD/1849. Wilkinson, R.I., 1983. Report on continued geological, geochemical and geophysical exploration of Reid lot 218 in the Upper Humber Valley area, Newfoundland; Wilkinson, R.I. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0808, 1983; 43 pages. Reid Newfoundland Company Limited, Westfield Minerals Limited, Atlantic Analytical Services Limited, O’Neill-McHugh Laboratories Limited, and X-Ray Assay Laboratories Limited. Wilkinson, R.I., 1983. Assessment report on geochemical and geophysical exploration for 1983 submission for the Deer Lake Basin silver project for Reid lot 218 in the Humber River, Wigwam Brook and Goose Pond areas, western Newfoundland, 4 reports; Wilkinson, R; Lebel, J.L. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0833, 1983; 93 pages. Westfield Minerals Limited, Chutine Resources Limited, Reid Newfoundland Limited, O’Neill-McHugh Laboratories Limited, Bondar-Clegg and Company Limited, and MPH Consulting Limited. Pilgrim, L., 1982. Assessment report on geological, geochemical, geophysical, trenching and drilling exploration for the Deer Lake Basin project for 1981 submission on Reid lot 218 in the Cormack, Wigwam Brook and Humber River areas, Newfoundland, 6 reports; Pilgrim, L; Wilkinson, R; Alter, H W; Taylor, R P; Elias, P; Patterson, M. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0770, 1982; 309 pages. Westfield Minerals Limited, Northgate Exploration Limited, Shell Canada Resources Limited, Atlantic Analytical Services Limited, X-Ray Assay Laboratories Limited, Chemical Projects Limited, Memorial University of Newfoundland, Terradex Corporation, Teledyne Isotopes Incorporated, Eda Instruments Incorporated, and Reid Newfoundland Company Limited.

…32

Wilkinson, R.I., 1981. Report on geological, geophysical and geochemical exploration for licenses 1276-1281 on the Gales Brook claims in the Upper Humber Valley area, Newfoundland; Wilkinson, R I. Newfoundland and Labrador Geological Survey, Assessment File 12H/0693, 1981. Atlantic Analytical Services Limited, Northgate Exploration Limited, Shell Canada Resources Limited, and Westfield Minerals Limited. Wilkinson, R.I., 1981. Report on geological, geophysical and geochemical surveys for the Deer Lake Basin project for license 12051, 1208 and 1209 in the Upper Humber Valley area, Newfoundland; Wilkinson, R. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0681, 1981. Northgate Exploration Limited, Shell Canada Resources Limited, and Westfield Minerals Limited. Wilkinson, R.I., 1981. Report on the geological, geochemical and geophysical exploration for licenses 1275 and 1282 on the Gales Brook claim in the Upper Humber Valley area, Newfoundland; Wilkinson, R. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0692, 1981. Atlantic Analytical Services Limited, Northgate Exploration Limited, Shell Canada Resources Limited, and Westfield Minerals Limited. Patterson, M., 1981. A report on the geological, geochemical and geophysical exploration work performed for the Cormack, Deer Lake Basin project on Reid lot 218 in the Cormack area, Newfoundland; Hiscott, R N; Patterson, M; Tuach, J; Wallgren, P. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0709, 1980. Northgate Exploration Limited, Shell Canada Resources Limited, and Westfield Minerals Limited. Tuach, J., 1980. Report on exploration including appendix on Reid lot 218 in the Upper Humber Valley area, Newfoundland; Hall, R D; Hiscott R N; Nuffield, E W; Patterson, M; Rogerson, R J; Saucier, A E; Steed, G M; Stouge, S; Tuach, J; Vanderveer, D G; Wallgren, P. Newfoundland and Labrador Geological Survey, Assessment File 12H/06/0647, 1980. Westfield Minerals Limited. Hiscott, R.N., 1979. Sedimentology of Humber Falls Formation, Wigwam Brook – RL 218 Drill Core Study. Consultant’s report to Westfield Minerals accompanying assessment report 12H/06/647. Northway Survey Corporation, 1979. Results of airborne survey of Reid lots 36, 38, 40, 42, 44-45 and 218 and many claims in the Deer Lake Basin, Newfoundland; Northway Survey Corporation Limited. Newfoundland and Labrador Geological Survey, Assessment File NFLD/1064, 1979. Northway Survey Corporation Limited and Westfield Minerals Limited. Hyde, R.S., 1979. Geology of Carboniferous strata in portions of the Deer Lake Basin, western Newfoundland; Hyde, R S. Newfoundland and Labrador Geological Survey, Open File, Report 79-6; 46 pages. Geofile No. 12H/0551.

…33

Dimmell, P.M., 1979. Second year assessment report including geophysical and geochemical surveys for license 1084 on claim block 1075 in the Gales Brook area, Newfoundland; Dimmell, P M. Newfoundland and Labrador Geological Survey, Assessment File 12H/0562, 1979. Noranda Exploration Company Limited and Phoenix Geophysics Limited. Byrne, C., 1979. Report on Uranium mineralization location in Reid lot 218 in the Wigwam Brook area, Newfoundland; Byrne, C. Newfoundland and Labrador Geological Survey, Assessment File 12H/16/0549, 1979. Westfield Minerals Limited. Byrne, C., 1978. Results of uranium exploration on Reid lots 35, 36, 38, 40, 42 and 218 in the Deer Lake area, Newfoundland; Byrne, C. Newfoundland and Labrador Geological Survey, Assessment File NFLD/0704, 1978. Westfield Minerals Limited. Dimmell, P.M., 1978. First year assessment report including geological and geochemical surveys of license 1084 in the Gales Brook area, Newfoundland; Dimmell, P M. Newfoundland and Labrador Geological Survey, Assessment File 12H/0092, 1978. Noranda Exploration Company Limited. Curtis, L., 1976. Report on reconnaissance of Reid Lots 218, 220, 222, 223, 41 and 44 and Tilt Cove area for uranium. Urangesellschaft Canada Limited. NFLD (952). Knight, I., 1976. Geology of the Carboniferous of the Codroy Valley and northern Anguille Mountains. Newfoundland Department of Mines, Report 76-1 Report of Activities, pp. 10-18.

…A1

APPENDIX 1. LIST OF CONTRACTORS & PERSONNEL; STATEMENT OF EXPENDITURES

CONTRACTORS AND VENDORS

Contractor or Vendor Location Goods and/or Services Provided

Altius Resources Inc. St. John's, NL geological equipment rentals

Bell Mobility Inc. St. John's, NL cellular phone service

Big Falls Tourist Lodge Bonne Bay, NL meals & accommodations

Bugden Signs St. John's, NL signage (men working in area)

Cross Town Express Ltd. St. John's, NL shipping & freight

Dave Billard Saskatoon, SKtechnical & professional assistance;

geology & DDH planning

Day & Ross (NFLD) Ltd. St. John's, NL shipping & freight

Department of Environment St. John's, NL fording permits

Dicks & Company Limited St. John's, NL field supplies

Dorman Roberts Ltd. Triton, NL shipping & freight

Eastern Analytical Limited Springdale, NL sampling supplies

Enterprise Rent‐a‐Car Corner Brook, NL vehicle leasing

Federal Express Toronto, ON shipping & freight

Ford Credit Canada Leasing Company Calgary, AB vehicle leasing

Ken Wasyliuk Saskatoon, SKtechnical & professional assistance; PIMA &

geochemical data management

Kenco Minerals Littleton, CO (USA)technical & professional assistance; geophysical

data review & DDH planning

Metro Deliveries Limited St. John's, NL shipping & freight

Momentum Conferencing Corp. Toronto, ON telephone conferencing services

National Dosimetry Services Ottawa, ON dosimetry monitoring

New Valley Drilling Company Ltd. Springdale, NL contract diamond drilling

Premium Enterprises Limited Deer Lake, NL fuel, supplies, meals

Provincial Airlines St. John's, NL passenger flights for crew changes

Rick Kusmirski Saskatoon, SK technical & professional assistance; geology & DDH planning

Rob's Grader Services & General Contracting Inc. Springdale, NL excavator & float hire for trench reclamation

Saskatchewan Research Council Saskatoon, SK geochemical analyses

Shears' Bus Service Ltd. Rocky Harbour, NL excavator & float hire for trench reclamation

VMS Consultants Inc. Corner Brook, NL technical & professional assistance; core logging

Wade Company Limited St. John's, NL printing & duplication

Wellmaster Tilsonburg, ON PVC pipe supplies for borhole surveys

EMPLOYEES

Name Affiliation Hometown Mandays Activities & Duties

Andrea Devereaux Altius Resources Inc. Torbay, NL 142.50 core logging, reporting, drafting, data synthesis, drilling

supervision, planning, logistics, geology, sampling

Chris Davis Altius Resources Inc. Wesport, NL 3.00 technical assistance, core handling, sampling

Dale O'Reilly Altius Resources Inc. Mount Pearl, NL 31.50 planning, logistics, geology, drilling supervision, reporting

Edison Keats Altius Resources Inc. Buchans, NL 70.75 technical assistance, core handling, sampling, borehole

surveying, trail & site preparation

Jason Flight Altius Resources Inc. Goulds, NL 13.00 reclamation review & reporting

Jessica Ivany Altius Resources Inc. Conception Bay South, NL 18.00 reclamation review & reporting, data compilation

Lloyd King Altius Resources Inc. Goulds, NL 1.00 reclamation

Mervin Davis Altius Resources Inc. Wesport, NL 73.50 technical assistance, core handling, sampling, borehole


Rod Churchill Altius Resources Inc. Portugal Cove, NL 2.25 program accounting, lands management, logistics, drafting

Irvine Annesley JNR Resources Inc. Sasktoon, Sk 18.00 planning, logistics, geology

Richard From JNR Resources Inc. Sasktoon, Sk 6.00 technical assistance, core handling, sampling, borehole


TOTAL MANDAYS 379.50

STATEMENT OF EXPENDITURES

Expenditure Amount 007897M 016221M

Accommodations 20,558.70$ 18,314.88$ 2,243.82$

Analytical Charges 24,397.20$ 21,134.20$ 3,263.00$

Drilling Services 175,472.75$ 156,321.30$ 19,151.45$

Drilling Supplies: PVC Piping 6,691.44$ 5,961.12$ 730.32$

Equipment Rental 14,700.00$ 13,095.61$ 1,604.39$

Field Supplies 3,069.16$ 2,734.19$ 334.97$

Meals 887.90$ 790.99$ 96.91$

Miscellaneous 134.20$ 119.55$ 14.65$

Permitting Costs (fording) 200.00$ 178.17$ 21.83$

Printing 570.00$ 507.79$ 62.21$

Shipping & Freight 3,946.24$ 3,515.54$ 430.70$

Technical & Professional Support 31,467.96$ 28,033.48$ 3,434.48$

Telephone Communications 616.43$ 549.15$ 67.28$

Travel: Airfare (field crew changes) 3,946.54$ 3,515.81$ 430.73$

Travel: Fuel 4,185.19$ 3,728.41$ 456.78$

Travel: Leasing/Rentals 5,218.90$ 4,649.30$ 569.60$

Travel: Mileage Claims 2,349.93$ 2,093.45$ 256.48$

Trench Reclamation 3,370.00$ 3,002.19$ 367.81$

Wages & Employee Benefits 136,193.93$ 121,329.45$ 14,864.48$

Subtotal 437,976.47$ 389,574.60$ 48,401.87$

15% Overhead 65,696.47$ 58,436.19$ 7,260.28$

TOTAL 503,672.94$ 448,010.79$ 55,662.15$

…A2

APPENDIX 2. DIAMOND DRILL HOLE DATABASE

Diamond Drill Hole Database; 2009 Drilling Campaign

UTM Zone: NAD27

DDH

No.License

No.

UTM

Easting

UTM

Northing

UTM

Accuracy (m)

EOH

(m)

DDH

Azimuth

Dip at

Collar

Overburden

Depth (m)

Geological Unit

at Collar

DDH

Probed

Maximum

Probe Depth (m)

PVC Pipe

in DDH

Casing

in DDH

PVC Pipe Above

Ground Extension (m)

Anomalous Interval(s) /

Lithology

Radiometric Peak /

Average (CPS)

RB‐09‐226 007897M 494,006 5,472,548 2 40.00 0 ‐90 7.36 Su YES 37.49 YES NO 0.30 14.14 ‐ 15.25m / Su

17.19 ‐ 18.03m / Su

19.41 ‐ 21.61m / Su

27.06 ‐ 28.47m / St

99/54

150/80

142/67

91/52

RB‐09‐227 007897M 493,268 5,472,549 3 51.00 0 ‐90 9.09 St YES 49.04 YES NO 0.30 11.88 ‐ 12.23m / St

28.73 ‐ 29.39m / St

35.95 ‐ 36.67m / Sm

36.94 ‐ 37.37m / Sm

42.75 ‐ 43.21m / Sm

142/74

120/65

141/66

94/55

94/59

RB‐09‐228 007897M 493,516 5,472,852 3 51.00 0 ‐90 4.83 Su YES 48.99 YES NO 0.20 3.49 ‐ 3.92m / OB

8.50 ‐ 9.06m / Su

9.26 ‐ 11.00m / Su

11.65 ‐ 17.14m / Su/Mu

17.28 ‐ 18.25m / Mu

21.61 ‐ 22.23m / Mu

22.79 ‐ 23.06m / Mu

31.07 ‐ 31.45m / St

48.58 ‐ 48.99m / St

80/53

109/66

104/61

143/65

84/55

108/54

90/61

89/57

79/57


3.92 ‐ 5.25m / OB/Su

6.74 ‐ 7.95m / Su

8.47 ‐ 10.09m / Su

10.96 ‐ 11.70m / Su

12.08 ‐ 12.68m / Su

13.00 ‐ 13.77m / Su/Mu

14.34 ‐ 16.65m / Mu

18.59 ‐ 18.90m / Mu

21.71 ‐ 22.27m / Mu

23.17 ‐ 23.91m / St

24.01 ‐ 24.86m / St

39.53 ‐ 40.03m / Sm

40.36 ‐ 40.98m / Sm

42.85 ‐ 43.32m / Sm

43.77 ‐ 44.00m / Sm

46.53 ‐ 47.02m / Sm

131/75

107/56

232/94

788/230

120/63

88/54

92/55

219/83

112/55

90/57

93/57

89/54

119/68

119/70

128/72

90/65

106/64

RB‐09‐230 016221M 492,995 5,473,181 3 101.00 0 ‐90 6.46 Su YES 39.35 YES NO 0.15 ‐‐ ‐‐


8.43 ‐ 8.83m / Su

10.88 ‐ 11.75m / Su

12.35 ‐ 13.55m / Su

13.78 ‐ 16.02m / Su/Mu

16.49 ‐ 17.19m / Mu

19.76 ‐ 20.40m / Mu

13.78 ‐ 15.47m / Su

20.83 ‐ 25.75m / Mu

131/75

97/54

113/60

95/56

115/59

104/56

90/60

115/61

100/53

RB‐09‐232 016221M 492,967 5,472,087 5 82.50 32 ‐45 9.70 Mu20 YES 78.48 YES NO 0.20 15.86 ‐ 16.23m / Mu

25.46 ‐ 25.95m / Mu

26.60 ‐ 27.91m / Mu

30.38 ‐ 34.14m / Mu

38.82 ‐ 44.89m / Mu/St

46.93 ‐ 47.52m / St

48.12 ‐ 48.54m / St

49.43 ‐ 50.54m / St

60.50 ‐ 60.94m / St

64.62 ‐ 67.42m / St

68.05 ‐ 68.82m / St

69.24 ‐ 70.23m / Mm

70.77 ‐ 72.18m / Sm

84/64

87/54

92/54

111/53

202/90

126/65

99/56

96/57

137/78

151/73

100/61

127/61

102/63

Page 1 of 3


UTM Zone: NAD27

DDH

No.License

No.

UTM

Easting

UTM

Northing

UTM

Accuracy (m)

EOH

(m)

DDH

Azimuth

Dip at

Collar

Overburden

Depth (m)

Geological Unit

at Collar

DDH

Probed

Maximum

Probe Depth (m)

PVC Pipe

in DDH

Casing

in DDH

PVC Pipe Above



Lithology

Radiometric Peak /

Average (CPS)

RB‐09‐233 007897M 493,057 5,472,058 5 40.58 32 ‐45 5.31 Su30 YES 38.04 YES NO 0.15 2.97 ‐ 3.57m / OB

3.97 ‐ 4.70m / OB

87/54

115/58

RB‐09‐234 007897M 493,099 5,472,015 5 41.58 032 ‐45 4.76 Su30 YES 39.50 YES NO 0.15 10.84 ‐ 11.07m / Su

15.35 ‐ 16.44m / Su

16.67 ‐ 16.96m / Su

108/63

108/63

106/62

RB‐09‐235 007897M 493,112 5,472,062 5 40.20 212 ‐45 5.65 Su30 YES 37.74 YES NO 0.15 6.90 ‐ 7.82m / Su

13.93 ‐ 14.43m / Su

23.30 ‐ 23.98m / Su

87/53

85/54

87/53

RB‐09‐236 007897M 493,073 5,472,096 5 40.22 212 ‐45 5.14 Su30 YES 37.94 YES NO 0.19 1.64 ‐ 5.70m / OB/Su

35.88 ‐ 36.49m / Mu

1006/245

97/52

RB‐09‐237 007897M 493,295 5,472,592 5 26.00 212 ‐45 10.90 St YES 11.86 YES NO 0.22 8.67 ‐ 10.05m / OB 167/81

RB‐09‐238 007897M 493,322 5,472,635 2 23.14 212 ‐45 8.00 Mu YES 21.32 YES NO 0.15 ‐‐ ‐‐

RB‐09‐239 007897M 493,349 5,472,670 5 75.25 212 ‐45 7.43 Su YES 72.66 YES NO 0.20 45.26 ‐ 47.10m / St

51.49 ‐ 52.12m / St

62.80 ‐ 63.44m / Sm

96/56

92/54

98/60

RB‐09‐240 007897M 493,238 5,472,647 6 49.92 212 ‐45 7.07 Su YES 47.06 NO NO 0.30 ‐‐ ‐‐

RB‐09‐241 007897M 493,256 5,472,674 5 59.98 212 ‐45 9.00 Mu YES 22.32 YES NO 0.19 7.71 ‐ 9.28m / OB/Mu

16.30 ‐ 19.06m / Mu

110/58

132/73

RB‐09‐242 007897M 493,195 5,472,675 5 41.76 212 ‐45 6.00 Su YES 38.92 YES NO 0.36 9.91 ‐ 12.30m / Su

14.43 ‐ 19.68m / Mu

21.64 ‐ 22.83m / Su

23.05 ‐ 23.60m / Mu

23.84 ‐ 25.46m / Mu

122/62

158/65

98/53

81/54

90/52


6.25 ‐ 6.95m / Su/Mu

8.44 ‐ 8.79m / Mu

9.46 ‐ 11.40m / Mu

12.45 ‐ 12.94m / Mu

13.32 ‐ 16.96m / Mu

17.41 ‐ 18.16m / Mu

19.11 ‐ 20.13m / Mu

41.60 ‐ 42.48m / St

44.45 ‐ 44.84m / Sm

92/54

326/143

83/58

348/103

163/94

133/65

102/59

95/53

119/63

178/85

RB‐09‐244 016221M 492,956 5,472,743 6 30.22 0 ‐90 6.65 St NO ‐‐ YES NO 0.19 ‐‐ ‐‐

RB‐09‐245 007897M 493,024 5,472,192 5 80.16 212 ‐45 7.59 Mu20 YES 77.99 YES NO 0.17 15.60 ‐ 17.11m / Mu

35.89 ‐ 38.84m / Mu

40.05 ‐ 40.49m / Mu

41.29 ‐ 43.03m / Mu/Sm

43.32 ‐ 44.41m / Sm

50.85 ‐ 51.34m / Sm

51.62 ‐ 52.20m / Sm

63.72 ‐ 64.50m / Sm

65.86 ‐ 71.11m / Sm/Ml

73.27 ‐ 74.05m / Sl

101/57

109/56

104/57

154/77

166/84

105/55

95/58

89/56

140/69

85/55


7.74 ‐ 8.29m / Su

8.70 ‐ 8.94m / Su

13.09 ‐ 13.68m / Su

39.58 ‐ 40.64m / Sst

40.99 ‐ 41.45m / Sm

110/62

117/66

139/72

104/56

102/60

112/64

RB‐09‐247 007897M 496,761 5,477,199 5 24.00 0 ‐90 5.65 Su(D) YES 22.47 YES NO 0.10 6.04 ‐ 6.59m / Su

10.20 ‐ 10.65m / Su

14.87 ‐ 15.57m / Su/Mu

104/60

87/57

87/54


29.01 ‐ 30.42m / Mu

62.27 ‐ 62.59m / RB

71.38 ‐ 71.65m / RB

72.79 ‐ 73.19m / RB

148/88

180/70

89/56

88/60

124/64

Page 2 of 3


UTM Zone: NAD27

DDH

No.License

No.

UTM

Easting

UTM

Northing

UTM

Accuracy (m)

EOH

(m)

DDH

Azimuth

Dip at

Collar

Overburden

Depth (m)

Geological Unit

at Collar

DDH

Probed

Maximum

Probe Depth (m)

PVC Pipe

in DDH

Casing

in DDH

PVC Pipe Above



Lithology

Radiometric Peak /

Average (CPS)

RB‐09‐249 007897M 496,583 5,477,509 5 49.52 0 ‐90 7.10 Mst YES 48.30 YES NO 0.32 7.32 ‐ 7.87m / Mu 98/57

RB‐09‐250 007897M 496,632 5,477,479 6 68.45 305 ‐45 8.88 Mst YES 66.19 YES NO 0.18 8.14 ‐ 9.30m / OB/Mst

12.98 ‐ 13.57m / Mst/Sst

35.56 ‐ 36.96m / Mst/Sst

99/55

116/62

256/118

RB‐09‐251 007897M 496,774 5,477,389 5 71.00 305 ‐45 5.70 Su(D) YES 66.70 YES NO 0.36 2.10 ‐ 5.72m / OB

6.47 ‐ 6.85m / Su

7.25 ‐ 9.75m / Su/Mu

20.55 ‐ 20.99m / Mu

22.34 ‐ 23.00m / Mu

46.51 ‐ 46.83m / Sst

52.68 ‐ 53.42m / Sst

123/63

96/58

287/110

96/54

85/55

85/56

140/77

RB‐09‐252 007897M 496,976 5,477,402 6 50.03 0 ‐90 4.26 Sst YES 48.07 No NO ‐‐ 4.55 ‐ 4.93m / Su

8.13 ‐ 8.84m / Su

125/72

132/81

RB‐09‐253 007897M 496,811 5,477,504 4 48.14 0 ‐90 6.00 Sst Yes 47.50 YES NO 0.40 25.49 ‐ 27.43m / Mst 412/138

RB‐09‐254 007897M 496,669 5,477,599 4 50.00 0 ‐90 8.58 Mu YES 48.45 YES NO 0.40 20.72 ‐ 21.03m / Mu 82/57

RB‐09‐255 007897M 496,547 5,477,497 5 47.00 0 ‐90 4.98 Mu YES 45.11 YES NO 0.48 7.55 ‐ 7.99m / Mu

41.23 ‐ 41.82m / Sl/RB

89/61

117/64

RB‐09‐256 007897M 496,586 5,477,469 6 70.00 305 ‐45 8.05 Su(D') YES 68.19 YES NO 0.30 12.36 ‐ 13.05m / Su

36.34 ‐ 37.38m / Mu

90/57

656/256


3.81 ‐ 5.08m / OB

10.80 ‐ 11.76m / Mu

14.92 ‐ 15.31m / Mu

88/64

110/66

84/55

82/54

RB‐09‐258 007897M 496,748 5,477,370 7 60.63 305 ‐45 5.40 Su YES 58.18 NO YES ‐‐ 3.77 ‐ 4.77m / OB

5.04 ‐ 6.91m / OB/Su

111/61

124/66

RB‐09‐259 007897M 496,552 5,477,517 6 61.93 325 ‐45 6.90 Mu YES 60.62 YES NO 0.30 10.33 ‐ 11.31m / Mu

33.21 ‐ 33.82m / Sst

36.35 ‐ 36.69m / Sst

40.43 ‐ 41.40m / Sst

57.54 ‐ 59.68m / Sl/RB

99/63

99/61

84/53

104/63

106/62

RB‐09‐260 007897M 496,534 5,477,689 6 41.00 0 ‐90 7.82 Su YES 39.63 YES YES 0.30 36.77 ‐ 37.58m / RB 141/74


6.39 ‐ 8.70m / OB/Su

13.18 ‐ 14.28m / Su/Mu

14.46 ‐ 15.61m / Mu

35.66 ‐ 35.94m / Sst

90/58

128/61

99/52

95/55

106/64

RB‐09‐262 007897M 497,117 5,477,074 6 20.33 300 ‐45 8.42 RB Fm YES 19.41 YES NO 0.74 11.12 ‐ 11.38m / RB

13.42 ‐ 14.27m / RB

92/61

134/82

RB‐09‐263 007897M 497,106 5,477,083 6 18.80 0 ‐90 9.11 RB Fm YES 16.44 YES NO 0.20 ‐‐ ‐‐

1958.18 Total Metreage (m)

**NOTES** (1) Bold "Yes" responses in PVC Pipe Column indicate that pipe does not go to EOH

(2) Bold "Yes" responses in DDH Probed Column indicate that DDH was not surveyed to EOH

Page 3 of 3

…A3

APPENDIX 3. DIAMOND DRILL LOGS

Hole No: RB-09-226

Easting/ Northing: 494,006 5,472,548

Dip at Collar: -90Bearing: 0

Total Depth (m): 40

Core Size: BQTK

Date Drilled: 26-Aug-09

License: 007897M

Contractor: New Valley Drilling

Logged By: Andrea Devereaux

Diamond Drill Core Log Sheet Number: 1 of 2

mE / mN

To (m) Formation DescriptionFrom (m) Litho UnitMagnetic

SusceptibilityOxidationNumberCPS

Test Depth (m)

Dip Magnetic Bearing

Corrected Bearing Property: Rocky BrookGrid Coordinates:

Member

27-Aug-09 -

0.00 7.36 OB Overburden OB

7.36 25.09 HF Greyish to greenish to buff coloured…mg to cg sst to pebble cgl with minor slt and mst sections…interval is unoxidized and has a reduced appearance overall… kaolinite alteration is present throughout both as alteration of k-fsp and as pore-fill…calcareous…fg organic detritus throughout is both diss and stratified (at ~90° TCA)…fg py throughout is most often associated with organic material…hosts moderate greenish coloured mst rip-up clasts throughout often with associated py mineralization…cgl’s are moderately well sorted to poorly sorted with clasts ranging in size from granule (<0.5cm diameter) to 1-2cm diameter and locally up to 8cm diameter…clasts are sub-rounded to sub-angular….vuggy texture throughout that is most prominant in cgl sections…

Su 65 - 103Su -1 - 10.00 - 0.02

from 7.36 – 8.12m core is broken and has a blocky appearance…

at 9.10m a thin (~1 – 2 mm thick) coal seam oriented sub-parallel TCA with significant organic wisps and blebs in area…py associated with this organic detritus…from 9.80 - 9.92m sst is fractured at ~25° TCA

from 13.44 – 13.56m is a reduced, fg sst bed oriented ~90° TCA with fg organic detritus…reduction laminae at ~90° TCA…cgl has reduction overprinting at 16.83 – 16.95m…coal seam present…from 17.30 – 25.09m greyish to greenish coloured, mg – cg sst has a more reduced appearance…sst hosts abundant muscovite throughout…hosts abundant fg organic detritus that is locally stratified…greenish, strongly reduced sections are present locally and surround organic detritus…from 20.11 – 20.22m sst is fractured sub-parallel TCA…

from 20.65 – 21.64m and 23.16 – 24.26m sst is tan-buff and has a mottled appearance…at 21.56 – 21.59m sst is fractured at ~45°TCA...at 21.64m is a mst bed at ~30°TCA….from 21.62 – 23.16m silty mst to slt is strongly reduced and has a stratified appearance….hosts abundant fg organic detritus throughout….lower bedding measurement at ~90° TCA…from 24.77 – 24.80m greenish, reduced slty mst section with angular mg – cg qtz and fsp grains…at ~90° TCA…grades into a cg sst beneath that is oxidized with some greenish intermixed mud…sst is vuggy….lower contact is sharp at 25.09m and is at ~70° TCA

25.09 38.16 HF Reddish-brown clayey to silty mst with lesser slt and fg-mg sst…strongly oxidized with only minor greenish reduction as spots and wisps locally…mst hosts moderate carbonate caliche ranging in size from ~1mm up to 2cm diameter and locally up to 5cm diameter…caliche are tan-buff to reddish-brown in colour...caliche-rich sections are highly disaggregated and often only caliche recovered…

Mu 59 - 91Mu -1 - 40.02 - 0.08

from 25.09 – 25.18m mst is greenish and strongly reduced (contact with overlying sst Mbr)…

from 25.97 – 30.01m cg sst bed at ~90 TCA…

from 29.48 – 29.62m mst is fractured(?) at ~20 TCA…

from 32.67 – 33.05m is a reddish-brown slt to fg sst…micaceous…

from 33.57 – 33.74m silty mst…strongly oxidized with moderate greenish, blotchy and wispy reduction…

RB-09-226

To (m) Formation Description

Sheet Number: 2 of 2

Litho UnitMagnetic

SusceptibilityOxidationNumberFrom (m) CPSMember

25.09 38.16 from 33.74 – 34.76m fg – mg sst has a mottled appearance (hematite being overprinted by reduction)…core is fractured parallel TCA from 33.87 – 34.76m…from 34.76 – 38.16m clayey to silty mst and minor slt that is locally nodular…blotchy oxidation and reduction (reduction mottles oxidation)…from 37.16 – 37.56m muddy section is partially disaggregated…

lower contact is sharp at ~90° TCA and is reduced

38.16 40.00 HF Greyish…cg – vcg sst…massive…abundant fg diss organic detritus that is locally stratified…minor kaolinite alt of fsp…tr fg diss py that is often associated with organic trash…EOH

St 60 - 87St -1 - 40.01 - 0.04

0.20m of core is missing from 16.00 - 19.00m; 0.10m of core is missing from 22.00 - 25.00m.EOH

HOLE GEOCHEMISTRY

ToFrom Length Sample No. Lithology

(m)(m) (m)

17.61 0.42 292017.19 Su

18.03 0.42 292117.61 Su

19.96 0.55 292219.41 Su

20.51 0.55 292319.96 Su

21.06 0.55 292420.51 Su

21.61 0.55 292521.06 Su

RB-09-226

Hole No: RB-09-227



Total Depth (m): 51

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

28-Aug-09 -

0.00 9.09 OB Overburden. HF sst and exotic (rhyolite and gabbro) boulders and cobbles. HF sst boulder is hematitized.

OB

9.09 30.00 HF Greyish to tan buff…cg – vcg sst that locally grades to granule – pebble cgl…normally graded (right way up)…micaceous…minor charcoal-grey to greenish mst sections (<10cm thick)…sst/cgl is characterized by the abundance of fg organic detritus that is diss and stratified throughout…abundant organic trash (wispy blebs and coal fragments)…local muddy to silty sections…grey and greenish coloured mst rip-up clasts throughout…significant fg py locally that is nodular and as small (<1cm – 2 cm) anhedral masses often surrounding organic trash… abundance of py may be the cause of IP Anomaly(?)…minor fg oxidized sulphides (<1%)…minor kaolinite alt of fsp’s throughout…

St 54 - 91St -1 - 30.00 - 0.02

from 9.86 – 10.01m sst is broken and fractured…fractures are at 60 – 70° TCA and parallel mst laminae…from 10.44 – 10.49m sst is fractured at ~35° TCA…

at 10.53m and 10.63m, core is broken at 50 and 60° TCA respectively…

from 12.99 – 13.26m a fg, beige coloured clay (dickite?) occurs as mm-scale stratifications at ~65° TCA…non-calcareous…at 13.44m is a 0.5cm thick coal-seam…from 13.42 – 13.44m fg py is abundant…

from 14.65 – 14.77m charcoal-grey muddy sst section…organic-rich…

from 14.77 – 14.91m greyish sst hosts abundant fg diss organic detritus and a coal seam…abundant fg py as anhedral masses and filling pore spaces of sst…from 15.16 – 15.37m greenish-grey mst bed at ~50° TCA that becomes organic-rich at the base of the section…from 27.15 – 28.10m significant fg py accumulations with tr cpy…py accumulations range from <0.5cm to >3cm in length… sst is fractured at 28.14 – 28.23m at ~25° TCA…at 28.71m sst is fractured…strong reddish-brown hematite along fracture surface with lesser, orangish-brown diss Fe-carb(?) further away from fracture…coal seam along fracture surface…minor greenish-yellow alteration (limonite?)…hematite has a purplish hue on fracture surface (manganese stain?)…lower contact is sharp at ~90° TCA

30.00 30.64 HF Greenish-grey to charcoal-grey mst that grades into a muddy fg sst…micaceous…organic-rich…lower contact is sharp at ~90° TCA

Mm 74 - 93Mm -10.02 - 0.06

RB-09-227



Litho UnitMagnetic


30.64 51.00 HF Reddish-brown to tan-buff in colour…cg – vcg sst that locally grades to granule – pebble cgl…interval is characterized by a weak to moderately strong, mottled/pervasive and mottled/stratified reddish-brown hematite throughout…a younger, bright red hematite overprints locally and is often as fg disseminations, stratifications and blotches/spots (less abundant)…hematite is occasionally very dark and has a purplish appearance…hematite disease most prominent towards bottom of ddh (39.44 – 51.00m)…an orangish alteration (Fe-carb?) overprints locally…micaceous…minor kaolinization of fsp’s throughout…weakly to moderately calcareous…organic trash locally throughout (most abundant towards top of interval (until approx 35.40m)…minor mst rip-up clasts throughout…sst is locally muddy (both greenish and reddish-brown intermixed mud)…from 30.64 - ~32.20m is non to weakly oxidized

Sm 65 - 107Sm 1 - 40.01 - 0.03

from 34.43 – 34.46m is a large vug in cg sst…appears to be a result of dissolution of carbonate…dark red to purplish hematite filling vug…from 34.96 – 35.15m is a muddy sst section…from 34.96 – 35.01m is mst…

from 36.00 – 36.46m and 36.72 – 36.86m sst is fractured sub-parallel TCA…no visible alteration or mineralization associated with fracture… fracture is underdeveloped from 36.86 – 36.89m…at 37.58m a thin (~1cm thick) greenish coloured mst at ~75° TCA……micaceous…

from 38.29 – 38.36m granule cgl has a muddy matrix…from 38.34 – 36.36m cgl is partially broken and disaggregated…possible fracture at 38.30m at ~90° TCA…strong reddish-brown hematite along fracture surface…from 38.49 – 38.51m pebble cgl is partially disaggregated…

at 40.08m strongly hematitized fracture at ~60° TCA that has an oily appearance…hematite is a brighter reddish-brown and margins of fracture (~5cm on each side) are hematitized as well…at 40.94m sst is fractured at ~90° TCA…strong purplish coloured hematite along fracture surface…an orangish Fe-carb(?) alteration on outskirts of hematite alt…at 40.94 - 41.56m, very intense, dark brown to purplish, stratified hematite…stratifications at 70 – 75° TCA…has a corrosive appearance…fractures at 41.23m, 41.57m, 41.65m and 41.95m between 70 – 90°…sst is very micaceous, has intermixed reddish and greenish coloured mud…fracture at 41.57m has moderate reddish hematite along fracture surface…from 45.00 – 45.08m sst is broken and fractured at ~30° TCA…

from 46.10 – 46.13m possible fault gouge(?)…greenish mst with cg-vcg angular grains of qtz and fsp that resemble adjacent vcg sst...possible fault at ~90° TCA…from 49.65 – 49.73m disaggregated pebble-cobble cgl…upper fracture surface at ~65° TCA and has strong reddish-orange hematite along surface…from 50.05 – 50.12m and 50.23 – 50.39m sst is fractured at ~25° TCA…hosts underdeveloped fractures (also at ~25° TCA) adjacent to these fractures…from 50.12 – 50.16m a fracture at ~65° TCA is very strongly hematitized (complete replacement to hematite vein?) and has an angular to sub-rounded qtz and fsp grains…fault gouge(?)…EOH

RB-09-227



Litho UnitMagnetic


0.18m of core is missing from 9.00 - 12.00m; 0.10m of core is missing from 12.00 - 15.00m; 0.08m of core is missing from 15.00 - 18.00m; 0.06m of core is missing from 33.00 - 36.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

12.23 0.35 292611.88 St

29.39 0.66 292728.73 St

36.67 0.72 292835.95 Sm

43.21 0.46 292942.75 Sm

RB-09-227

Hole No: RB-09-228



Total Depth (m): 51

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

29-Aug-09 -

0.00 4.83 OB Overburden. HF sst cobbles OB

4.83 14.14 HF Tan-buff to beige to greyish cg – vcg sst and pebble to cobble polymictic cgl (locally colourful) with lesser greyish to dark grey-green mst to siltstone sections locally…moderate fg organic detritus (wisps and blebs) that is locally stratified…kaolinite alteration both as pore-fill and as fsp alteration throughout…non-calcareous to calcareous…fsp’s are an orangish colour…locally micaceous…has intermixed beigish coloured clay (dickite?) locally that also occurs as laminae…core is moderately broken and locally has a blocky appearance…sst has is a beige colour from 4.83 - ~7.25m due to the abundant intermixed beige clay (dickite?)…a bedding instance at 8.07m at ~80° TCA…

Su 66 - 103Su -1 - 00.01 - 0.09

at 9.04m sst is fractured and has possible organic stain along fracture surface…

from 9.04 – 14.14m sst hosts more abundant organic trash and has a reduced (greyish) rather than neutral (tan-buff) appearance…local minor fg py associated with organic trash…from 9.31 – 9.33m sst is fractured at ~35° TCA and has patchy organic stain on fracture surface…from 9.80 – 10.28m cg – vcg sst has abundant intermixed greenish mst…mud content increases from 9.80 – 10.28m and dickite(?) is also more abundant within this same section…minor small (<1cm – 2cm diameter) rusty patches within sub-interval…possible oxidized py although none observed…underlying mst exhibits cross-bedding…from 10.28 – 12.64m dark greenish-grey mst to slt…fg diss organic trash…micaceous…good recovery and intact…slt is fractured at 11.23m at ~30° TCA…mst is very organic-richand has a charcoal-grey appearance locally…from 12.18 – 12.20m is a coal seam...sst is fractured at 13.30 – 13.34m at ~35° TCA…

from 13.39 – 14.17m is another clayey to silty mst section…dark greenish to locally charcoal-grey coloured…very minor remnant reddish-brown oxidation present in places…weathered and partially disaggregated…possible limonitic alteration present locally throughout (yellowish alteration)…lower contact is sharp at 14.14m…(core at contact is rounded from coring, thus no measurement taken)

14.14 26.10 HF Reddish-brown to greenish coloured…dominantly clayey to silty mst with minor mg – cg sst sections locally…minor carbonate caliche throughout (<0.5cm – 2cm diameter)…caliche is locally abundant…dominantly oxidized with significant greenish reduction overprinting locally…core is somewhat weathered and is broken and partially disaggregated throughout…

Mu 65 - 98Mu -1 - 40.04 - 0.19

the upper contact, from 14.14 – 15.94m is a reduced, greenish mst that has moderate yellowish alteration (limonite?) locally…a buff to reddish-brown coloured fragmented carbonate caliche(?) section from 15.20 – 15.24m is at ~55° TCA and has moderate reddish-brown to greenish intermixed mud…moderate remnant oxidation present throughout sub-interval…from 20.81 – 22.10m is a tan-buff to greenish to reddish-brown granular mst section (cg sst with significant intermixed mud) and smaller (~2 – 5cm thick) mst sections which appear to be bedded at ~80° TCA…a band of limonitic weathering at 21.36 – 21.37…the base of this sub-interval (from 21.43 – 22.10m) is comprised of small, buff to reddish-brown coloured caliche (not all react with 10% HCl) with intermixed greenish mud and some granular sst sections (cg qtz and fsp grains in mst)…

RB-09-228



Litho UnitMagnetic


14.14 26.10 from 22.10 – 24.00m and 25.16 – 26.06m similar to 15.94 – 20.81m except for fact that oxidation is being overprinted by greenish reduction…from 24.00 – 25.16m dark greenish to buff coloured siltstone (from 24.00 – 24.17m) that grades into fg – mg sst…hosts abundant fg organic detritus that is disseminated and locally stratified throughout…micaceous…a fracture at ~40° TCA also spans this sst section…stratifications are at ~70 – 85° TCA…lower contact is sharp at ~80° TCA and is reduced clayey mst

26.10 51.00 HF Greyish to tan-buff coloured…cg – vcg sst that locally grades to granule/pebble cgl and in rare instances cobble cgl with lesser mst and slt sections…unit is characterized by the overall reduced appearance and the abundance of organic trash ranging from fg disseminations to large, >5cm, coal fragments with abundant fg masses of py that are often associated with these fragments (commonly 1 – 2 cm rims surrounding trash and locally up to 6cm)…minor kaolinite as pore fill and as alteration of fsp’s throughout…hosts minor and locally abundant charcoal-grey mst rip-up clasts throughout…sst is locally a tan-buff colour as a result of abundance of peach-pink fsp grains…

St 59 - 94St -10.00 - 0.04

from 26.10 – 27.13m, 28.67 – 30.00m and 33.25 – 33.62m core is broken and has a blocky appearance…minor greenish-grey clayey mst sections at 30.80 – 31.02m, 31.30 – 31.32m (at ~80° TCA) and 32.95 – 33.22m (at ~65° TCA)…at 32.58m, an underdeveloped fracture at ~70° TCA followed by a fracture at 32.63m that has an organic stain(?) on fracture surface…possible fracturing at 33.61m (55° TCA), along a ~1cm thick coal seam…significant fg py mineralization surrounding fragment…from 35.01 – 35.08m sst is fracture at ~20° TCA…

at 36.18m and 36.23m sst is fractured at 50° and 65° TCA respectively…hosts minor rusty patches overprinting (oxidized sulphides?)…from 37.35 – 37.44m sst is fractured…sst is very micaceous and hosts abundant fg organic detritus…at 41.62m sst is fractured at 30° TCA…

at 41.86m trace malachite staining…

from 42.50 – 42.77m is a section of highly broken and partially disaggregated cgl…

from 44.28 – 44.36m sst is fractured sub-parallel TCA…possible fault as sst is crushed(?)/disaggregated…at 44.53m coal fragment (~4cm x 2cm) with a 1.5cm rim of fg py surrounding it…

from 50.17 – 50.69m is a charcoal-grey silty mst to silt section with abundant fg organic detritus that is stratified throughout…stratifications are at ~90° TCA…this section is possibly the Mm Member, making the underlying sst the Sm Mbr…sst from 50.69 – EOH is unoxidized and thus is considered St here...EOH

RB-09-228



Litho UnitMagnetic


0.10m of core is missing from 9.00 - 12.00mEOH

HOLE GEOCHEMISTRY


(m)(m) (m)

9.06 0.56 29308.50 Su

9.84 0.58 29319.26 Su

10.42 0.58 29329.84 Su

11.00 0.58 293310.42 Su

12.15 0.50 293411.65 Su

12.65 0.50 293512.15 Su

13.15 0.50 293612.65 Su

13.65 0.50 293713.15 Su

14.15 0.50 293813.65 Su

14.65 0.50 293914.15 Mu

15.15 0.50 294014.65 Mu

15.65 0.50 294115.15 Mu

16.15 0.50 294215.65 Mu

RB-09-228

Hole No: RB-09-229



Total Depth (m): 51.19

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

30-Aug-09 -

0.00 5.10 OB Overburden. OB

5.10 13.27 HF Tan-buff to reddish to greenish in colour…cg – vcg sst with minor mst to siltstone sections…moderate greenish intermixed mud throughout…moderate kaolinite alteration of fsps…micaceous…sst is vuggy throughout with vugs locally reaching up to 3cm in length…weakly calcareous…fsp’s are a pinkish-peach colour…fg diss orgranic detritus throughout…

Su 69 - 230Su -1 - 30.00 - 0.07

from 5.10 – 9.00m sst has an unoxidized (neutral) appearance…core is highly broken and has a blocky appearance…core is broken and ~45 – 90° TCA throughout with most between ~70 – 90° TCA…at 8.21m is a large vug in sst that has a yellow-green clay in parts of vug (up to 130 CPS on RS-125 handheld, Assay of 1.0% K, 2.2 ppm U and 7.9 ppm Th)…from 8.76 – 9.00m vcg sst hosts abundant brownish-green mst rip-up clasts and intermixed beigish clay throughout that gives the sst a grungey yellowish-beige colour…from 8.76 – 8.80m and 8.91 – 9.00m, possible crush zones(?)…mst (greenish to dark grey and reddish-brown mst) with angular cg – vcg qtz and fsp grains throughout…from 9.00 – 10.37m cg to vcg sst hosts weak to moderate pervasive and blotchy reddish hematite…hosts minor bright white specks of kaolinite alteration of fsp’s throughout (more abundant than rest of unit)…vuggy…sst is fractured at 9.13m, 9.74m, 10.04m and 10.32m at ~70 – 75° TCA…from 10.37 – 13.27m is tan-buff cg – vcg sst with significant greenish, intermixed mud throughout that gives the sst a reduced appearance…hosts minor organic trash as wisps and specks…greenish and reddish-brown mst rip-up clasts throughout, though the reddish-brown are rare…from 10.91 – 11.06m sst hosts abundant reddish and greenish coloured mud…from 10.91 – 10.94m is a greenish clayey – silty mst bed at ~55° TCA with weak remnant reddish-brown oxidation…this sst/mst intermixture was the start of a radiometric anomaly that continues into the underlying mst section…radiometrics up to 180 CPS on GR-135 handheld (Assay 1.2% K, 9.9 ppm U, and 0.7ppm Th)…sst is bedded at ~75° TCA…the underlying mst (from 11.06 – 11.47m) is a greenish coloured clayey to silty section with minor reddish-brown mottled hematite within the first ~10cm of sub-interval…bedded at ~80° TCA…micaceous…locally has a charcoal grey appearance due to increased organic content…most anomalous section of ddh with >220 CPS on RS-125 handheld and it assayed 2.0% K, 14.7ppm U and 2.8ppm Th…from 12.88 – 13.27m greenish intermixed mud and mst rip-up clasts are abundant within the sst…underdeveloped fracture at 13.12 – 13.16m…partially disaggregated at 12.96m – 13.04m at mst rich areas…lower contact is sharp at ~75° TCA

13.27 22.80 HF Greenish to tan-buff to reddish-brown in colour…dominantly clayey to silty mst and slt with lesser mg-vcg sst sections…interval is characterized by the overall strongly reduced appearance with minor mottled hematitization locally…mst hosts minor to moderate buff to reddish-brown carbonate caliche throughout…caliche range from <0.5cm to 4cm diameter and locally carbonate veinlet-rich sections (up to 7cm thick) are present…mst is partially disaggregated in these caliche-rich sections…

Mu 64 - 144Mu -10.04 - 0.19

from 13.27 – 13.40m clastic carbonate section with abundant veinlets and significant intermixed greenish mud…

RB-09-229



Litho UnitMagnetic


13.27 22.80 from 15.96 – 17.81m slt and fg – mg sst has significant spotty green ‘chlorite’ alteration…this interval of sst also hosts abundant fg organic detritus that is diss, wispy and as bedding parallel laminations…laminations are at ~75 – 90° TCA…from 17.81 – 18.29m greenish mst has a granular appearance with abundant fg – cg fsp and qtz grains throughout (possible gouge?)…from 20.53 – 21.66m tan-buff to greenish coloured cg - vcg sst…calcareous to very calcareous…fg organic detritus throughout…locally very vuggy (dissolution of carbonate?)…vuggyness increases with depth within this sub-interval…sst appears to be bedded at ~90° TCA…lower contact is gradational…organic content (layers up to 1.5cm thick and wispy detritus) increases with depth as it grades into the underlying St Member

22.80 36.87 HF Greyish to buff coloured…cg–vcg sst that locally grades to granule–pebble cgl and lesser dark greenish to charcoal-grey mst and siltstone sections...sst locally hosts abundant dark greenish to charcoal-grey mst rip-up clasts…interval is characterized by abundant organic detritus throughout (wisps, fg disseminations, coal seams, and stratifications)…stratifications are between 35 – 90° TCA with most between 50 – 60° TCA…micaceous…minor to moderate clay development (kaolinite alteration of fsp’s and dickite(?)…interval hosts abundant fg disseminated py throughout…py mineralization is most abundant surrounding large organic trash (eg. coal seams or larger fragments)…local oxidized sulphides…tr cpy(?)…sst locally hosts abundant greenish-grey intermixed mud…

St 62 - 98St -10.01 - 0.14

at 24.24 – 24.34m and 24.50 – 24.54m sst is fractured at 25° and 35° TCA respectively…

at 24.68 – 24.70m and 24.72 – 24.74m sst is fractured at 45° and 50° TCA respectively…

at 24.82 – 27.39m dark greenish to charcoal-grey mst to slt section with beigish clay (dickite?) throughout…dark colour result of increased organic content…fairly intact…white carbonate veinlets (1 – 2mm thick) at 24.47m and 27.50m…micaceous…from 30.00 – 30.02m is a 2cm coal seam with abundant fg py in sst adjacent to coal and on coal seam itself…at ~70° TCA…from 30.34 – 30.48m sst hosts significant intermixed greenish-greyish intermixed mud and has a granular texture…from 30.45 – 30.48m as it is a muddy section with abundant cg–vcg angular to sub-angular qtz and fsp grains and trace nodular py (gouge?)…from 30.48 – 32.00m sst is cg-vcg…greyish in colour…has moderate kaolinite alteration and beigish clay…significant fg py (and tr cpy?) throughout sub-interval…py is locally stratified…from 32.00 – 33.80m sst is characterized by abundant dark green to charcoal-grey mst rip-up clasts throughout…from 35.64 – 35.75m dark greenish to charcoal-grey mst – slt section…

from 36.11 – 36.42m slt to cg sst hosts significant wispy organic detritus which are dominantly oriented parallel to bedding (~90° TCA)…lower contact is gradational with green mud becoming intermixed at base of unit…this member was truncated at this point due to Mm below, although it could possibly continue to ~42.00m if the following mst is not truly the Mm member

36.87 37.03 HF Dark greenish-grey mst…massive…similar to mst’s described in overlying St Mbr…from 36.98 – 37.00m coal seam at ~90° TCA…lower contact is sharp at ~65° TCA

Mm 66 - 85Mm -10.04 - 0.05

37.03 51.19 HF Reddish-brown to reddish to tan-buff…cg-vcg sst that locally grades to granule-pebble cgl…minor mst-slt sections throughout interval (<20cm thick)…minor to moderate kaolinite alteration of fsp’s that is visible as bright white specks…interval is characterized by a reddish-brown mottled/pervasive and mottled/stratified hematite alteration throughout…an intense, bright red pervasive hematite occurs locally, often near fractures/faults and rarely as hematite disease spots…despite intense oxidation present throughout, there are instances of organic trash throughout, even in strongly oxidized areas…

Sm 63 - 101Sm -1 - 40.00 - 0.22

RB-09-229



Litho UnitMagnetic


37.03 51.19 from 37.03 – 42.00m cg-vcg sst strongly resembles overlying St Mbr as this sub-interval is not oxidized and hosts minor organic debris…at 40.98m fracture is strongly oxidized (bright reddish to orangish hematite alteration of sst) and hematite bleeds into overlying sst from 40.93 – 40.98m…fracture is at ~90° TCA and has a greyish hematite alteration (specular hematite?) and an oily appearance (manganese stain?)…from 41.27 – 41.31m is a coalified wood fragment with fg py mineralization on coal fragment and in adjacent sst…from 41.93m to 51.19m hematite is pervasive (sst no longer resembles St Mbr)…

sst is fractured at 42.06 – 42.12m at ~85° and 65° TCA respectively…

crush zone(?) at 42.35 – 42.38m consisting of reddish-brown mst and sst grains (qtz and fsp) with moderately strong hematite alteration of crush zone and competent sst on either side…from 44.03 – 44.08m core is broken…

from 44.54 – 44.86m reddish-brown to greenish-grey mst with minor rusty brown overprinting (Fe-carb?)…locally has a granular texture…micaceous...appears to be bedded at ~60° TCA…at 46.16m sst is fractured at ~55° TCA and from 46.16 – 46.23m sst is fractured sub-parallel TCA…

from 46.98 – 47.07m sst is strongly hematitized…fracture at 47.05m is strongly hematitized (reddish-brown to greyish coloured hematite)...weakly corrosive hematite mineralization…up to 0.22 on magnetic susceptibility meter…from 48.38 – 48.70m sst has significant reddish-brown intermixed mud…from 48.57 – 48.70m is dominantly mst with angular to sub-angular qtz and fsp grains…gouge zone(?)...EOH

RB-09-229



Litho UnitMagnetic


0.08m of core is missing from 9.00 - 12.00m; 0.18m of core is missing from 12.00 - 15.00m; 0.10m of core is missing from 15.00 - 18.00m; 0.40m of core is missing from 18.00 - 21.00m; 0.22m of core is missing from 24.00 - 27.00m; 0.07m of core is missing from 39.00 - 42.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

7.35 0.61 29436.74 Su

7.95 0.60 29447.35 Su

9.01 0.54 29458.47 Su

9.55 0.54 29469.01 Su

10.09 0.54 29479.55 Su

11.70 0.74 294810.96 Su

14.80 0.46 294914.34 Mu

15.26 0.46 295014.80 Mu

15.72 0.46 295115.26 Mu

16.18 0.46 295215.72 Mu

16.65 0.47 295316.18 Mu

40.03 0.50 295439.53 Mu

40.98 0.62 295540.36 Mu

43.32 0.47 295642.85 Mu

47.02 0.49 295746.53 Sm

RB-09-229

Hole No: RB-09-230



Total Depth (m): 101

Core Size: BQTK


License: 016221M




mE / mN



Test Depth (m)



Member

01-Sep-09 -

0.00 6.46 OB Overburden. Gabbro boulder. OB

6.46 8.00 HF Reddish to pinkish cg – vcg sst…massive…interval is characterized by mottled/pervasive and mottled/stratified hematite throughout…moderate kaolinite alteration of fsp’s that exists as bright white specks in sst…minor white mica throughout…hematite is bright red and characteristic of the western side of the PML and occurs as fg disseminations…few instances of hematite disease in the last ~35cm of interval…

Su 72 - 78Su 20.00 - 0.01

sst is fractured at 7.66m and 7.81m at ~65 - 70° TCA…

lower contact is sharp (no measurement taken as core is rounded from drilling)

8.00 15.27 HF Reddish to pale green coloured…dominantly clayey to silty mst with minor muddy sst sections…interval is characterized by a strong reddish-rusty oxidation with minor pale green reduction spots…interval becomes more reduced with depth and a sandy section starts at ~13.50m…

Mu 53 - 94Mu -1 - 40.02 - 0.07

from 8.00 – 13.06m mst has an overall massive appearance…strong reddish-rusty oxidation with minor greenish reduction specks…micaceous…hosts reddish carbonate caliche locally throughout…caliche ranges from <0.5cm up to 5.0cm diameter…from 13.06 – 15.27m interval has significant intermixed mud with lesser interbedded mst sections…significant fg diss organic detritus visible in sandy sections…interval becomes more reduced (greenish) with depth…micaceous…towards base of interval (14.62 – 14.67m and 14.97 – 15.04m) cg sst sections are present and sst hosts a deep reddish, fg diss stratified/pervasive hematite…sst sections also have moderate kaolinite alteration…from 15.05 – 15.17m sst and muddy sst are fractured sub-parallel TCA…lower contact is sharp at ~85° TCA and is reduced

15.27 31.37 HF Tan-buff to reddish…dominantly cg-vcg sst that locally grades to granule-pebble and cobble cgl…minor thin (<5cm thick) mst sections locally…interval is characterized by a weak to strong mottled/pervasive, stratified, mottled/stratified hematite and local hematite disease (reddish fg diss hematite accumulations)…large reddish hematite blotches (~5cm diameter) are locally present from ~26.50m onwards…weak to moderate kaolinite alteration of fsp’s…micaceous…interval hosts significant greyish and lesser reddish-brown to greenish mst throughout both as rip-up clasts and intermixed mud…abundance of greyish mud locally gives the sst a grey appearance…locally vuggy…fsp’s are locally altered a peach to orangish colour…sst is moderately broken throughout and locally has a blocky appearance…fractures range from ~65 - 90° TCA with most between 70 – 80° TCA…fractures are often hematitized…qtz pebbles are locally bright white (vs. clear) and have a recrystallized appearance…despite the fact that this interval is termed the St Mbr here, no organic trash was observed throughout the interval…possible that oxidation may have destroyed trash(?)…this interval may actually be the Sm Mbr…

St 60 - 93St -1 - 40.00 - 0.33

at 18.51m is an approx 1cm2 gypsum(?) fragment…bright white and no rxn with 10% HCl…

from 18.88 – 19.02m greyish mst section bedded at ~75° TCA…top of sub-interval has qtz and fsp grains throughout mud…gouge(?)…from 19.84 – 19.90m a greenish-grey granular mst section with large fragments of qtz and fsp throughout…well cemented (not ‘puggy’)…gouge(?)…

RB-09-230



Litho UnitMagnetic


15.27 31.37 underdeveloped fracture at 20.25 – 20.29m at ~55° TCA and from 20.29 – 20.34m sst is fractured parallel TCA…from 21.08 – 21.15m sst is broken at ~80° TCA and parallel TCA…sst is strongly hematitized, partially disaggregated and muddy…at 27.83m sst is fractured at ~90° TCA…fracture is strongly hematitized (reddish to dark grey hematite) and has carbonate crystals along fracture surface…fracture is followed by an underdeveloped fracture from 27.83 – 27.90m that is at ~25° TCA…from 28.46 – 28.53m hematite vein(?)…sst is very strongly hematitized and is deep reddish to dark grey in colour overprinting sst (complete replacement)…carbonate crystals…corrosive style hematitization…very dense and has magnetic susceptibility measurement of 0.33.lower contact is sharp and has an intense hematite blotch…no measurement taken as core was rounded (coring artifact)

31.37 32.94 HF Greenish in colour…clayey to silty mst with muddy, mg-cg sst sections towards the base of the interval (32.27 – 32.94m)…interval is strongly reduced with only minor weak to moderate reddish, stratified hematite present locally (dominantly in sandy sections, rare in mst)…sandy sections are micaceous and have fg diss organic detritus throughout…upper contact (with St Mbr) has strong, reddish to rusty coloured hematite patches for first ~3cm of interval)…lower contact appears to be gradational, however core is rounded at base of interval

Mm 67 - 88Mm -1 - 10.02 - 0.09

32.94 59.09 HF Tan-buff to reddish…dominantly cg-vcg sst that locally grades to granule-pebble cgl…local mst section…sst in interval is characterized by a weak mottled/stratified and mottled/pervasive hematite along with reddish patchy “hematite disease” throughout…hematite is a dark reddish to almost purple colour…kaolinite alteration of fsp’s is moderate (bright white specks) throughout…fsp’s are peachy to orange throughout…minor beigish clay alteration (dickite?) locally throughout that is often stratified…both reddish-brown and greenish coloured mst rip-ups are common throughout interval and are locally abundant…minor fg organic detritus…multiple instances of cross-bedding identified throughout…minor limonite alteration locally…micaceous…

Sm 58 - 90Sm -1 - 40.00 - 0.20

at 35.08m well developed calcite crystals filling vug ~2cm x ½ cm wide…

from 35.44 – 35.62m muddy section within sst…greenish mst interbedded with cg sst that has moderately strong deep red to purplish hematite…from 35.57 – 35.62m hematitized sst and mst is broken and partially disaggregated…from 36.96 – 37.00m is a 4cm thick reddish-brown to greenish mst section at ~75° TCA…

from 38.04 – 44.09m dominantly reddish to rusty coloured, strongly oxidized with reduction at the upper and lower contacts (38.04 – 38.46 and 43.03 – 44.09m) and is greenish with weak remnant oxidation patches visible…mostly clayey to silty mst and slt to fg sst with minor mg-cg sst sections towards base of sub-interval…sub-interval is strongly oxidized with minor small greenish reduction as spots..mst recovery was good…fairly competent…from 39.30 – 40.76m clayey mst hosts reddish carbonate caliche ranging from < ½ cm to ~3.5cm diameter…from 42.00 – 43.77m siltstone to fg sst…oxidation is weakly mottled…at 48.59m deep reddish fg disseminations of hematite become larger and more abundant with depth, becoming patchy to almost pervasive disseminations at 48.87 – 48.99m…broken sst at 48.98m…possibly fracture-related…underdeveloped fracture at 48.98 – 49.02m at ~45° TCA…fg disseminations continue until ~49.26m…from 49.56 – 49.68m cgl is broken and partially disaggregated…

at 49.82m, hematite vein/fracture with well developed calcite crystals on fracture surface…fracture surface is at ~80° TCA…from 50.37 – 50.41m strongly hematitized fracture/vein(?)…sst has mostly been replaced by hematite with some calcite crystals on surface…sst is broken at ~70° TCA…hematitized sst is very dense and has a magnetic susceptibility reading of up to 0.20…from 53.75 – 54.14m sst to cgl is broken and partially disaggregated…from 53.75 – 54.00m sst is strongly hematitized with dark reddish hematite and well developed calcite crystals filling vugs…very dense with a magnetic susceptibility reading of only 0.00 – 0.06…at 53.93 – 53.98m sst has underdeveloped fracture parallel TCA…from 54.00 – 54.14m cgl is partially disaggregated…

RB-09-230



Litho UnitMagnetic


32.94 59.09 from 53.73 – 55.81m greenish to greyish coloured clayey mst…possibly a large rip-up clast…

from 57.24 – 57.33m, cgl is broken and partially disaggregated…

lower contact is sharp at ~70° TCA

59.09 63.47 HF Dominantly rusty-red, clayey to silty mst to siltstone…interval is characterized by strong, rusty-red oxidation with local weak mottling and minor greenish reduction as spots throughout…interval hosts only minor reddish carbonate caliche locally…mst to siltstone is micaceous…minor charcoal grey patches and wisps throughout (organic detritus?)…good recovery…

Ml 68 - 100Ml -1 - 40.09

from 59.09 – 59.63m mst is reduced and is a greenish colour with some remnant oxidation present…from 59.09 – 59.24m is a pale green ‘puggy’ mst section…possible fault gouge(?)…lower contact is sharp at ~80° TCA and is reduced from 63.37 – 63.47m

63.47 93.59 HF Tan-buff to greenish to reddish-brown in colour…cg-vcg sst and cgl with local muddy sections…interval is dominantly unoxidized to weakly oxidized with local moderately strong reddish to reddish-brown sections/patches…fsp’s are a peachy-orange colour…weak to moderate kaolinite alteration of fsp’s throughout…minor greenish and reddish-brown mst rip-up clasts locally…interval is more oxidized towards the top of the interval and becomes more neutral (less oxidized and reduced) with depth…

Sl 64 - 88Sl -1 - 20.01 - 0.06

from 63.47 – 71.45m interval is moderately to strongly oxidized with mottled/stratified, mottled/pervasive and blotchy hematite…deep reddish, fg disseminated hematite accumulations are also present…from 66.55 – 69.84m is reddish-brown to rusty-red coloured, strongly oxidized clayey mst that has minor greenish reduction wisps and blotches throughout that become more abundant with depth…hosts reddish carbonate caliche locally throughout that ranges in size from <0.5cm - >3.0cm diameter…the upper and lower contacts of mst sub-interval (from 66.55 – 66.65m and 69.65 – 69.84m) are strongly reduced…no bedding measurement taken as underlying sst core is rounded (coring artifact)… from 71.45 – ~90.00m is weakly oxidized…minor weak, rusty-orange, hematite disease and weak mottled hematite locally…from 72.74 – 72.76m and 74.20 – 74.52m cgl’s are broken…

from 78.84 – 80.29m and 81.76 – 84.30m sst and cgl’s are broken (core has a blocky appearance) and some cgl sections are partially disaggregated…from 80.22 – 80.29m sst/cgl is very broken, partially disaggregated and moderately hematitized with a greenish, clayey ‘puggy’ mst immediately beneath (80.29 – 80.31m)…fault zone(?)…from 80.29 – 81.74m and 84.30 – 86.02m sst has significant intermixed greenish mud and locally has a granular texture…mst sections hosts significant fg organic detritus throughout…interbedded mst with cg sst (thin 1-2cm sections) with some gradational sections locally…from 87.46 – 87.56m strong reddish hematite blotch in area that is dominantly unoxidized…

from 86.45 – 86.52m and 86.79 – 86.84m cgls are broken and the later sub-interval is partially disaggregated…from ~90.00 – 93.59m sst becomes more oxidized with a mottled/stratified, pervasive and pervasive/stratified hematite locally throughout sub-interval…hematite is a deep reddish, fg disseminated hematite…within this sub-interval are greenish, reduced silty mst sections at 90.14 – 90.29m and 91.07 – 91.24m…the latter mst interval is followed by a zone of broken and fractured core from 91.24 – 91.59m…fracturing is at ~40 – 45° TCA…from 91.97 – 92.07m sst is fractured at ~35° TCA…

from 92.22 – 92.28m sst is broken and partially disaggregated…

from 92.36 – 92.47m large hematite blotch causing sst to have a reddish colour that is followed by a possible fracture at 92.47m at ~55° TCA…from 92.79 – 92.93m sst is fracture at ~20° TCA…


RB-09-230



Litho UnitMagnetic


93.59 101.00 RB Dark green to charcoal grey-black…clayey to silty mst, siltstone and shl…interval hosts moderate greyish to greenish coloured carbonate caliche, calcite veins and veinlets (white-greyish) with one instance of a peachy coloured veinlet…veinlets are commonly 1 – 3mm wide and are oriented between 45 – 90° TCA and parallel TCA…coalified wood fragments towards base of interval…interval is characterized by dark colour (organic content) and significant calcareous material…EOH

RB 59 - 82mst/slt/shl -10.07 - 0.13

0.28m of core is missing from 9.00 - 12.00m; 0.08m of core is missing from 24.00 - 27.00m; 0.15m of core is missing from 27.00 - 30.00m; 0.04m of core is missing from 30.00 - 33.00m; 0.06m of core is missing from 33.00 - 36.00m; 0.10m of core is missing from 57.00 - 60.00m; 0.15m of core is missing from 69.00 - 72.00m; 0.35m of core is missing from 87.00 - 90.00m; 0.20m of core is missing from 99.00 - 101.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

36.72 0.53 295836.19 Sm

37.25 0.53 295936.72 Sm

37.78 0.53 296037.25 Sm

RB-09-230

Hole No: RB-09-231



Total Depth (m): 50

Core Size: BQTK

Date Drilled: 01-Sep-09

License: 007897M




mE / mN



Test Depth (m)



Member

02-Sep-09 -

0.00 7.49 OB Overburden. HF sst boulders and cobbles and an exotic (gabbro) boulder OB

7.49 15.47 HF Reddish-brown to tan-buff cg-vcg sst…sst is characterized by a weak to strong, reddish-brown hematite…hematite is mottled/pervasive, pervasive/stratified and mottled/stratified…a bright, brick-red pervasive hematite is locally present…micaceous…sst is moderately broken and fractured throughout…

Su 62 - 93Su -1 - 40.01 - 0.10

from 7.62 – 8.02m sst is fractured and broken numerous times (at 7.62m, 7.72m, 7.79m and at 7.82 – 7.91m)…fractures appear to follow hematite stratifications at 35 – 55° TCA…

at 8.61m sst is fractured at ~50° TCA…fsp’s for ~0.5cm on either side of fracture and on fractured surface itself have a brighter pinkish to orangish appearance…

at 9.35m possible fracture in sst at ~40° TCA…

from 9.44 – 9.71m sst is broken and is followed by rounded core (coring artifact)…

at 9.78m and from 9.98 – 10.11m multiple fractures in sst at ~30° TCA (paralleling stratifications)…

from 11.98 – 12.40m possible fault zone…from 11.98 – 12.08m is a strongly hematitized cg-vcg sst with a pervasive reddish-brown hematite...part of core looks as though it has been eaten away (very dark red to charcoal-grey corrosive-style hematitization)…from 12.08 – 12.25m greenish, granular mst section with abundant cg-vcg grains of sub-rounded qtz and fsp (gouge?)…from 12.25 – 12.40m is more very strongly hematitized cg-vcg sst…sharp boundary of hematitization (no gradual dissipation)…possibly sheared (fabric visible in sst)…

from 12.77 – 12.82m reddish-brown mst section at ~40° TCA…

from 13.16 – 13.27m greenish reduced granular mst section…adjacent sst is also greenish…possible fracture at 50° TCA…

from 13.45 – 13.78m reddish coloured, very strongly hematitized fragmented caliche horizon(?)…cannot distinguish features due to intense overprinting of oxidation…fractured and broken locally…

at 14.06m vug in sst has well developed calcite crystals filling vug…

lower contact is sharp, strongly oxidized and very micaceous (for last ~10cm of interval)…contact is at ~50° TCA…

15.47 27.34 HF Reddish-brown to greenish…dominantly clayey to silty mst that grades into slt and fg-mg sst towards the base of the interval…mst hosts moderate reddish-brown carbonate caliche throughout…most caliche are small (<1cm diameter) but there are some up to ~3cm diameter…caliche-rich horizon at 22.25 – 22.31m…minor limonite alteration locally throughout… slt and sst sections are dominantly greenish and reduced with only weak mottled/pervasive and mottled/stratified hematite present locally…micaceous and hosts significant fg diss organic detritus thoughout…this interval is both oxidized and reduced, although reduction is more prominent…oxidation is mottled by grey-green to greenish reduction within the msts…reddish-brown remnant, patchy oxidation present locally…

Mu 62 - 91Mu -1 - 20.02 - 0.14

from ~15.47 – 17.00m mst is dominantly oxidized with only weak greenish reduction patches and spots throughout…

RB-09-231



Litho UnitMagnetic


15.47 27.34 from 20.00 – 20.82m is a tan-buff to reddish-brown cg sst with minor thin (1-2cm wide) greenish interbedded mst…sst hosts abundant greenish and reddish-brown (although green is more common) intermixed mud locally throughout and is locally weakly consolidated and has a granular appearance…ssts appear to be bedded at ~45 – 55° TCA…

at 21.85 – 21.90m and 22.00 – 22.04m large brick-red hematite patches (brighter and more intense than oxidation in area)…interval becomes silty at 24.39m and by 26.70m has graded into a mg, micaceous sst with significant intermixed mud…

lower contact is gradational

27.34 50.00 HF Tan-buff to reddish-brown…cg-vcg sst that locally grades to cgl with minor reddish-brown to greenish clayey to silty mst sections (25 – 35cm thick)…interval is characterized by a weak to moderately strong, reddish-brown mottled/pervasive and mottled/stratified hematite as well as a spotty ‘hematite disease’…hematite disease spots are locally smaller, fg dissemination accumulations…interval hosts abundant reddish-brown to green ish mst rip-up clasts locally…fsp’s are a peachy-orange colour throughout…kaolinite alteration is weak throughout…sst/cgl is moderately fractured…fractures measure between 35 – 80° TCA and most are not hematitized…

St 59 - 99St -1 - 40.00 - 0.06

from 27.58 – 27.70m greenish silty mst-stiltstone resembling gradational section from overlying Mu member…included in the St Mbr due to fact that overlying sst (from 27.34 – 27.58m) did not resemble the Mu Mbr, …bedded at ~50° TCA…

from 29.67 – 30.37m sst is moderately broken and fractured(?) and has a blocky appearance…fracturing(?) ranges from 45 – 80° TCA…at 30.21m sst is fractured and has a muddy to granular appearance…gouge(?)…reddish-brown intermixed mud…underdeveloped fractures locally…

at 33.05m fracture between vcg sst/cgl and mg-cg sst…fracture surface is very strongly hematitized and has an oily appearance…fracturing is at ~45° TCA…

from 34.57 – 34.62m a greyish-brown silty mst section that is broken and partially disaggregated…no measurement available…

from 35.69 – 36.04m a grey-green to reddish-brown clayey to silty mst to slt…dominantly reduced with moderately strong mottled/pervasive and stratified remnant oxidation...micaceous…no bedding surface available for measurement…

at 37.07m sst/cgl is fractured at ~55° TCA and has strong reddish-brown hematite on fracture surface…the matrix of pebble/granule cgl is completely replaced by hematite (extends approx. 4 cm up-hole from fracture)…

from 39.93 – 40.25m is a muddy section…from 39.93 – 40.02m cg-vcg sst/granule cgl has significant intermixed greenish-grey and reddish-brown mud and mst rip-up clasts…cgl is weakly consolidated…from 40.02 – 40.09m mg-cg sst with abundant greenish-grey mud has a granular appearance…from 40.09 – 40.25m is greenish-grey to reddish-brown clayey to silty mst…bedded at ~60° TCA…

from 40.33 – 40.36m sst is fractured and broken core has a ‘sugary’ appearance resulting from significant calcite crystals on surface…hosts moderate reddish-brown to orangish patchy hematite (+/- Fe-carbonate?)…fractured at ~85° TCA…

at 42.48m sst is fractured at ~50° TCA and is strongly hematitized with hematite bleeding out into adjacent sst for ~3cm on either side…strong reddish-brown, corrosive-style hematitization…fracture has an oily appearance…

from 45.26 – 45.32m tan-buff sst and reddish-brown mst section that is broken and partially disaggregated…does not appear to be gouge…EOH

RB-09-231



Litho UnitMagnetic


1.75m of core is missing from 5.00 - 8.00m; 0.10m of core is missing from 11.00 - 14.00m; 0.70m of core is missing from 14.00 - 17.00m; 0.60m of core is missing from 17.00 - 20.00m; 0.80m of core is missing from 20.00 - 23.00m; 0.10m of core is missing from 25.00 - 29.00m; 0.25m of core is missing from 29.00 - 32.00m; 0.05m of core is missing from 32.00 - 35.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

11.32 0.44 296110.88 Su

11.75 0.43 296211.32 Su

14.34 0.56 296313.78 Su

14.90 0.56 296414.34 Su

15.47 0.57 296514.90 Su

RB-09-231

Hole No: RB-09-232




Core Size: BQTK


License: 016221M




mE / mN



Test Depth (m)



Member

03-Sep-09 -

0.00 9.70 OB Overburden. HF sst boulder and cobble OB

9.70 15.22 HF Reddish-brown to grey-green to tan-buff in colour…dominantly siltstone - fg sst with lesser mg-cg sst, granule-pebble cgl and silty mst…interval is characterized by an overall ‘ruddy’ appearance resulting from mottled reddish-brown oxidation, green-grey reduction blotches and bleaching along fractures…

Mu20 50 - 93Mu20 -1 - 40.04 - 0.08

from 9.70 – 11.73m ruddy, reddish-brown to greenish coloured siltstone and mg-cg sst to pebble cgl…from 9.70 – 9.96m is strongly reduced, grey-green siltstone with minor patchy reddish-brown oxidation…from 9.96 – 10.50m fg-mg sst has a ruddy appearance (reddish-brown mottled/stratified hematite), is coarser (mg – cg sst and pebble cgl)…from 10.50 – 11.73m mottled/stratified hematite…fractures at 11.15m and 11.28m at ~35° TCA…from 11.73 – 15.22m reddish-brown to grey-green clayey to silty mst - stilstone and fg sst…sub-interval is characterized by locally strong reddish-brown oxidation and local reduction (reduction bands, mottling and bleaching)…from 13.33 – 13.99m and 14.79 – 15.20m is an anomalous, spotty green alteration...mottling of reduction(?)…from 12.84 – 13.11m sst is fractured at ~10-15° TCA…from 12.99 – 13.25m reddish-brown to greenish clayey – silty mst section at ~50° TCA...at 13.38m and 15.00m fg – mg sst is fractured at 15° and 25° TCA respectively…lower contact is sharp and broken

15.22 42.04 HF Dominantly reddish-brown clayey – silty mst and siltstone with minor fg-mg sst…interval is characterized by a strong, reddish-brown oxidation with minor greenish to dark green-grey coloured reduction as wisps and patches locally…mst-siltstone hosts carbonate caliche throughout that is locally abundant…mst is somewhat weathered, thus structures are difficult to interpret as they may be coring/weathering artifacts…overall, interval has a massive appearance…

Mu 59 - 95Mu -1 - 40.09 - 0.12

from 15.22 – 19.59m reddish-brown, strongly oxidized silty mst…sub-interval is strongly oxidized and hosts minor carbonate caliche (<0.5cm diameter)…from 16.62 – 19.59m mst has a dark grey-green colour rather than reddish-brown…from 19.59 – 24.43m reddish-brown siltstone - fg sst…hosts moderate small (dominantly <1cm diameter) tan to reddish-brown carbonate caliche…minor grey-green reduction (mottling, wisps and patches) throughout…much of core in this sub-interval is broken or fractured…from 21.46 – 22.43m siltstone-fg sst is fractured parallel TCA…from 23.52 – 23.84m siltstone - fg sst is badly broken and core immediately down-hole (from 23.84 – 24.00m) is fractured sub-parallel TCA…from 24.43 – 42.04m dominantly reddish-brown clayey – silty mst that is strongly oxidized with minor weak greenish to grey-green reduction as patches and wisps…from 24.43 – 31.47m reddish-brown mst has minor to moderate reduction (patches and wisps) and moderate to abundant carbonate caliche throughout…from 31.47 – 36.45m reddish-brown mst has a massive appearance with only minor caliche locally and very minor wispy reduction locally…from 36.45 – 39.78m reddish-brown mst with abundant carbonate caliche…moderate greenish to grey-green reduction mottling oxidation…caliche-rich sections locally (only caliche recovered)…caliche is buff to reddish-brown in colour and locally up to ~5cm in diameter…

RB-09-232



Litho UnitMagnetic


15.22 42.04 from 39.78 – 42.04m massive silty mst…from 39.78 – 40.58m mst is dominantly reduced with weak reddish-brown oxidation patches (mottled) and virtually no caliche…from 40.58 – 42.04m silty mst is a grey-green colour, becoming darker (charcoal-grey) with depth as a result of increasing organic content…hosts weak to moderate, yellowish limonite alteration locally…lower contact is sharp at ~45° TCA and is reduced…marked by a coal seam (~1 – 2 cm thick) in underlying sst which is rimmed by fg py…

42.04 45.74 HF Greyish…cg-vcg sst and cgl…interval is characterized by an overall reduced, greyish appearance and an abundance of organic trash…organic trash (fg disseminations and wispy belbs) that are dominantly stratified… larger organic trash fragments are rare…stratifications range from ~40 – 60° TCA with most either at ~45° or ~60° TCA…micaceous…locally very micaceous…hosts minor to moderate greenish-grey clayey-silty mst sections…moderate greenish-grey mst rip-up clasts and intermixed mud locally throughout…

St 68 - 107St -10.01 - 0.06

from 43.12 – 43.23m cgl is broken and partially disaggregated…

from 44.98 – 45.03m greenish-grey clayey mst bed at ~55° TCA…

lower contact is gradational and is marked only on the presence of hematite and the lack of organic trash in the sst’s and cgl’s following this point…

45.74 68.82 HF Reddish-brown to tan-buff…mg-vcg sst and cgl…sst is characterized by varying degrees and types of reddish-brown hematite throughout that overall increases (amount and intensity) with depth…forms of hematitization include mottled/pervasive, stratified, pervasive/stratified and local ‘hematite disease’…micaceous…fsp’s are a peachy-orange colour…minor kaolinite alteration throughout… sst/cgl is moderately broken and fractured locally throughout…unsure if this interval is an oxidized St Mbr or if it is the Sm Mbr...

Sm 59 - 100Sm -1 - 30.01 - 0.11f

from 45.74 – 49.17m sst and cgl is weakly oxidized…hosts a weak, reddish-brown, mottled, pervasive/stratified and pervasive hematite with lesser blotchy hematite…local bleaching along fractures and as minor spots and blotches…cgl and sst are moderately broken and fractured throughout…sst is fractured at 48.22m, 48.23m, 48.29m and 48.44m between 35° - 50° TCA…fracture surfaces are bleached with bleaching bleeding into adjacent sst for ~0.5 – 1.0cm...from 49.17 – 55.05m sst has deep reddish-brown ‘hematite disease’ blotches overprinting a weak, stratified hematite…hematite disease blotches are larger and more abundant toward top of sub-interval and lessen (smaller and less abundant) with depth within sub-interval…blotches generally range from 0.25cm – 0.50cm diameter…from 49.17 – 49.28 sst has a large, reddish, intense hematitic blotch…at 49.63m granule cgl is fractured at ~80° TCA with strong reddish hematite and manganese stain(?) from 49.58 – 49.64m… from 55.01 – 55.05m reddish-brown clayey mst bed…appears to be bedded at ~40° TCA…

RB-09-232



Litho UnitMagnetic


45.74 68.82 from 50.05 – 68.82m sst is more strongly hematitized…sst – cgl is characterized by a moderate to strong reddish-brown mottoled/pervasive, mottled/stratified and pervasive/stratified hematite…from 50.36 – 50.38m reddish-brown granular mst (fault gouge?)…from 50.32 – 50.39m foliations(?) visible…coarser qtz and fsp grains intermixed with reddish-brown mst exhibits a foliated fabric(?) parallel to suspect fault zone (~50° TCA)…at 51.32m and 51.41m cgl is broken…from 51.55 – 52.40m cgl is fairly broken and core has a somewhat blocky appearance…from 51.55 – 51.65m cgl hosts abundant reddish-brown mst rip-up clasts…from 51.65 – 51.78m cgl is badly broken and partially disaggregated…at 54.26 m sst is fractured at ~50° TCA…at 55.41m sst is fractured at ~60° TCA…possible fractures in sst at 57.11m and 57.21m and 57.91m at 45 – 57° TCA…at 58.15m thin greenish clayey mst bed(?) or possible larger mst rip-up clast as there are some larger ones in the area…from 59.47 – 60.35m cgl is broken with a blocky appearance…from 59.83 – 59.87m cgl is broken and disaggregated…from 59.94 – 59.98m cgl is weakly consolidated and is partially disaggregated…from 60.07 – 60.35m cgl is completely broken and disaggregated…anomalous radiometrics were recorded over this broken zone by the down-hole radiometric probe…~1.20m lost core between 60.00 – 63.00m…at 60.80m possible fracture paralleling stratifications ( ~55° TCA)…from 61.15 – 61.83m cgl is broken and core has a blocky appearance…from 61.53 – 61.56m reddish-brown clayey-silty mst section that has some cg qtz and fsp grains encompassed within possible fault gouge(?)…from 65.73 – 65.77m thin, reddish-brown clayey mst with vcg grains of qtz and fsp on top of mst…at 66.89m and 67.10m sst is fractured at 35° and 40° TCA respectively…significant reddish-brown mst rip-up clasts in area of both of these fractures…possible foliations parallel to first fracture plane(?)…from 67.40 – 67.81m are reddish-brown to greenish-grey clayey mst sections…dominantly oxidized with moderate greenish-grey reduction mottling oxidation…bedded at ~25° and 50° TCA respectively…at 68.26m sst is fractured at ~40° TCA…lower contact is sharp and appears to be at ~70° TCA but core may be broken

68.82 70.60 HF Grey-green to reddish-brown…clayey-silty mst…strongly reduced with weak to moderate reddish-brown mottled oxidation locally…massive…moderately weathered and thus it is difficult to distinguish structure from coring and weathering artifacts…from 69.28 – 69.31m is a reddish-brown, strongly hematitized mg sst section at ~50° TCA…lower contact is sharp…no measurement taken as underlying sst core is partially rounded (coring artifact)

Ml 62 - 100Ml -1 - 20.09 - 0.23

70.60 82.50 HF Tan-buff to reddish-brown…cg-vcg sst and granule-pebble cgl with grey-green to reddish-brown clayey-silty mst sections locally…hosts weak to moderate kaolinite alteration of fsp’s throughout…interval is characterized by a weak, reddish-brown stratified and mottled/pervasive hematite throughout…micaceous…

Sl 60 - 91Sl -1 - 10.00 - 0.09ff

from 70.60 – 73.14m sst is characterized by a weak, reddish-brown, fg disseminated hematite that is stratified…stratifications are locally wavy to sub-parallel TCA, but are most often between 50 – 70° TCA…a bedding measurement at 70.74m is at 45° TCA…sst is strongly hematitized at 70.60m and hematite continues down-hole for ~5cm…from 71.28 – 71.36m a brighter red, more intense hematite is present…sst is fractured at 72.76m, 72.78m, 72.88m and 72.92m and fracturing ranges from 45 – 70° TCA…from 73.10 – 73.22m sst hosts abundant intermixed mud and sst is broken along mst bedding…

at 73.39m sst is fractured at ~65° TCA and is moderately hematitized (reddish-brown hematite)…at 73.42m sst has a corrosive style hematization with a white carbonate (~2cm thick halo) surrounding vug-like feature…from 73.45 – 74.33m sst and cgl is virtually unoxidized…hosts increasingly abundant greenish coloured mst rip-up clasts (locally up to ~6cm long) with depth…gradation into the underlying mst interval…appears to be bedded at ~55° TCA…hosts fg disseminated, reddish hematite accumulations (spots) for last ~15cm of sub-interval…from 74.33 – 75.51m greenish to grey-green to reddish-brown clayey to silty mst that is strongly reduced with only minor weak reddish-brown oxidation present throughout…bedded at~47° TCA…from 75.51 – 75.84m fg-mg sst has intermixed greenish and reddish-brown intermixed mud…very micaceous..hosts abundant fg disseminated organic detritus and moderate reddish-brown mottled/pervasive hematite…

RB-09-232



Litho UnitMagnetic


70.60 82.50 from 75.84 – 82.50m dominantly cg-vcg sst that is unoxidized to weakly oxidized…weak to moderate kaolinite alteration of fsp’s…reddish-brown to grey-green clayey mst sections at 78.86 – 78.91m and 80.49 – 80.54m…from 79.10 – 80.61m sst hosts significant greenish mst rip-up clasts…from 80.00 – 80.49m mud chips are even more abundant and sst is fairly broken and locally has a blocky appearance…from 81.31 – 82.50m sst becomes fg - mg and hosts abundant fg diss organic detritus that is stratified…micaceous…from 81.81 – 82.50m sst is badly broken…EOH

RB-09-232



Litho UnitMagnetic


0.15m of core is missing from 45.00 - 48.00m; 0.14m of core is missing from 51.00 - 54.00m; 1.20m of core is missing from 60.00 - 63.00m; 0.10m of core is missing from 63.00 - 66.00m; 0.20m of core is missing from 66.00 - 69.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

39.36 0.54 296638.82 Mu

39.90 0.54 296739.36 Mu

40.44 0.54 296839.90 Mu

40.98 0.54 296940.44 Mu

41.52 0.54 297040.98 Mu

42.04 0.52 297141.52 Mu

42.52 0.48 297242.04 St

43.00 0.48 297342.52 St

43.48 0.48 297443.00 St

43.96 0.48 297543.48 St

44.44 0.48 297643.96 St

44.89 0.45 297744.44 St

47.52 0.59 297846.93 St

60.94 0.44 297960.50 St

65.18 0.56 298464.62 St

65.74 0.56 298565.18 St

66.30 0.56 298665.74 St

66.86 0.56 298766.30 St

67.42 0.56 298866.86 St

68.82 0.77 298968.05 St

69.74 0.49 299069.25 Mm

71.24 0.47 299170.77 Sm

71.71 0.47 299271.24 Sm

72.18 0.47 299371.71 Sm

RB-09-232

Hole No: RB-09-233




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

09-Sep-09 -


5.31 8.04 HF Reddish-brown cg-vcg sst and minor cgl… interval is characterized by a weak reddish-brown mottled and pervasive/stratified hematite with minor, brighter reddish-brown hematitic patches locally…vuggy… micaceous…hosts minor kaolinitie alteration of fsp’s throughout…from 6.18 – 6.66m sst has a weak to moderate limey-green alteration (limonite?) that overprints qtz and fsp grains in sst and a mst rip-up clast at 6.64m…core is highly broken and fractured and has a blocky appearance throughout…fractures are dominantly 45 - 60° TCA, but range from 35 – 70° TCA throughout and is generally parallel to stratifications…from 7.71 – 7.96m cgl is very broken…

Su30 62 - 98Su30 1 - 20.01 - 0.04

8.04 8.66 HF Reddish-brown mg-cg sst with significant intermixed silty mst…interval is characterized by a moderately strong mottled/pervasive hematite with moderate greenish reduction spots locally…sst is fractured at 8.59m at ~40° TCA and sst here is more strongly hematitized (more intense reddish-brown hematite)…lower contact is gradational (sst grades into a silty mst)…an overall increase in hematitization with depth is visible…

Su22 62 - 87Su22 1 - 30.02 - 0.05

8.66 15.02 HF Dominantly greyish-green to reddish-brown, interbedded ‘ruddy’ slt – fg sst and clayey to silty mst…interval is characterized by stratified oxidation and reduction with approximately equal proportions of each…reddish-brown oxidation is being mottled by grey-green reduction and tan-buff bleaching…bedding instances measure between 45 – 55° TCA and stratifications follow this bedding…

Su20 52 - 81Su20 -1 - 30.07 - 0.12

from 8.66 – 9.16m brownish coloured silty mst with very small lime-green alteration spots (limonite?)…locally sandy…gradation from overlying sst…

from 9.16 – 9.56m reddish-brown slt that grades into a fg sst and is strongly oxidized (reddish-brown in colour)…

from 9.56 – 10.41m ‘ruddy’ reddish-brown to greenish fg-mg sst…

from 10.41 – 15.02m interbedded ‘ruddy’ slt-fg sst and clayey-silty mst…dominantly reduced with weak to moderately strong reddish-brown oxidation locally…some mst’s within this sub-interval host minor, small, buff-coloured carbonate caliche (<1cm diameter) locally…at 13.94m slt – fg sst is fractured at ~45° TCA…

15.02 16.77 HF Colourful, polymictic cgl and lesser tan-buff to reddish-brown, cg-vcg sst…sst hosts a weak stratified reddish-brown hematite while cgl appears to be unoxidized…normally graded…cgl is moderately broken throughout and from 16.63 – 16.68m cgl is highly broken and partially disaggregated… from 16.68 – 16.74m an underdeveloped fracture sub-parallel TCA and here cgl is very calcareous (buff to orangish carbonate) and vuggy (as a result of dissolution of carbonate)…

Su10 59 - 84Su10 10.02 - 0.13

lower contact is sharp at ~40° TCA, though contact is partially broken…

16.77 19.40 HF Reddish-brown clayey – silty, nodular mst…hosts abundant buff coloured carbonate caliche that ranges in size from <1 – 5cm diameter...in places, only caliche was recovered…interval is strongly oxidized with patchy and wispy greenish reduction locally…lower contact is gradational into the underlying slt-fg sst section…end of member is marked by the lack of caliche…

Mu25 50 - 84Mu25 -1 - 30.06 - 0.14

19.40 25.17 HF ‘Ruddy’ reddish-brown slt-fg sst with greenish coloured reduction patches and along fractures…hosts carbonate caliche that is well cemented in sst/sltstone…micaceous..slt-fg sst hosts abundant greenish, intermixed mud locally throughout… from 21.40 – 21.90 greenish to reddish-brown clayey-slt that is strongly at top of sub-interval (contact with overlying sst)…

Mu20 59 - 104Mu20 -1 - 20.12 - 0.16

RB-09-233



Litho UnitMagnetic


19.40 25.17 slt-fg sst is fractured at 20.21m, 20.87m, 21.05 – 21.10m, 22.20m and 21.89m between 37 – 65° TCA…

lower contact is at 55° TCA

25.17 40.58 HF Reddish-brown clayey-silty mst, slt and fg-mg sst with minor granule-pebble cgl…mst and slt-fg sst are locally nodular…hosts minor greenish coloured reduction locally throughout…carbonate caliche range from small (<0.5cm diameter) up to 6cm diameter locally and are rare to abundant throughout…core recovery is good throughout interval except in caliche-rich sections (from 27.90 – 28.26m, 38.48 – 38.79m and 40.00 – 40.58m) where only buff-coloured caliche and minor reddish-brown mst was recovered…from 25.17 – 27.90m carbonate caliche are only small (<1cm diameter) and are minor…clayey –silty mst is moderately weathered throughout making the distinction between structures and coring/weathering artifacts difficult…

Mu10 58 - 90Mu10 -1 - 30.06 - 0.14

from 25.17 – 25.28m moderate yellowish limonite alteration overprinting oxidation and reduction in mst…from 27.00 – 27.90m moderate reduction mottling oxidation…

at 28.67m mst becomes silty to granular and grades into granule/pebble cgl at 28.90m…gradational sections hosts abundant intermixed reddish-brown mst and has a granular texture…

from 28.90 – 29.58m reddish-brown granule/pebble (matrix supported) cgl at 52° TCA…

cgl is fractured at 29.15m (25° TCA) and 29.24m (52° TCA)…

from 29.58 – 29.86m reddish-brown granular mst section with rare carbonate caliche…

from 29.86 – 33.74m dominantly reddish-brown slt to fg sst with minor interbedded clayey-silty mst sections…moderately well oxidized with minor greenish reduction spots and buff-coloured mottling throughout…from 29.86 – 31.32m fg-mg sst has a granular appearance due to presence of small (<0.5cm diameter) carbonate caliche and caliche fragments…slt-fg sst is fractured at 30.41m, 31.05m, 30.10m and 31.24m at 20 – 35° TCA…

from 31.32 – 40.58m dominantly reddish-brown clayey mst with minor interbedded slt–fg sst…hosts minor carbonate caliche throughout sub-interval (<1cm diameter) except from 38.48 – 38.79m and 40.00 – 40.58m which are disaggregated sections with predominantly only caliche recovered…caliche in these sections are larger, locally >5cm diameter, and are buff coloured…sub-interval is overall strongly oxidized with weak greenish reduction mottling oxidation locally (greenish spots and wisps)…EOH

0.23m of core is missing from 6.00 - 9.00m; 0.36m of core is missing from 9.00 - 12.00m; 0.85m of core is missing from 15.18m - 18.00m; 0.10m of core is missing from 18.00 - 24.00m; 0.30m of core is missing from 24.00 - 27.00m; 0.20m of core is missing from 36.00 - 39.00m.

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-233

Hole No: RB-09-234




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

10-Sep-09 -


4.76 17.33 HF Tan-buff to reddish-brown…cg-vcg sst with minor, thin (generally <5cm thick) cgl sections…interval is characterized by a weak to moderate reddish-brown to reddish hematite alteration that is locally mottled/stratified, stratified and spotty (‘hematite disease’)…patchy hematite is also present but is less common…weak to moderate kaolinite alteration of fsp’s throughout…fsp’s are locally a peachy-orange colour…vuggy…vugs locally reaching up to ~3cm diameter and cut through diameter of core…sst is locally very muddy and has a granular appearance…sst is moderately to highly broken and fractured throughout and has a blocky appearance for most of the interval…sst is fractured/broken at ~40 – 70° TCA with the majority between 45 – 65° TCA in areas of stratified hematite, fracturing appears to be parallel to stratifications…hosts minor beigish clay (dickite?) that is most often stratified throughout…locally micaceous..moderate small, reddish-brown mst rip-up clasts throughout…

Su30 59 - 79Su30 -1 - 40.00 - 0.07

from 4.76 – 6.85m sst is very highly broken and has a blocky appearance…mostly broken at ~45-65° TCA…fracture at 6.07m (broken core, no measurement) has moderately strong, reddish hematite along fracture surface and along part of core…hematite is patchy and locally corrosive…at 7.51m vug in sst is ~2cm in diameter and tunnels through entire diameter of core…non-calcareous…from 8.28 – 8.33m sst is fractured sub-parallel TCA…fracture surface has a weak reddish-brown hematite with an orangish alteration (Fe-carb?)…from 9.24 – 9.30m sst hosts significant intermixed greenish mud and abundant small, reddish-brown mst rip-up clasts and is partially disaggregated…from 10.21 – 10.42m greenish to reddish-brown muddy sst to silty mst…very calcareous…hosts reddish-brown mottled/stratified hematite…from 10.31 – 10.42m sst is broken and partially disaggregated…appears to be bedded at ~50° TCA…from 10.42 – 11.12m sst is characterized by a fg, reddish disseminated hematite that locally accumulates to form blotches or smaller ‘hematite disease’…micaceous…from 10.54 – 10.60m sst is broken sub-parallel TCA and at ~70° TCA…from 11.12 – 12.00m lost core…at 11.12m sst is broken and fracture surface has a strong, reddish hematite alteration and a possible organic stain on portion…from 12.53 – 12.67m mg sst is fractured sub-parallel TCA, is partially disaggregated and has moderate to strong reddish-brown hematite along fracture surface as well as an organic(?) stain…from 13.05 – 14.22m sst is very vuggy…possible dissolution of mst as vugs/sst do not effervesce with 10% HCl and there are abundant small reddish-brown mst rip-up clasts throughout sub-interval…a bedding instance at 13.06m is at ~42° TCA…at 13.63m sst is fractured at ~75° TCA and is strongly hematitized with a dark greyish (charcoal-grey) hematite(?)…from 13.99 – 14.22m sst is fractured (twice) at 40° and 30° TCA and has numerous strongly hematitized vugs (reddish-brown and dark greyish – possibly dissolution of mst)…vugs range in size from <0.5cm and up to 5cm x 3cm…from 15.28 – 15.70m sst has significant intermixed greenish mud…reddish-brown mst rip-up clasts with reduced (greenish) rims…from 15.51 – 15.60m and 15.65 – 15.70m are granular mst sections with abundant cg-vcg grains of qtz and fsp within a greenish to reddish-brown silty mst…

RB-09-234



Litho UnitMagnetic


4.76 17.33 from 16.16 – 16.24m sst is fractured at ~30° TCA…very micaceous…moderate to strong reddish-brown to greyish coloured patchy hematite alteration…core immediately down-hole is rounded…from 16.80 – 17.21m sst is being overprinted by an orangish-brown alteration (oxidation of fg disseminated sulphides?)…lower contact is at ~35° TCA and is sharp

17.33 18.22 HF Reddish-brown fg-mg sst with minor silty mst – siltstone…strongly oxidized (reddish-brown colour) with a weak to moderate, greenish reduction mottling oxidation throughout interval…micaceous…massive…at 17.85m sst is fractured at 50° TCA…from 18.15 – 18.40m sst hosts minor large qtz and fsp grains and has a granular appearance…at 18.10m core is rounded (drilling artifact)…

Su22 60 - 83Su22 -1 - 30.05 - 0.14

at 18.63m fracture at ~42° TCA with an organic stain along fractured surface…

lower contact is sharp and broken

18.22 23.85 HF ‘Ruddy’ reddish-brown to greenish coloured…interbedded clayey-silty mst , siltstone and fg sst with mst being most abundant…dominantly oxidized (reddish-brown) with stratified greenish reduction overprinting and weakening strength of oxidation resulting in the ‘ruddy’ appearance…hosts minor tan-buff to reddish-brown carbonate nodules locally throughout but are most abundant from 21.00 – 21.20m…from 21.11 – 21.18m is a caliche-rich section where only caliche (and minor mud) were recovered…moderately weathered, broken and partially disaggregated…

Su20 54 - 83Su20 -1 - 30.08 - 0.17

from 23.11 – 23.85m interval changes from dominantly clayey – silty mst and siltstone to a siltstone – fg sst…very micaceous…from 23.11 – 23.39m is dominantly oxidized with weak to moderate reduction overprinting…from 23.39 – 23.85m is more reduced and remnant oxidation has a ‘ruddy’ appearance and becomes more reduced with depth within this section…stratifications appear to follow laminae and siltstone/sst is frequently broken along these laminae…lower contact is sharp at ~50° TCA

23.85 25.23 HF Tan-buff cg-vcg sst with local colourful polymictic cgl sections…k-fsp-rich…hosts a weak reddish-brown mottled/pervasive and mottled/stratified hematite throughout…hosts fg disseminated organic detritus that is stratified locally throughout…minor greenish coloured mst rip-up clasts locally…interval is fairly intact with the exception of some cgl areas that are broken (from 24.75 – 24.84m and at 25.12m)…bedding instances throughout range from ~50 - 55° TCA…lower contact is sharp at ~45° TCA…

Su10 65 - 85Su10 0 - 10.03 - 0.08

25.23 27.51 HF Reddish-brown to greenish…nodular clayey-silty mst and siltstone…hosts abundant tan-buff to reddish-brown carbonate caliche, most of which are <1cm diameter but some are up to 5cm diameter…caliche-rich sections locally exist…both oxidized and reduced with approximately equal proportions of each…

Mu25 48 - 82Mu25 -1 - 40.09 - 0.11

from 25.23 – 25.71m greenish to reddish-brown clayey-silty mst…from 25.23 – 25.39m greenish nodular silty mst is highly broken and disaggregated…from 25.39 – 25.49m dominantly reddish-brown nodular mst with minor greenish reduction patches and minor nodules locally…from 25.49 – 26.71m nodular, reddish-brown clayey-silty mst and siltstone…nodule-rich…competent (intact)…nodules often have reddish-brown cores and tan-buff (reduced?) rims…from 26.71 – 27.29m dominantly reddish-brown clayey-silty mst with greenish sections…nodule-free…from 27.27 – 27.51m silty mst is granular (cg-vcg grains of qtz and fsp throughout) as it grades into the underlying sst section…grades into a muddy sst at the end of this sub-interval…lower contact is gradational

27.51 32.15 HF Tan-buff to reddish-brown…cg-vcg sst and colourful cgl…interval is characterized by a weak to moderate, reddish-brown mottled/pervasive and pervasive/stratified hematite throughout…cgl and sst locally have significant intermixed greenish mud and a granular to silty texture…interval is fairly intact except in some areas where cgl is broken along larger clasts (from 29.07 – 29.13m and 31.08 – 31.15m)…from 31.05 – 31.09m sst is broken and partially disaggregated…

Mu 50 - 88Mu -1 - 20.01 - 0.07

sst is fractured(?) at 28.57m, 28.58m, 28.66m and 28.70m at ~45° TCA…sst in this area has significant intermixed greenish mud and is poorly consolidated…

RB-09-234



Litho UnitMagnetic


27.51 32.15 at 30.27m sst is fractured at ~30° TCA…


32.15 34.58 HF Reddish-brown siltstone – fg sst and minor silty mst…strongly oxidized with minor greenish reduction and mottling throughout, locally giving a ‘ruddy’ appearance…minor greenish, more strongly reduced sections locally…reduction is weak to non-existent from 32.15 – 32.51m…from 32.51 – 32.60m silty mst section is greenish, strongly reduced and broken…from 32.60 – 34.48m weak to moderately strong reduction patches and mottling is present…at 32.42m possible fracture in fg sst at ~55° TCA…

Mu18 58 - 93Mu18 -1 - 40.06 - 0.12

from 33.00 – 33.14m slt is broken and crumbled followed by a fracture at ~20° TCA at 33.14m…at 34.02m fg sst is fractured at 35° TCA…


34.58 39.50 HF Reddish-brown to brownish coloured clayey – silty mst…strongly oxidized…hosts minor carbonate caliche throughout…strongly weathered (broken and crumbled) in places…

Mu18 62 - 75Mu18 40.03 - 0.12

from 34.58 – 35.72m clayey-silty mst is a reddish-brown colour and hosts only minor, tan coloured caliche…caliche are small (dominantly <1cm – 1cm diameter)…from 35.72 – 37.04m mst is more of a brownish colour, possibly a function of reduction(?) and hosts small caliche throughout…from 37.04 – 39.50m reddish-brown to rusty-brown clayey-silty mst with minor caliche throughout… from 37.63 – 37.74m is a caliche-rich section where caliche are larger (up to ~3.5cm diameter) and more abundant than elsewhere in interval…lower contact appears to be gradational but contact area is poorly consolidated and cannot pick-up to examine

39.50 41.58 HF Reddish-brown…fg-mg sst and lesser siltstone…strongly oxidized with greenish reduction along fractures and as blotches…reduction also mottles oxidation giving sst a ‘ruddy’ appearance…from 40.98 – 41.42m…hosts moderate tan-buff to reddish-brown carbonate nodules throughout which are well cemented…sst is fractured at 39.76m, 39.95m, 40.13m, 40.46m, 41.05m and 41.48m between 25 – 60° TCA…EOH

Mu10 58 - 90Mu10 -1 - 30.04 - 0.06

0.29m of core is missing from 6.00 - 9.00m; 0.87m of core is missing from 9.00 - 12.00m; 0.15m of core is missing from 15.00 - 18.00m; 0.77m of core is missing from 18.00 - 21.00m; 0.08m of core is missing from 27.00 - 30.00m; 0.14m of core is missing from 30.00 - 33.00

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

15.90 0.55 299415.35 Su

16.44 0.54 299515.90 Su

RB-09-234

Hole No: RB-09-235




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

11-Sep-09 -

0.00 5.65 OB Overburden. HF sst cobbles. OB

5.65 19.81 HF Reddish-brown to tan-buff cg-vcg sst and cgl…sst is locally muddy (greenish and reddish-brown intermixed mud) and is often broken and disaggregated in these areas (11.76 – 11.83m, 13.22 – 13.29m, 14.09 – 14.40m)…micaceous…hosts minor to moderate kaolinite alteration of fsp’s throughout…minor chalky white alteration (gypsum?) is also present locally throughout and is often pore-filling…sst/cgl is characterized by a weak to moderate mottled/stratified and pervasive reddish-brown hematite throughout…a spotty, reddish-brown, blotchy hematite is less abundant…hematite alteration is also locally fracture-related…interval is quite broken and fractured throughout and locally has a blocky appearance…fracture are at 10 – 50° TCA but most commonly are 40 – 50° TCA throughout…sst is vuggy throughout (dissolution of mst?)…

Su30 51 - 80Su30 -1 - 40.02 - 0.08

from 5.65 – 6.24m sst is very broken (only fragments of core recovered in places)…hosts abundant reddish-brown mst rip-up clasts locally…

from 6.80 – 7.01m, 7.25 – 7.33m, 7.38 – 7.42m sst is highly broken and partially disaggregated…crush zones(?)…from 7.42 – 7.48m is fractured parallel TCA and there is ~1.50m lost core from 6.00 – 9.00m…

strongly hematitized fractures at 9.00m, 9.15m, 13.92m 15.28m and 16.28m at ~45° TCA…have a reddish-brown, corrosives style hematite along fractured surface…

from 9.15 – 9.78m greenish (anomalous green) mg sst with reddish-brown mottled and spotty hematitization locally…anomalous green colour result of intermixed siltstone and silty mst(?)…

from 16.28 – 16.58m sst hosts minor to moderate beige-yellow alteration (limonite?)…is locally rusty…followed by a greenish, micaceous silty mst from 16.58 – 16.65m and then a strong reddish-brown, strongly hematitized (blotch hematite) in a mg sst…fg disseminated organic detritus is present throughout sub-interval…

at 18.64 – 18.74m sst is fractured at ~10° TCA…organic stain and a beigish-yellow alteration (limonite?) along fracture surface…

from 19.26 – 19.81m polymictic cgl…strongly hematitized (reddish-brown pervasive and fg disseminations) from 19.26 – 19.52m…cgl is fractured at 19.32m at ~45° TCA and has an organic stain along fracture surface…hematite bleeds out into adjacent cgl and overprints clasts away from fracture…

lower contact is sharp

19.81 20.59 HF Reddish, mg sst…massive…characterized by a moderately strong, reddish, mottled/pervasive hematite throughout…minor greenish reduction spots and wisps locally…minor pink lithic fragments…lower contact is sharp at ~45° TCA

Su22 60 - 76Su22 2 - 30.03 - 0.04

20.59 26.07 HF Greenish to reddish-brown clayey-silty mst and siltstone – fg sst with greenish mg-cg sst and cgl towards base of interval…mst is micaceous…hosts minor carbonate caliche throughout and carbonate-rich sections locally…locally strongly weathered…

Su20 57 - 79Su20 -1 - 20.07 - 0.12

from 20.59 – 24.40m is dominantly greenish to reddish-brown clayey – silty mst with lesser interbedded siltstone – fg sst and caliche-rich horizons…dominantly reduced with moderate reddish-brown mottled oxidation…mst is locally very micaceous and locally hosts minor carbonate nodules…from 21.00 – 21.78m mst is strongly oxidized…

RB-09-235



Litho UnitMagnetic


20.59 26.07 from 24.40 – 26.07m dominantly greenish…from 24.40 – 25.29m and 25.53 – 25.72m is mg-cg sst… from 25.29 – 25.33m and 25.72 – 26.07m is cgl…sst is dominantly greenish with weak, mottled, reddish-brown hematite…very micaceous…hosts moderate fg disseminated organic detritus that is locally stratified…often a tan-buff, bleached(?) rim around mottled hematite…cgl is a colourful polymictic cgl and clasts range from granule – cobble size…

lower contact is sharp at ~40° TCA and underlying mst is reduced

26.07 29.00 HF Reddish-brown to greenish…clayey, nodular mst…mst is both oxidized and reduced with oxidation being more prominent…carbonate is tan-buff to reddish-brown in colour…reddish-brown nodules often have a buff, weathered ‘rind’…in places only caliche was recovered (mst completely disaggregated), but in places, nodules are well cemented and core is intact…

Mu25 52 - 80Mu25 -1 - 40.04 - 0.14

from 28.40 – 29.00m reddish-brown to greenish clayey mst is free of carbonate nodules…is both oxidized and reduced and has a granular texture as it grades into underlying sst member…


29.00 33.37 HF Reddish-brown to tan-buff…fg-mg sst and cgl with minor greenish to reddish-brown silty mst that is locally granular…the uppermost portion of interval (from 29.00 – 30.98m) is finer grained (fg-mg sst with local granules and pebbles) and becomes conglomeratic from 30.98 – 33.36m…interval is characterized by a weak to moderate, reddish-brown mottled/pervasive and pervasive/stratified hematite alteration throughout…

Mu20 45 - 76Mu20 -1 - 30.04 - 0.05

from 29.00 – 29.50m mg sst with mottled reddish-brown hematite…massive…

from 29.50 – 29.90m greenish silty-granular mst…small amount of weak, reddish-brown, patchy oxidation followed by a muddy pebble cgl from 29.90 – 30.00m…from 30.00 – 30.14m granular mst section that is reddish-brown with lesser greenish reduction and hosts pebble-sized clasts throughout…

from 30.14 – 30.98m dominantly mg-cg sst with granules and pebbles throughout…

interval becomes a polymictic cgl from 30.98 – 33.36m and clasts are cobble sized and larger (up to 11cm diameter)…poorly sorted…sub-interval is fairly intact except towards the base of sub-interval (from 32.66 – 33.36m) where cgl is broken and partially disaggregated…core locally has a blocky appearance…minor intermixed greenish mud throughout…


33.37 35.81 HF ‘Ruddy’ reddish-brown to greenish siltstone – fg sst with lesser interbedded clayey to silty mst…interval is fairly intact with the exception of mst’s which are moderately weathered…

Mu20 63 - 74Mu20 -1 - 40.06 - 0.08

from 33.36 – 34.42m is strongly oxidized… from 33.36 – 33.54m and 34.16 – 34.42m reddish-brown clayey mst sections at 50° TCA…completely oxidized…

from 34.42 – 35.81m oxidation is being mottled by a greenish, blotchy reduction giving siltstone – fg sst a ‘ruddy’ appearance…siltstone is fractured at 34.53m, 35.37m and 35.40m at 30 – 40° TCA…

lower contact is sharp at 60° TCA and underlying mst is reduced

35.81 40.20 HF Reddish-brown to brown…clayey to silty mst that locally hosts abundant tan-buff to reddish-brown carbonate caliche…interval is strongly oxidized with only weak reduction(?) as charcoal-grey overprinting from 36.84 – 38.08m which gives mst a brownish, rather than reddish-brown, appearance…despite fact that mst is slightly weathered, interval is fairly intact…from 36.80 – 36.90m, 38.24 – 38.52m and 39.00 – 39.23m are caliche-rich sections…

Mu10 60 - 73Mu10 -1 - 30.04 - 0.10

from 39.30 – 39.81m and 39.90 – 40.20m are reddish-brown sst sections…from 39.30 – 39.46m siltstone-fg sst…from 39.46 – 39.81m is fg-mg sst…from 39.90 – 40.20m mg sst…sub-intervals are reddish-brown and moderately well oxidized with minor weak wispy and patchy reduction throughout…sst is fractured at 39.61m at 35° TCA and at 39.90 – 40.02m at ~25° TCA…EOH

RB-09-235



Litho UnitMagnetic


1.50m of core is missing from 6.00 - 9.00m; 0.34m of core is missing from 9.00 - 12.00m; 0.09m of core is missing from 12.00 - 15.00m; 0.04m of core is missing from 15.00 - 18.00m; 0.41m of core is missing from 18.00 - 21.00m; 0.30m of core is missing from 24.00 - 27.00;

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-235

Hole No: RB-09-236




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

11-Sep-09 -


5.14 6.54 HF Tan-buff to yellowish to reddish-brown…cg-vcg sst and cgl…hosts abundant peachy-pink fsp’s that have a beige clay alteration (dickite?) with limonite overprinting(?)…vuggy…interval is badly broken throughout and cgl is partially disaggregated…

Su30 52 - 80Su30 0 - 10.01 - 0.02

from 5.14 – 5.62m is a tan-buff pebble-cobble cgl that is broken throughout and completely disaggregated from 5.44 – 5.62m…

from 5.62 – 6.54m is cg-vcg sst…badly broken and fractured…fracturing ranges from 40 – 70° TCA with the most between 40 – 50° TCA…a weak reddish-brown hematite is locally present on fracture surfaces (rare)…weak kaolinite alteration of fsp’s throughout…micaceous…hosts minor organic detritus (fg disseminated and wispy trash)…has a yellowish appearance locally (limonite overprinting?)…


6.54 14.64 HF ‘Ruddy’ greenish-grey to reddish-brown siltstone-fg sst with lesser greenish clayey mst, mg sst and granule-pebble cgl…interval has a reduced appearance overall and the ‘ruddy’ appearance of siltstone-fg sst appears to be the result of mottling of the oxidation…interval is moderately to strongly weathered and broken throughout…fracturing measures 35 – 50° TCA…

Su20 47 - 87Su20 -1 - 20.03 - 0.09

from 6.54 – 10.61m greenish-grey, strongly weathered clayey-silty mst…micaceous…1.50m of core is lost from 6.00 – 9.00m…

from 9.41 – 10.12m greenish-grey mg sst…from 9.41 – 9.50m mst has a granular to sandy texture…from 9.78 – 10.22m is a sst and cgl section…at 9.78m (contact with overlying mst) has black organic stain…from 9.94 – 10.07m is broken and fractured…bedding instance at ~60° TCA…

from 10.12 – 10.22m is greyish with pink fsp’s and lithic fragments…in sharp contact with underlying mst…this section is anomalous to the Su20 member…

from 10.61 – 14.64m ‘ruddy’ reddish-brown to greenish siltstone–fg sst with minor interbedded greenish mst…siltstone-fg sst is both oxidized and reduced…oxidation is being mottled by patchy and stratified reduction and is also bleached…oxidation is reddish-brown mottled/pervasive and mottled/stratified and has a ruddy appearance…locally vuggy…moderately broken throughout, especially in areas of more significant mst…


14.64 15.76 HF Colourful polymictic cgl…massive to weakly bedded…vuggy…non to weakly calcareous…core is locally broken and fractured…very minor kaolinite alteration as pore-fill locally…lower contact is sharp at 37° TCA and underlying mst is reduced

Su10 62 - 88Su10 00.05 - 0.06

15.76 19.66 HF Reddish-brown to greenish…nodular clayey to silty mst…interval is characterized by the abundance of carbonate caliche and the overall disaggregated appearance of mst…mst is both oxidized and reduced (approximately equal proportions of each)…oxidized and reduced sections, and patchy reduction overprints oxidation…carbonate caliche are buff to reddish-brown in colour and reddish-brown nodules often have buff, weathered ‘rinds’…in places mst is completely disaggregated and only caliche was recovered…from 18.59 – 18.65m and 18.77 – 18.33m siltstone-fg sst that is reddish-brown and locally hosts carbonate caliche as well…

Mu25 52 - 88Mu25 -1 - 40.06 - 0.14

lower contact is sharp, but broken and is strongly reduced from 19.42 – 19.66m

RB-09-236



Litho UnitMagnetic


19.66 25.69 HF ‘Ruddy’ reddish-brown to greenish siltstone-fg sst with lesser interbedded clayey-silty mst and cg sst – cgl…only rare instance of carbonate caliche throughout…siltstone–fg sst is locally broken, often in areas bordering mst sections…

Mu20 58 - 90Mu20 -1 - 30.05 - 0.14

from 19.66 – 20.62m reddish-brown with greenish reduction as patches…siltstone and lesser fg-mg sst…from 19.66 – 20.07m siltstone-fg sst hosts minor carbonate caliche…appears to be bedded at ~40° TCA…

from 20.62 – 20.79m greenish to reddish-brown clayey mst section…

from 20.79 – 22.64m ‘ruddy’ tan-buff to reddish-brown to greenish…mg-cg sst and local colourful, polymictic cgl with minor greenish silty mst–siltstone…sub-interval is characterized by a weak reddish-brown mottled/pervasive hematite throughout that gives sst it’s ‘ruddy’ appearance…from 21.65 – 21.78m is a polymictic cgl section at 37° TCA…cgl section is followed by a greenish silty mst-siltstone that is broken and disaggregated…from 22.01 – 22.09m sst is broken…from 22.62 – 22.64m hosts carbonate nodules that are stratified and section appears to be at ~42° TCA…

from 22.64 – 23.23m reddish-brown, dominantly oxidized, clayey-silty mst with only minor patchy-wispy greenish reduction locally…

from 23.23 – 25.69m ‘ruddy’ reddish-brown to greenish siltstone-fg sst…moderately broken and fractured…fracturing at 23.54m, 24.00m, 24.92m and 25.02m at 32 - 45° TCA and from 24.40 – 24.47m and 24.66 – 24.82 sub-parallel TCA…


25.69 35.78 HF Reddish-brown to brownish…clayey-silty mst and siltstone-fg sst…locally hosts abundant buff to reddish-brown carbonate caliche…interval is dominantly strongly oxidized with only weak charcoal grey to grey-green reduction as patches locally…mst is weathered and partially disaggregated…siltstone-fg sst is intact…interval is fractured locally…fracturing ranges from sub-parallel TCA (a single instance) to 30 – 50° TCA…instances of bedding throughout range from 45 – 55° TCA…

Mu10 62 - 93Mu10 -1 - 40.07 - 0.12

from 25.69 – 29.38m reddish-brown to brownish clayey-silty mst…partially disaggregated…carbonate caliche are rare…massive…from ~27.00 – 28.70m mst is a brownish colour (rather than reddish-brown) and appears to be a result of charcoal grey patchy overprinting (reduction related?)…

from 29.38 – 35.78 reddish-brown…dominantly siltstone-fg sst with lesser clayey-silty mst that is often interbedded…buff to reddish-brown carbonate caliche is locally abundant and ranges in size from <1cm – 3cm diameter…caliche is moderately to well cemented (core is intact)…minor greenish reduction is present throughout as wisps and spots and sometimes surrounding caliche…

lower contact is gradational (same mst, just lacking caliche)

35.78 40.22 HF Reddish-brown to brownish…clayey mst…moderately to strongly weathered and partially disaggregated …interval hosts only minor buff to reddish-brown carbonate caliche…caliche is dominantly small (<1cm diameter)…a weak charcoal grey to greenish patchy overprinting (reduction?) gives the interval a brown rather than the reddish-brown colour...EOH

Mu7 62 - 83Mu7 3 - 40.04 - 0.14

RB-09-236



Litho UnitMagnetic


1.5m of core is missing from 6.00 - 9.00m; 0.14m of core is missing from 9.00 - 12.00m; 1.35m of core is missing from 15.00 - 18.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-236

Hole No: RB-09-237



Total Depth (m): 26

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

12-Sep-09 -

0.00 10.90 OB Overburden. Exotic (granodiorite and rhyolite boulders and cobbles) and HF sst boulder. OB

10.90 11.00 OB Overburden(?). HF Sst boulder. Tan-buff cg sst with hematite disease and minor to moderatek kaolinite alteration of fsp's

OB

11.00 14.00 OB Overburden. Only 0.15m of core recovered over this interval...HF sst…tan-buff, cg-vcg sst and cgl…un oxidized...micaceous…cgl formed of caliche and fsp fragments…not typical of area, suggesting it is actually OB.

OB

14.00 26.00 HF Greyish…cg-vcg sst that locally grades to granule-pebble cgl…interval is characterized by the overall reduced appearance and the abundance of organic trash (fg disseminated organic detritus that is often stratified and larger organic trash fragment, wisps and blebs)…organic trash often has significant fg disseminated py accumulations associated with it…tr – 1% oxidized sulphides (py) throughout…hosts greyish coloured mst rip-up clasts locally which are abundant from ~21.30 – 26.00m…locally vuggy (dissolution of mst)…locally very micaceous…hosts a bright white kaolinite alteration of fsp’s (bright white spekcs)…minor beigish clay alteration (dickite?) that is often stratified with fg organic detritus...bedding instances throughout measure ~45 – 55° TCA…

St 43 - 91St -10.00 - 0.03

from 16.19 – 16.27m a grey-green ‘puggy’ mst section at 55° TCA…very micaceous…abundant fg organic detritus throughout…

from 17.03 – 17.10m core is badly rounded (coring artifact)…

at 17.15m organic trash fragment (coal) with abundant fg py surrounding trash…core is badly rounded (coring artifact)…

from 17.98 – 18.41m sst is moderately broken and has a blocky appearance…from 17.98 – 18.12m sst hosts abundant, large (5cm x 3cm) grey-green mst rip-up chips…

at 18.79m sst is fractured at ~47° TCA...from 18.79 – 19.68m sst is moderately broken and has a blocky appearance…

from 22.66 – 23.00m sst hosts abundant greyish mst rip-up clasts…from 22.66 – 22.79m sst is weakly consolidated…

from 23.00 – 23.57m sst and cgl are somewhat broken and partially disaggregated…from 23.00 – 23.10m sst hosts abundant intermixed mud and is weakly consolidated…from 23.24 – 23.29m and 23.43 – 23.57m cgl is broken and partially disaggregated…

from 24.37 – 24.45m sst and greyish clayey mst are broken…

at 25.05m a small (~1cm diameter) bleb of white, chalky, talc-like clay…no reaction with 10% HCl…powder-like…only instance observed in this ddh…

from 25.90 – 26.00m completely disaggregated sst…EOH

RB-09-237



Litho UnitMagnetic



EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-237

Hole No: RB-09-238




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

12-Sep-09 -

0.00 8.00 OB Overburden. HF sst and exotic (syenite) boulders with some reddish-brown puggy material OB

8.00 11.00 HF Only 0.37m of core recovered in this interval…core recovered consists dominantly of reddish-brown clayey mst to ‘pug’ that hosts reddish-brown carbonate caliche and minor sst…interpreted as a shallow dipping fault as observed in RB-09-237 or possibly an indication of movement along Mu stratigraphy in the area…

Flt 65 - 73Flt -1 - 40.03 - 0.11

from 8.00 – 8.06m tan-buff cg sst with peachy-orange fsp’s…core is cobble sized, broken and somewhat rounded…possible overburden…

from 8.06 – 8.08m are two pebble-sized exotic pebbles which resemble clasts from disaggregated cgl in the area or may also be OB…

from 8.08 – 8.37m reddish-brown clayey mst…strongly oxidized…hosts reddish-brown carbonate caliche throughout…from 8.08 – 8.13m mst is greenish and reduced…hosts buff carbonate caliche

11.00 14.00 HF Only 1.05m recovered from this interval…consists of dominantly reddish-brown, clayey to ‘puggy’ mst that hosts reddish-brown to tan-buff carbonate caliche and some pebbles…highly broken and disaggregated for most of interval…mst resembles Mu member except for the pebbles…

Flt 65 - 88Flt 40.03 - 0.07

14.00 15.49 HF Continuation of previous interval…mixture of clayey-‘puggy’ mst that locally hosts pebbles and sst blocks(?)…

Mu 58 - 83Mu -1 - 40.00 - 0.14

from 14.00 – 14.04m reddish-brown clayey –‘puggy’ mst with minor greenish reduction…

from 14.04 – 14.75m sst that is locally muddy and disaggregated…from 14.04 – 14.15m competent, reddish-brown cg-vcg sst that has significant intermixed greenish mud…from 14.15 – 14.52m tan-buff vcg sst that hosts reddish-brown and greenish mst locally throughout…from 14.52 – 14.59m and 14.62 – 14.68m sst hosts significant greenish intermixed mud, is poorly consolidated and is completely disaggregated from 14.52 – 14.58m…from 14.68 – 14.75m sst has significant intermixed reddish-brown mud and is poorly consolidated…fault gouge(?)…

from 14.75 – 15.24m greenish to brownish clayey mst…massive with minor pebbles/vcg’s of qtz and fsp locally…

from 15.24 – 15.49m grey-green clayey-puggy mst…micaceous…no pebbles visible


15.49 23.14 HF Greyish coloured…cg-vcg sst that locally grades to granule/pebble cgl…interval is characterized by the overall reduced appearance and the abundance of organic trash (fg disseminated organic detritus that is often stratified, organic trash fragments and coal seams) throughout…micaceous…minor fg-mg oxidized sulphides locally throughout…minor beigish coloured clay (dickite?) that is often stratified with fg organic detritus…minor kaolinite alteration of fsp’s throughout (bright white specks)…fg py is present throughout interval as fg disseminations that are locally stratified and as larger accumulations around organic trash +/- possible cpy(?) (trace)…interval is fairly intact…hosts minor greenish-grey to grey mst rip-up clasts locally throughout… a bedding instance at 22.84m is at 35° TCA…

St 51 - 86St -10.00 - 0.01

at 15.60m sst is fractured at ~40° TCA and is broken from 15.60 – 15.62m…

at 16.05m sst is fractured at ~50° TCA…

at 19.19m coal seam ~4-5mm thick oriented at 45° TCA with abundant fg py on coal seam…

RB-09-238



Litho UnitMagnetic


15.49 23.14 at 20.32m a coal seam ~4 – 12mm thick oriented at 65° TCA and has abundant py on coal/organic fragment and through adjacent sst…trace cpy(?)…

at 22.28m coal seam at 25° TCA…trace py…

sst is fractured at 22.93m, 23.97m and 23.04m at 27 – 35° TCA…EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-238

Hole No: RB-09-239




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

13-Sep-09 -

0.00 7.43 OB Overburden. HF sst cobble. OB

7.43 9.96 HF Tan-buff…cg-vcg sst…unoxidized…has moderate kaolinite alteration of fsp’s throughout…fsps are a peachy-orange colour throughout…locally vuggy as a result of dissolution of carbonate (vugs locally effervesce with 10% HCl) and mst…interval is moderately broken and locally has a blocky appearance…

Su 50 - 84Su 00.01 - 0.02

at 7.89m sst is fractured at ~43° TCA…

from 7.89 – 7.95m sst is fractured sub-parallel TCA…

sst is fractured at 9.00m (40° TCA) and 9.02m (50° TCA) and 9.10 – 9.18m (sub-parallel TCA)…

from 9.31 – 9.96m cg-vcg sst is broken, has a blocky appearance and is locally partially to completely disaggregated…

lower contact is sharp, broken and partially disaggregated

9.96 19.34 HF Dominantly reddish-brown to greenish clayey mst that locally hosts reddish-brown to tan-buff coloured carbonate caliche with lesser cg sst that is locally very muddy and weakly consolidated…mst is dominantly strongly oxidized with reduced sections at patches…

Mu 57 - 85Mu -1 - 40.02 - 0.13

from 12.67 – 12.96m greenish granular mst…strongly reduced…hosts abundant intermixed cg qtz and fsp grains…poorly consolidated, broken and partially disaggregated…

from 15.10 – 15.40m, 16.40 – 16.58m and 16.74 – 16.79m are caliche-rich sections…dominantly only caliche recovered with minor reddish-brown clayey mst…caliche are reddish-brown with tan-buff rims…

from 16.16 – 16.25m well cemented, caliche-rich horizon with dominantly reddish-brown caliche (0.5 – 2cm diameter) and minor cg qtz grains throughout…greenish mst cementing nodules…completely intact…

from 16.79 -17.04m sst…from 16.79 – 16.89m weakly consolidated cg sst with significant intermixed greenish-grey mud…broken…from 16.89 – 16.94m is a tan-buff, cg sst block followed by similar cobbles from 16.94 – 17.04m…

from 18.00 – 18.39m tan-buff cg sst that has moderate greenish intermixed mud locally…from 18.14 – 18.16m greenish clayey mst section ~2cm thick, bedded at 55° TCA…from 18.12 – 18.14m is granular…hosts weak reddish-brown mottled hematite from 18.28 – 18.39m…has pink lithic fragments and resembles sst in Su member further up-hole in this ddh…

from 18.39 – 18.44m greenish, clayey – ‘puggy’ mst and greenish mst with abundant cg of qtz and fsp (granular looking), weakly consolidated sst that is partially disaggregated…

from 18.44 – 18.93m clayey mst is both oxidized and redueced…approximately equal proportions of each…

from 18.93 – 19.34m greenish-grey clayey to ‘puggy’ mst…micaceous…from 19.24 – 19.34m mst hosts abundant cg qtz and fsp grains embedded on surface of mst (doesn’t appear to be throughout mst)…

lower contact is sharp at ~40° TCA…

RB-09-239



Litho UnitMagnetic


19.34 47.10 HF Greyish…cg-vcg sst and cgl that is characterized by the overall grey, reduced appearance and the presence of organic trash (large fragments and fg disseminated and stratified organic detritus)…minor greyish mst sections (often <30cm) locally throughout…weak kaolinite alteration of fsps throughout…micaceous…pyrite is present as fg disseminations that are locally oxidized…hosts fg beige-coloured clay alteration (dickite?) that is often stratified with organic detritus…greyish to charcoal grey mst rip-up clasts are locally abundant…minor white, very soft clay alteration (gypsum?) present locally…

St 56 - 85St -10.00 - 0.02

sst is fractured at 19.73m , 19.99m, 21.74m, 21.76m, 22.54m and 22.96m at 45 – 60° TCA…

from 24.46m sst is fractured/broken along a large, greyish mst rip-up clast with a very soft, bright white, clayey alteration (gypsum?)…has been observed interval in smaller quantities elsewhere in ddh…

from 24.72 – 24.82m greyish silty mst section bedded at 65° TCA…very micaceous…

from 26.15 – 26.85m sst hosts greyish to charcoal grey mud and mst rip-up clasts that are stratified…from 26.62 – 26.73m greyish, micaceous, clayey mst with significant white clay specks (gypsum?)…

from 26.85 – 27.13m greyish to charcoal grey, clayey-silty mst…cg-vcg, angular to sub-angular qtz and fsp grains on surface of core…bedded at 60° TCA…

sst is fractured at 27.20m, 27.76m and 28.10 – 28.16m at ~55° TCA…

from 29.24m – 29.60m greenish-grey to charcoal grey clayey mst section…

from 29.60 – 30.91m sst is moderately broken and has a blocky appearance…from 30.21 – 30.28m silty mst and partially disaggregated cgl section…mst has abundant intermixed cg-vcg qtz and fsp grains…

from 34.15 – 34.43m sst is very vuggy (dissolution of mst)…

from 34.76 – 34.84m and 34.92 – 34.98m sst hosts significant intermixed greenish mud, is fractured at ~40° TCA and is broken and partially disaggregated…the later sub-interval is very micaceous and is fg-mg…

at 36.96m sst/pebble cgl is fractured at ~50° TCA…

from 37.60 – 37.63m sst is fractured and partially disaggregated (crushed?)…

from 39.23 – 39.85m sst – pebble cgl is moderately broken and locally has a blocky appearance…at 39.23m and 39.36m sst is fractured at 35 – 45° TCA…

sst is fractured at 40.21m at 40° TCA…

at 40.32m and 42.07m sst is fractured at 50 and 30° TCA respectively…organic stain along fracture surfaces with fg py mineralization associated with organic detritus…the later fracture is followed by a sub-parallel fracture from 42.07 – 47.13m…

from 42.37 – 42.42m sst is badly broken…

from 42.62 – 42.66m sst hosts a large charcoal grey mst rip-up clast…

from 46.85 – 46.90m sst is fractured sub-parallel TCA along a coal fragment…minor py associated with organic trash…

from 46.98 – 47.00m coal seam with significant py mineralization on organic trash and into adjacent sst/pebble cgl…

lower contact is sharp at 40° TCA

47.10 49.12 HF Dark greenish-grey to charcoal grey…clayey-silty mst and siltstone…micaceous…hosts significant organic trash throughout (fg disseminated detritus, coal fragments and wispy organic blebs) which results in the dark colour of this interval…overall, mst/siltstone is in good condition except from 47.10 – 47.38m where silty mst is broken and crumbled…

Mm 52 - 98Mm -10.03 - 0.08

from 47.38 – 48.25 is dominantly siltstone with interbedded clayey mst…

from 48.28 – 48.68m clayey to silty mst…

RB-09-239



Litho UnitMagnetic


47.10 49.12 from 48.68 – 49.12m interbedded clayey-silty mst and siltstone…


49.12 75.27 HF Greyish to tan-buff…mg-vcg sst and granule/pebble cgl with lesser dark greenish-grey to black clayey-silty mst ...interval resembles St member above with abundant organic trash locally throughout, but interval has more abundant peachy-pink lithic fragments throughout and weak to moderate kaolinite alteration of fsp’s that gives the sst a tan-buff colour…interval is moderately broken throughout…hosts minor to abundant greyish-green to charcoal-grey mst rip-up clasts locally…locally vuggy (dissolution of mst)…vugs range in size from minute to >3cm diameter…significant intermixed greyish mud for sections generally <10cm thick and in these areas, sst and cgl are poorly consolidated…micaceous…hosts minor fg disseminated py throughout which is locally abundant (surrounding large organic fragments)… fg oxidized sulphides locally throughout… bedding instances measure 45 – 55° TCA…

Sm 50 - 92Sm -1 - 00.00 - 0.10

at 42.27m sst is fractured along an ~1cm thick organic trash layer at ~70° TCA…two large nodular py masses on fracture surface and fg py in adjacent sst (~3cm up-hole)…

at 42.91m and 42.99m charcoal-grey mst sections (0.5 – 1cm thick) in vcg sst to granule-pebble cgl…sections are at 40° TCA…

at 52.92m sst is fractured at 40° TCA…

from 53.16 – 53.21m sst hosts organic trash (coal) resembling roots…significant fg py surrounding trash and into adjacent sst…

from 53.59 – 53.70m greenish-grey clayey mst section…

at 54.17m sst is fractured along a thin, dark greyish mud bed at 35° TCA…

sst is fractured at 56.67m at 40° TCA…

from 58.08 – 59.21m sst is moderately broken and fractured and sst locally has a blocky appearance…fracturing is at 35 – 50° TCA with most between 40 – 45° TCA…fracturing often follows stratified mud laminae in sst and/or have organic stain along fractured surface…from 58.38 – 58.48m sst hosts organic trash (root-like appearance) with abundant fg py mineralization surrounding trash and into adjacent sst…

sst is fratured at 63.31m and 63.48m at 50° and 60° TCA respectively..

from 64.90 – 65.75m black to dark green-grey, clayey mst…massive…has a shale-like appearance…bedded at 50° TCA…sst at lower contact (65.75 – 65.76m) has a strong, rusty-red hematite alteration (this is the only oxidation observed throughout interval)…

from 67.11 – 67.37m green-grey to black silty mst at 40° TCA…very micaceous…hosts abundant stratified organic detritus throughout…

from 67.52 – 67.83m sst hosts abundant large fragment s of organic trash in addition to significant fg organic detritus and wispy organic blebs…from 67.52 – 67.59m organic trash fragment with py mineralization and the wood grain preserved in mg-cg sst…from 67.69 – 67.76m and 67.81 – 61.83m large coal fragments in cg-vcg sst with py mineralization on fragment…

from 68.51 – 69.10m sst is fractured and broken…from 68.60 – 68.80m and 69.02 – 69.09m sst is highly broken…

from 70.34 – 70.44m grey to charcoal grey silty mst section…very micaceous…gradational into underlying mst…

from 71.59 – 71.62m greyish silty mst with minor intermixed cg qtz and fsp grains throughout giving a sandy texture…micaceous…bedded at 47° TCA…EOH

RB-09-239



Litho UnitMagnetic


1.96m of core is missing from 9.00 - 12.00m; 0.30m of core is missing from 12.00 - 15.00m, 0.95m of core is missing from 15.00 - 18.00m; 0.34m of core is missing from 18.00 - 21.00m; 0.08m of core is missing from 24.00 - 27.00m; 0.20m of core is missing from 30.00 - 33.00m; 0.07m of core is missing from 60.00 - 63.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-239

Hole No: RB-09-240




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

14-Sep-09 -

0.00 7.00 OB Overburden. HF sst pebbles, cobbles and boulders. OB

7.00 7.07 OB From 6.65 – 7.00m is a reddish-brown to earthy-brown mg sst…very micaceous…hosts reddish-brown to earthy-brown pervasive-stratified hematite…fg disseminated organic detritus throughout…sst is moderately broken and has a blocky appearance…broken along bedding parallel laminations…stratifications and fracturing at 45 – 60° TCA…

OB

from 7.00 – 7.07m is a granodiorite(?) cobble with reddish-brown clayey-puggy mst with intermixed exotic pebbles and cg-vcg qtz and fsp grains throughout…if this cobble was not present, it would appear that OB ended at 6.65m. However, with this exotic cobble, it would suggest that the overlying sst is actually overburden.

7.07 7.92 HF Reddish…cg sst…micaceous…characterized by a mottled/pervasive and locally pervasive/stratified hematite alteration with minor, more intense, reddish-brown patchy hematite…minor to moderate kaolinite alteration of fsp’s…massive…lower contact is sharp and appears to be at ~80° TCA

Su 62 - 93Su -1 - 30.01 - 0.03

7.92 24.42 HF Reddish-brown to greenish…dominantly clayey mst with local caliche sections and lesser siltstone and mg-cg sst…interval is dominantly oxidized with local reduced patches and sections throughout…interval is weathered and broken making the distinction between structure and coring/weathering artifacts difficult…from ~21.20 – 24.83m interval is reduced with only minor remnant oxidation…hosts minor yellowish limonite alteration locally…caliche-rich sections are from 11.40 – 11.62m, 13.57 – 13.66m, 14.82 – 14.92m, 14.98 – 15.13m, 15.27 – 15.32m, 17.12 – 17.56m, 17.81 – 18.52m, 18.70 – 19.04m…

Mu 60 - 90Mu -1 - 40.02 - 0.17

from 7.92 – 8.11m greenish-grey silty mst…a reddish-brown mg-cg, strongly hematitized micaceous sst cobble with tan-buff (bleached) spots and is followed by reddish-brown clayey mst…from 8.00 – 11.00m only 18cm of core was recovered (fault?)…

from 15.53 – 15.75m greenish sandy mst section…dominantly greenish with minor reddish-brown oxidation…significant intermixed mg-cg grains of qtz and fsp…granular mst…

from 18.18 – 18.41m greenish, reduced, very micaceous, silty mst – siltstone…hosts weak reddish-brown patchy hematite…

from 20.90 – 23.10m silty mst – siltstone to granular mst and minor cg sst and cgl…sub-interval is strongly reduced with only weak to moderate remnant patchy and stratified oxidation…micaceous to very micaceous…from 20.90 – 21.24m silty mst with minor intermixed sand (granular texture)…from 22.12 – 22.32m intermixed mst and mg-cg sst with local weak to moderate reddish-brown oxidation that is stratified…from 22.32 – 22.62m tan-buff to greenish mg-cg sst with intermixed green mud that becomes less significant with depth within sub-interval…from 22.33 – 22.61m hosts an underdeveloped fracture sub-parallel TCA...from 23.04 – 23.10m is a pebble cgl section composed of pebble-sized clasts of qtz and fsp with greenish intermixed mud…

from 24.16 – 24.42m greenish clayey-puggy mst…very micaceous…strongly reduced…at 55° TCA

RB-09-240



Litho UnitMagnetic


24.42 49.92 HF Greyish to tan-buff…mg-vcg sst and cgl with minor green-grey to charcoal grey mst locally…sst locally hosts grey to charcoal grey intermixed mud…muddy areas are often weakly consolidated, broken and partially disaggregated…interval is characterized by the abundance of organic trash (fg disseminated and stratified organic detritus, wispy organic blebs and large coal fragments)…micaceous…trace to 1% fg disseminated py and oxidized sulphides..locally pitted (dissolution of mst rip-up clasts)… hosts minor beige clay (dickite?) locally that is often stratified…stratifications are at 35 – 40° TCA…bedding instances vary from 35-40° TCA throughout…moderately broken and fractured throughout…fracturing is at 30 – 90° TCA…core locally has a blocky appearance…

St 51 - 81St -10.01 - 0.12

from 24.76 – 25.36m sst is moderately broken and fractured and has blocky appearance…fractures(?) are at ~90° TCA…

at 26.63m sst is fractured at 45° TCA along a dark grey, very micaceous silty mst…

from 27.24 – 27.82m sst hosts significant dark greyish mud throughout (mst rip-up clasts, mst laminae and interbedded mst)…moderately broken and has a blocky appearance…sst is fractured at 40 – 50° TCA and ~90° TCA throughout…from 27.24 – 27.26 and 27.73 – 27.82m greenish-grey to dark grey mst sections…the later interval is very micaceous…from 27.65 – 27.74m sst hosts abundant wispy organic detritus that is stratified…

at 28.00m sst is fractured at 45° TCA and has organic stain(?) on fracture surface…

from 30.25 – 30.28m dark to charcoal grey clayey mst (organic-rich)…very micaceous…minor intermixed mg-cg qtz and fsp grains…bedded at ~60° TCA…

from 30.32 – 30.41m muddy sst hosts abundant wispy organic detritus that is stratified and larger vitreous-looking coal fragments throughout…at 30.40m fractured at 30° TCA…from 30.40 – 30.55m sst is fractured parallel TCA…

from 34.57 – 34.84m cg-vcg sst has significant intermixed greenish-grey to dark grey mst…sst is weakly consolidated and is locally partially disaggregated…

from 37.92 – 37.98m greenish-grey clayey-silty mst at ~50° TCA…

from 37.98 – 39.84m sst and cgl is moderately broken and fractured and has a blocky appearance locally…from 38.60 – 38.66m is a greenish-grey to charcoal grey, micaceous, clayey mst…from 38.73 – 38.90m sst is badly broken and fractured…fracturing measures 40 – 45° TCA…

at 39.26m sst hosts coal fragments along fractured sst surfaces…minor fg py surrounding coal fragment…tr – 1% py and oxidized sulphides in adjacent sst…sst fractured at 45° TCA…

at 39.88 – 39.89m vitreous looking coal seam at 40° TCA…trace py associated with trash…

from 40.41 – 40.55m, 41.00 – 41.08m, 41.17 – 41.20m and 41.36 – 41.52m is moderately broken and locally disaggregated…

from 47.60 – 48.09m sst hosts mst rip-up clasts that are locally eroded giving sst a pitted appearance…

from 48.09 – 48.17m is a green-grey to charcoal grey silty mst section with minor intermixed mg-cg qtz and fsp grains resulting in a granular texture…


at 49.50m sst is fractured at 55° TCA…EOH

RB-09-240



Litho UnitMagnetic


2.82m of core is missing from 8.00 - 11.00m; 0.10m of core is missing from 14.00 - 17.00mEOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-240

Hole No: RB-09-241




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

15-Sep-09 -

0.00 9.00 OB Overburden. HF sst cobble...exotic (rhyolite, granite and gabbro) pebbles and cobbles...reddish-brown, puggy mst with intermixed exotic pebbles…

OB

from 6.00 - 9.00m only 0.24m recovered

9.00 28.37 HF Reddish-brown to greenish to charcoal grey…clayey-silty mst and siltstone that is locally nodular…lesser reddish-brown to greenish to tan-buff fg-cg sst…

Mu 50 - 90Mu -1 - 40.04 - 0.08

from 9.00 – 10.53m dark green, dominantly siltstone with lesser clayey-silty mst…micaceous…from 10.24 – 10.53m clayey mst that is broken and partially disaggregated…

from 10.53 – 13.98m tan-buff cg-vcg sst…tan-buff colour is result of abundant peachy-pink fsp (lithic fragments)…sub-interval is virtually unoxidized…sst has a weak to moderate kaolinite alteration throughout (alt of fsp’s)…micaceous… bedded at 50° TCA…broken and fractured throughout…from 12.00 – 12.82m sst is moderately to highly broken and fractured...fracturing is at 25 – 55° TCA and sub-parallel TCA…from 12.26 – 12.38m and 12.66 – 12.82m sst is highly broken and core is somewhat rounded…from 13.05 – 13.98m greyish to greenish mud (intermixed and as mst rip-up clasts)…from 13.78 – 13.89m greenish-grey, micaceous, clayey mst section at 30° TCA…

from 13.98 – 16.30m reddish-brown to greenish clayey-silty mst…both oxidized and reduced (approximately equal proportions of each)…from 13.98 – 14.20m mst is nodular with buff to reddish-brown carbonate caliche (0.5cm - ~3cm diameter)…interval grades into underlying siltstone section…

from 16.30 – 19.03m reddish-brown to greenish to tan-buff siltstone and fg-mg sst that locally has a ‘ruddy’ appearance…weak, mottled and mottled/stratified reddish-brown hematite throughout results in the ‘ruddy’ appearance…bedded at ~50° TCA…from 16.30 – 16.81m and 18.92 – 19.09m reddish-brown to greenish, well laminated siltstone and fg-mg sst…micaceous…greenish mud laminae are at ~45° TCA and fracturing parallels these laminae…from 18.32 – 18.66m sst is highly broken and fractured…fracturing is at 80 – 90° TCA…

from 19.09 – 21.04m charcoal grey to green-grey dominantly siltstone and minor silty mst…micaceous…massive…from 19.09 – 19.30m charcoal grey coloured…

from 21.04 – 28.37m reddish-brown to greenish clayey–silty mst that is locally nodular and minor sst with local muddy sst and granular mst…interval is dominantly oxidized with reduced patches and sections locally…interval is badly broken and weathered…

from 21.04 – 21.76m a tan-buff to greenish, well cemented caliche section…moderately broken and partially disaggregated especially in mud-rich areas…at 21.30m is fractured at 45° TCA…from 21.30 – 21.32m is broken, greenish mst and sst rubble…from 21.53 – 21.76m sst/mst/caliche intermixture is broken and partially disaggregated…

from 21.76 – 27.14m dominantly reddish-brown clayey-silty nodular mst…locally caliche-rich (only caliche recovered)…is dominantly oxidized with minor to moderate greenish reduction as patches and sections locally…mst locally has significant qtz and fsp grains…from 23.82 – 24.15m and 27.11 – 27.85m are granular mst sections…from 27.15 – 27.33m is a cg sst with minor greenish mud as laminae and an intermixture…from 25.60 – 28.37m is dominantly reduced...


RB-09-241



Litho UnitMagnetic


28.37 59.98 HF Greyish mg-vcg sst and cgl…micaceous…interval is characterized by an overall reduced appearance and the abundance of organic trash throughout (fg disseminated and stratified detritus, wispy organic blebs, larger coalified wood fragments)…interval hosts tr – 1% fg disseminated py and localy py accumulations associated with larger organic trash fragments…<1% fg oxidized sulphides…interval is moderately broken and fractured throughout…fracturing measure 40 – 70° TCA but is most often 45 – 55° TCA…locally badly broken and partially to completely disaggregated (crush zones?)…sst locally hosts significant intermixed greenish-grey to grey, clayey-silty mst, mst laminae and rip-up clasts…mst-rich sections are weakly consolidated…locally vuggy (dissolution of mst chips)…hosts weak to moderate kaolinite alteration of fsp’s…minor beige clay (dickite?) is often stratified with organics…hosts minor white, chalky alteration locally throughout (gypsum?)…gypsum was reportedly observed in high grade boulders (SRC petrography)…gypsum(?) is most significant from ~45.00 – 59.98m…sst locally has a tan-buff appearance as a result of the abundant peachy-pink lithic fragments…bedding instances measure 40 – 70° TCA…

St 52 - 88St -10.00 - 0.03

from 38.40 – 42.02m sst is badly broken and completely disaggregated…crush zone(?)…

from 42.86 – 43.02m and 46.73 – 46.83m cgl is broken…

from 46.70 – 46.95m sst and cgl is broken and partially disaggregated…

at 47.85m large k-fsp fragment is partially altered (replaced by gypsum?)…

from 50.52 – 50.66m large, coalified wood fragment (roots?)…abundant fg py mineralization surrounding fragments…trace cpy observed (sampled for geochem)…EOH

2.76m of core is missing from 6.00 - 9.00m; 1.17m of core is missing from 9.00 - 12.00m; 2.20m of core is missing from 12.00 - 15.00m; 1.29m of core is missing from 24.00 - 27.00m; 0.26m of core is missing from 27.00 - 30.00m; 0.10m of core is missing from 42.00 - 45.00m; 0.27m of core is missing from 45.00 - 48.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

17.40 0.55 299716.85 Mu

17.95 0.55 299817.40 Mu

18.50 0.55 299917.95 Mu

19.06 0.56 300018.50 Mu

50.66 0.14 299650.52 St

RB-09-241

Hole No: RB-09-242




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

16-Sep-09 -

0.00 6.00 OB Overburden. HF sst cobbles OB

6.00 12.48 HF Reddish-brown to tan-buff…cg-vcg sst...highly broken and fractured throughout and core has a blocky appearance for most of interval...fracturing is at 30-45° TCA but is most commonly at 30-40° TCA...fracture surfaces are locally moderately hematized +/- minor manganese(?) staining...fsp’s are peachy-pink in colour throughout...a bright white clay alteration (pore-fill) (gypsum/kaolinite?) is abundant throughout as bright white specks...interval is characterized by a weak to moderate reddish-brown, mottled hematite and minor pervasive and stratified hematite throughout...core is locally vuggy (dissolution of mst rip-up clasts)...micaceous...

Su 44 - 89Su -1 - 30.01

from 9.43 - 9.67m and 9.78 - 9.93m, 10.61 - 10.66m and 10.72 - 10.78m sst is highly broken and partially disaggregated...sst rubble is locally moderately to strongly hematized…

lower contact is sharp, strongly oxidized and broken...underlying mst is strongly reduced

12.48 32.50 HF Greenish to reddish-brown…clayey-silty mst that is locally nodular with lesser slt-fg sst and mg-cg sst...from 12.48 - 21.62m is reduced and from 21.62 - 30.00m is oxidized…lower contact (from 30.00-32.50m) is dominantly reduced...mst’s throughout are moderately weathered and partially disaggregated making the distinction between structure and weathering/coring artifacts difficult...

Mu 54 - 88Mu -1 - 40.00 - 0.12

from 12.48 - 21.62m greenish clayey-silty mst, slt – fg sst and mg sst...sub-interval is dominantly reduced with only minor reddish-brown mottled and patchy oxidation locally...mg sst is micaceous, hosts moderate fg diss stratified organic detritus and larger, wispy organic blebs towards the base of sub-interval (~21.20 - 21.62m)...greenish colour of sst’s is the result of greenish mst laminae... a weak reddish brown mottled hematite is present locally…from 12.48 - 14.47m strongly reduced greenish clayey mst with strongly oxidized, reddish-brown patches at 13.36 - 13.40m and 13.56 - 13.57m...from 14.47 - 15.56m is a tan-buff, unoxidized cg sst that becomes vcg from 15.42 - 15.56m...tan-buff colour is a result of abundance of pink-peach fsp’s…from 15.56 - 15.95m mst’s host abundant buff coloured carbonate caliche...from 15.95 - 20.38m interbedded silty mst, slt - fg sst...from 20.38 - 21.62m tan-buff to greenish, fg-mg-sst that hosts abundant fg organic trash that is locally stratified...

from 21.62 - 32.50m is dominantly reddish-brown, clayey-silty nodular mst...only minor caliche throughout most of sub-interval, but caliche-rich sections are locally present...mst is completely disaggregated with only caliche recovered...caliche is reddish-brown to buff coloured...interval is strongly oxidized throughout with only patchy and wispy greenish reduction present locally...from 21.86 - 22.08m is a reddish-brown to greenish fg-mg sst that is broken...from 23.26-24.18m is a patchy, weak to moderately strong limonite alteration...from 28.38 - 28.28.67m is a caliche-rich section...from 30.00-32.50m is dominantly reduced mst...

from 32.77 - 32.89m, greyish mg-cg sst at 45° TCA…


32.50 41.76 HF Greyish…cg-vcg sst and minor granule-pebble cgl...locally bedded...interval is characterized by the overall reduced appearance and the presence of significant organic trash throughout (fg disseminated organic detritus that is often stratified and small organic fragment and wisps)... micaceous…sst hosts fg disseminated py (tr) and oxidized sulphides (tr-1%)...moderate bright white specks of clay alt throughout...sst hosts minor small greenish-grey mst rip-up clasts throughout…vuggy...sst is moderately broken and fractured...fractures measure 40 - 50° TCA and fractures locally have an organic stain...bedding instances measure 45 - 60° TCA

St 62 - 78St -10.00 - 0.03

RB-09-242



Litho UnitMagnetic


32.50 41.76 at 36.76m sst is fractured at ~45° TCA along a greyish, silty, v. micaceous, clayey mst…

at 36.87 - 36.90m greyish clayey mst section…

at 38.25 - 38.29m sst is fractured at ~45° TCA…sheared fabric(?) in adjacent sst...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

10.39 0.48 39019.91 Su

10.87 0.48 390210.39 Su

11.35 0.48 390310.87 Su

11.83 0.48 390411.35 Su

12.30 0.47 390511.83 Su

16.51 0.52 390615.99 Mu

17.03 0.52 390716.51 Mu

17.55 0.52 390817.03 Mu

18.08 0.53 390917.55 Mu

18.60 0.52 391018.08 Mu

RB-09-242

Hole No: RB-09-243




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

17-Sep-09 -

0.00 5.13 OB Overburden. HF sst pebbles and cobbles and exotic pebbles. OB

5.13 6.71 HF Tan-buff…mg-cg sst and polymictic cgl...moderately broken…from 5.13 - 6.12m cgl is badly broken and locally partially to completely disaggregated...sst hosts moderate fg diss organic detritus that is stratified...fsp’s are peach to pinkish in colour and the abundance of these fsp’s gives sst a tan-buff colour...moderate kaolinite alteration of fsp’s...interval is unoxidized...minor muscovite throughout...

Su 60 - 95Su 00.02 - 0.04

from 5.13 - 6.12m polymictic conglomerate is highly broken and locally partially to completely disaggregated…from 6.12 - 6.71m mg-cg sst...massive...some fracturing throughout...fractures are at 60 - 70° TCA...at 6.41m an underdeveloped fracture at 75° TCA…lower contact is sharp at ~80° TCA and underlying slt is broken

6.71 26.06 HF Greenish to reddish-brown to tan-buff coloured…dominantly clayey - silty mst and slt-fg sst with lesser cg-vcg sst and granule cgl...from 6.71 - 14.28m is dominantly cg-vcg sst and cgl with lesser silty mst-slt and from 14.28 - 26.06m is the more characteristic Mu member (nodular mst with lesser slt)…

Mu 50 - 103Mu -1 - 30.03 - 0.15

from 6.71 - 14.28m tan-buff to greenish cg-vcg sst and granule cgl with lesser interbedded greenish silty mudstone-silt and fg sst...sst/cgl locally hosts abundant greenish mst rip-up clasts and intermixed mud that gives the sst a greenish appearance...sst is moderately micaceous, hosts weak to moderate kaolinite alt of fsp’s...locally vuggy (dissolution of carbonate(?) as sst is locally weakly calcareous)...sharp contact with underlying mst that is broken...from 8.08 - 8.40m, 8.67 - 9.08m and 9.62 - 10.14m greenish, clayey-silty mst sections are moderately weathered and broken…minor interbedded slt locally...from 8.10 - 8.33m weak reddish-brown, remnant oxidation...from 9.08 - 9.36m and 12.00 - 12.74m greenish-grey to charcoal grey slt that strongly resembles St Mbr...abundant stratified fg organic detritus…v. micaceous...at 12.74m slt contact with underlying cg sst is sharp…from 12.73 - 12.74m vuggy mst…faulted contact(?)…from 11.65 - 11.82m dark, charcoal grey slt-shl...massive…underlying sst (from 11.82 - 12.00m) hosts abundant, large (~3cm diameter) mst rip-up clasts that resemble overlying slt-shl…from 7.84 - 7.94m and 10.95 - 11.33m mg sst is fractured and broken...sst is fractured sub-parallel TCA…from 8.50 - 8.54m granule cgl hosts abundant greenish mst rip-up clasts…broken and partially disaggregated…from 14.28 - 26.06m is the typical Mu Mbr...greenish to reddish-brown, clayey-silty mst and slt-fg sst with minor thin (3-5cm thick) interbedded mg-cg sst locally...interval is dominantly reduced with minor patchy and wispy reddish-brown oxidation locally, except from ~20.70 - 25.00m where mst is oxidized with minor reduced sections and greenish reduced patches...from 14.28 - 14.92m, greenish caliche-rich mst...strongly weathered and disaggregated with only caliche recovered from 14.49 - 14.74m...caliche is buff to reddish-brown in colour and is often broken carbonate-rich horizon (caliche fragments) rather than nodules...marker nodular mst...

RB-09-243



Litho UnitMagnetic


6.71 26.06 from 14.92 - 20.80m greenish to reddish brown slt-fg sst and mg-cg sst with lesser interbedded clayey-silty mst...sub-interval has a vuggy appearance as a result of reddish-brown oxidation with greenish reduction overprinting...micaceous throughout (locally v. micaceous)…partly weathered…hosts moderate to abundant fg diss organic detritus that is often stratified...from 19.16 - 19.67m greenish to reddish-brown, clayey - silty mst that hosts moderate small caliche throughout…from 20.17 - 20.31m dark green to reddish-brown… v. micaceous…organic rich clayey mst…

from 18.14 - 19.18m tan-buff to greenish…mg-cg sst...greenish mst laminae and mst rip-up clasts throughout...locally v.micaceous…hosts abundant fg diss organic detritus that is often stratified…from 20.80 - 26.06m greenish to reddish-brown…clayey - silty mst and minor interbedded cg sst...sub-interval is both oxidized and reduced (approx equal proportions of each)...mst is locally nodular...nodules are buff to reddish-brown and range in size from <0.5 – >3.0cm diameter with most 0.5 – 1cm diameter...minor weak yellowish limonite alteration present locally...from 22.40 - 22.48m tan-buff to reddish-brown cg sst at ~75° TCA…

from 23.28 - 24.02m reddish-brown mst hosts more abundant nodules than rest of sub-interval…

from 25.38 - 26.02m mst is strongly reduced and is virtually free of caliche…


26.06 43.72 HF Greyish…cg-vcg sst and granule-pebble cgl with lesser interbedded greenish-grey to charcoal grey mst...sst hosts moderate to abundant organic trash (fg diss organic detritus that is often stratified, wispy organic blebs and fragments)...hosts greyish to greenish-grey mst rip-up clasts that are locally abundant...sst hosts minor (<1%) fg diss py throughout...py is locally abundant surrounding organic trash and organic-rich sections and is locally as massive py accumulations...moderate to strong kaolinite alt of fsp’s...fsp’s are locally a pale peach colour which gives the sst a tan-buff rather than greyish colour...sst is badly broken and locally partially disaggregated...vuggy (dissolution of mst)...minor beige clay (dickite?) throughout that is often stratified...

St 58 - 99St -1 - 20.00 - 0.04

from 31.08 - 31.16m sst is muddy (intermixed greyish mud) and broken (at ~80° TCA)…

from 31.80 - 32.25m sst is broken and fractured and has a blocky appearance...fracturing measures ~75-90° TCA... from 32.38 - 35.57m and 37.73 - 39.33m sst is moderately to badly broken and locally has a blocky appearance...from 32.38 - 33.24m, 34.15 - 34.22m, 34.33 - 34.39m, 34.60 - 35.57m and 40.72 - 40.99m are highly broken and partially to completely disaggregated...crush zones (?)...from 36.27 - 36.50m highly broken…from 35.44 - 35.57m and 37.19 - 37.36m sst is fractured parallel TCA…

at 41.25 - 41.30m charcoal grey-black clayey mst section (core underneath is rounded) with broken sst core that is almost completely py…at 43.41m appears to be an oxidation front as sst hosts a weak reddish-brown pervasive hematite as well as very strong reddish brown fracture-related hematite at 43.45m…hematite bleeds into adjacent sst (43.40 - 43.47m) with patchy reddish-brown hematite in area as well...lower contact is sharp and broken...the end of this member is based on the introduction of oxidation and the possibility that mst underneath is the Mm Mbr and the lack of organic detritus in underlying mst

43.72 43.79 HF Charcoal grey to reddish-brown silty mst...granular...micaceous...organic rich...underlying sst hosts abundant fg py at contact with mst…

Mm 70 - 84Mm -1 - 20.06 - 0.07

lower contact is sharp and appears to be erosional

RB-09-243



Litho UnitMagnetic


43.79 59.49 HF Reddish-brown to reddish to tan-buff…cg-vcg sst and granule-pebble cgl with minor granular mst sections...sst/cgl hosts minor to moderate grey-green to reddish-brown mst rip-up clasts throughout... weak kaolinite alt of fsp’s throughout ...moderately micaceous…interval is characterized by a reddish-brown to reddish hematite alt throughout that is mottled, pervasive/mottled , stratified/pervasive, mottled/stratified, spotty hematite disease and fracture-related...sst hosts minor organic trash throughout (fg diss and stratified detritus)…significantly less trash than overlying St Mbr...interval is moderately broken locally, but is, for the most part intact with good core recovery... fracturing throughout ranges from ~30 - 90° TCA with most between 50-70° TCA...

Sm 49 - 92Sm 1 - 40.01 - 0.11

at 45.89m strongly hematized fracture at ~ 45° TCA...has an oily appearance…

at 48.75 and 48.77m strongly hematized fracture at 70-75° TCA...from 48.68 - 48.83m strong reddish pervasive hematite…from 49.63 - 49.68m, 52.09 - 52.17m, 52.87 - 52.89m and 54.70 - 54.85m are reddish-brown to dark grey granular mst sections...fault zones (?)...sections are at 60 - 90° TCA with most at 60 - 70° TCA…at 50.06m sst is fractured at ~30° TCA and is moderately hematized…

from 54.74 - 54.96m and 57.97 - 59.49m sst hosts abundant greyish-brown to greenish mst rip-up clasts…at 57.87m very strongly hematitized fracture (hematite vein?)…sst is completely replaced by hematite and has an oily appearance...from 57.84 - 57.91m complete replacement by hematite…fracture is at ~50° TCA...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

6.71 0.46 39116.25 Su

9.94 0.48 39129.46 Mu

10.42 0.48 39139.94 Mu

10.90 0.48 391410.42 Mu

11.40 0.50 391510.90 Mu

15.40 0.52 391614.88 Mu

15.92 0.52 391715.40 Mu

16.44 0.52 391815.92 Mu

16.96 0.52 391916.44 Mu

RB-09-243

Hole No: RB-09-244




Core Size: BQTK


License: 016221M




mE / mN



Test Depth (m)



Member

17-Sep-09 -

0.00 6.65 OB Overburden. HF sst cobbles and boulders and minor exotic (gabbro) pebbles and cobbles OB

6.65 18.46 HF Greyish...mg-vcg sst and cgl with minor charcoal grey to greenish-grey clayey-silty mst beds and sections...interval is characterized by the overall reduced appearance and the abundance organic trash (fg diss organic detritus that is often stratified, wispy organic blebs and larger organic fragments)...sst hosts minor fg diss py that is locally oxidized..py is more abundant (nearly massive) surrounding organic trash fragments and into adjacent sst...sst hosts minor greenish-grey mst rip-up clasts...sst is locally vuggy (dissolution of mst)...moderate to strong kaolinite alt of fsp throughout...fsp’s are locally a pale peach colour which gives sst a tan rather than greyish colour...hosts minor beige clay (dickite?) that is locally stratified...micaceous (locally v.micaceous)...sst-cgl is moderately broken and fractured throughout with fractures ranging from 55-90° TCA...

St 61 - 96St -10.00 - 0.02

at 7.18 - 7.23m is a strongly pyritized organic fragment...adjacent sst is also pyritized within this zone…

from 7.32 - 7.44m sst is fractured sub-parallel TCA...and following sst from 7.44 - 7.49m is muddy, broken and partially disaggregated…

from 7.58 - 7.64m sst is fractured sub-parallel TCA...

from 7.64 - 9.17m (1.26m lost from 6.00 -9.00m) is a greenish-grey, granular mst section that is partially disaggregated...mst hosts abundant mg-vcg grains of qtz and fsp throughout...patchy charcoal grey mst locally…

greenish-grey to charcoal-grey mst sections from 11.91 - 11.94m (at ~85° TCA), from 11.97-12.14m (locally granular) and from 12.91 - 12.97m…

from 12.33 - 12.62 sst is moderately broken and core has a blocky appearance…

lower contact is sharp at ~90° TCA and is strongly hematized (reddish-brown, pervasive hm) from 18.42 - 18.46m

18.46 18.60 HF Greenish-grey to reddish-brown...clayey-silty mst...dominantly reduced with strong, patchy, reddish-brown oxidation...organic-rich...lower contact is sharp at ~90° TCA

Mm 58 - 89Mm -1 - 30.06 - 0.10

18.60 30.22 HF Tan-buff to reddish-brown...cg-vcg sst and cgl with minor greenish-grey to charcoal grey to reddish-brown mst locally...hosts minor to moderate greenish-grey to reddish-brown mst rip-up clasts throughout...tr fg diss py... micaceous...moderate kaolinite alt of fsp’s...fsp’s are a pale peach colour...moderate fg diss organic detritus locally that is often stratified with minor beige clay (dickite?)...interval is characterized by a weak to moderate reddish-brown hematite alt that is as “hematite disease”, blotchy and to a lesser extent, fracture-related...sst is moderately broken and fractured locally...fractures range from 55 - 80° TCA with most ~70 - 75° TCA...

Sm 58 - 84Sm 1 - 20.01 - 0.09

mst sections are from 18.80 - 18.87m, 25.17 - 25.30m, 28.64 - 28.71m and 29.80 - 30.22m…

from 18.90 – 19.21m cgl is broken and locally has a blocky appearance...from 18.97 - 19.11m, cgl is highly broken and partially disaggregated…

from 29.69 - 29.80m sst is fractured sub-parallel TCA and has moderate reddish-brown hematite along fracture surface…

strongly hematized fractures are at 21.09m (~90° TCA), 28.95m (~70° TCA) and 29.18m (~85° TCA)…

RB-09-244



Litho UnitMagnetic


18.60 30.22 at 26.52m carbonate vein (space-filling crystals)…

from 29.18 - 29.80m reddish mg-cg sst with abundant fg organic detritus that is stratified...v. micaceous...strongly resembles St Mbr but with oxidation…

from 18.46 – 30.22m may all actually be St Mbr with an oxidation front(?)...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-244

Hole No: RB-09-245




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

22-Sep-09 -


7.59 12.70 HF ‘Ruddy’, pale reddish-brown to greenish slt and fg sst that is locally conglomeratic (granule cgl sections) with lesser clayey-silty mst...interval in both oxidized (reddish-brown) and reduced (greenish)…

Mu20 58 - 92Mu20 -1 - 40.04 - 0.12

from 7.59 - 9.55m slt-fg sst is a pale reddish-brown colour and hosts significant tan-buff carbonate caliche, caliche fragments and wispy fragments...from 8.65 - 9.22m slt-fg sst is highly broken and fractured...fracturing at 30-35° TCA ...from 9.09 - 9.20m is a reddish-brown clayey mst section with tan-buff carbonate caliche towards base of sub-interval (9.18 - 9.20m)...

from 9.22 - 12.70m pale, ‘ruddy’ slt-fg sst and clayey mst...from 9.65 – 9.78m slt-fg sst is conglomeratic (granule cgl)...from 9.44 - 10.03m slt-fg sst hosts tr – 1% diss oxidized py…

at 9.42m fg sst is fractured at ~25° TCA…

from 10.11 - 10.76m reddish-brown to greenish clayey mst...from 10.11 - 10.26m mst is strongly reduced and hosts reddish-brown to tan-buff carbonate caliche throughout...from 10.26 - 10.76m is strongly oxidized, reddish-brown mst…

from 11.41 - 11.74m reddish-brown clayey mst…

at 12.03m slt is fractured at 50° TCA and is strongly reduced…

fracturing at 12.15m (20° TCA), 12.24m (45° TCA), 12.46m (40° TCA) and 12.64m (55° TCA)…

lower contact is sharp at 40° TCA and underlying mst is strongly reduced

12.70 42.98 HF Reddish-brown to brownish...clayey-silty mst that is locally nodular with minor slt-fg sst...interval is moderately weathered and partially disaggregated...dominantly oxidized with minor greenish reduction as spots, patches and wisps...from 38.00 – 42.98m is strongly reduced...

Mu10 42 - 104Mu10 -1 - 40.06 - 0.15

from 12.70 - 18.18m is clayey mst that hosts only rare, small (<1cm diameter) carbonate caliche...from 12.70 - 12.80m mst is strongly reduced...from 12.80 - 14.78m and 17.65 - 18.18m mst is a brownish colour as it has a charcoal grey overprint (reduction related?) and gives mst a brownish rather than reddish-brown colour...

from 18.18 - 32.48m mst is nodular...nodules range from 1mm - >3.5cm diameter...mst is locally very nodular and mst is almost completely disaggregated...local caliche fragment horizons...caliche are buff to reddish-brown to greenish in colour…

from 18.18 - 18.70m and 19.50 - 19.90m reddish brown slt that hosts minute (1-2mm diameter), buff carbonate caliche and caliche fragments...sst is moderately fractured and broken locally...slt is fractured at 18.20m (50° TCA), 18.25m (50° TCA) and 18.47 - 18.59m (15° TCA), from 19.50 - 19.65 (broken) and 19.75 - 19.90m (fractured parallel TCA)...

from ~21.33 - 23.52m nodular slt-fg sst...its competent nature identifies it from the surrounding mst…

from 27.00 – 31.00m mst is very nodular, strongly weathered and partially disaggregated…

from 32.48 - 36.26m reddish-brown mst is caliche-free…

from 36.26 - 42.98m pale green to dark greenish-grey clayey-silty mst that has increasing organic content with depth...mst has minor interbedded slt and fg-cg sst…

RB-09-245



Litho UnitMagnetic


12.70 42.98 from 36.26 - 37.65m pale green clayey mst...micaceous...hosts minor reddish-brown to pale green interbedded slt and fg sst...from 37.29 - 37.35m hosts reddish-brown to greenish sst lenses...at 36.56 - 36.64m buff to yellowish phosphate(?) sections (no reaction with 10% HCl)...

from 37.65 - 42.98m dark green-grey to charcoal grey mst with minor interbedded slt-fg-sst and mg-cg sst...micaceous...has black (organic-rich) sections with elevated radiometrics (up to 104 cps on handheld GR-135)...from 41.95 - 42.40m is greyish-green to black, slt-mg sst with intermixed, organic-rich mud...at 42.05m is an organic fragment (~0.5cm × 2.0cm) rimmed by py...from 42.15 – 42.23m abundant organic detritus...appears to be bedded at ~60° TCA... from 42.83 - 42.90m mg-cg ‘ruddy’ sst...at 42.85m is a pyritized fragment of sst completely surrounded by reddish-brown hematite...

lower contact is sharp and reduced (from 46.94 - 46.98m is organic-rich) and is at ~55° TCA

42.98 67.11 HF Reddish-brown to tan-buff...mg-vcg sst and cgl and minor greyish to reddish-brown mst locally...micaceous...fsp’s are peach in colour...weak kaolinite alt of fsp’s throughout...interval is characterized by the moderate to strong reddish-brown hematite alt throughout...hematite is mottled/pervasive, as hematite disease, mottled-stratified and locally fracture-related (less common)...sst hosts abundant fg diss detritus that is locally stratified...sst and cgl are moderately broken and fractured...locally vuggy (dissolution of carbonate – effervesces with 10% HCl)...

Sm 58 - 84Sm 1 - 40.01 - 0.09

from 42.98 - 44.00m pebble to cobble cgl...from 42.98 - 43.28m cgl hosts abundant fg py accumulations locally…

from 44.00 - 44.65m cg-vcg sst...sst is fractured at 44.06m (35° TCA) and 44.56m (at ~45° TCA)... at 44.65m sst is fractured at ~57° TCA and is strongly hematized...from 44.65 - 45.78m is grey-green to reddish-brown mst that is locally granular with minor interbedded(?), moderately to strongly hematized, cg sst that is broken...from 45.38 - 45.69m is a granule-pebble cgl that is locally ‘ruddy’ and disaggregated...contact with underlying sst is greenish and reduced...

from 48.19 - 48.23m sst is fractured at ~60° TCA, is strongly hematized and is broken and partially disaggregated…

from ~50.12 - 52.10m mg-cg sst...v. micaceous...hosts abundant fg diss organic detritus that is stratified...sst is fractured at 30-65° TCA throughout sub-interval with most at ~45-65° TCA...often bleached along the margins of fracture surface...at 52.07m sst is fractured and strongly hematitized...reddish-brown, pervasive hematitization extends into adjacent sst from 51.87 - 52.10m...

from 52.10 - 53.31m is cgl section (pebble to cobble cgl) that is moderately broken and partially disaggregated…

from 53.31 - 56.20m sst hosts ‘hematitie disease’...’disease’ is most intense from 53.31 - 54.20m and 55.71 - 56.21m... from 55.66 - 55.80m very strong, pervasive hematite disease emanating from fracture at 55.67m (~40° TCA)…

from 58.32 - 59.00m and 59.58 - 60.58m sst is moderately broken and fractured and has a blocky appearance...fracturing is at 40-80° TCA with most at 40-70° TCA... fractures are locally moderately to very strongly hematized... at 59.65m, 60.07 - 60.12m and 60.50m fractures are very strongly hematized and have a corrosive appearance...

from 60.90 - 61.01m sst is fractured sub-parallel TCA...fracture surface is moderately to strongly hematized…

from 64.92 - 65.00m brownish slt-fg sst…

at 65.28m sst is fractured...small greenish to reddish-brown mst rip-up clasts in adjacent sst have a sheared fabric…

from 65.40 - 65.62m sst hosts abundant greenish-grey mst rip-up clasts…

from 66.02 - 66.21m sst is very calcareous...from 66.02 - 66.11m sst is fractured sub-parallel TCA and fracture has CaCO3 vein along fractured surface...from 66.15 - 66.21m sst is fractured at ~35°TCA...has a black organic stain and abundant “sugary” CaCO3 mineralization...from 60.15 - 60.17m sst is v. vuugy and calcareous...appears that sst has been partially replaced...


RB-09-245



Litho UnitMagnetic


67.11 72.36 HF Pale green...clayey mst with minor interbedded slt-fg sst...weak reddish-brown oxidation locally... rare instances of carbonate caliche...mst is somewhat weathered, but is fairly intact…

Ml 63 - 94Ml -1 - 10.09 - 0.11

at 70.64m mst is fractured at ~40° TCA and has minor reddish-brown oxidation along fracture surface…


72.36 80.16 HF Tan-buff to reddish-brown...cg-vcg sst and lesser greenish to reddish-brown clayey-silty mst that is locally granular...sst and mst are micaceous...fsp’s are peach in colour...weak kaolinite alt of fsp’s throughout...sst hosts minor fg diss organic detritus that is often stratified...sst is characterized by a weak to moderate reddish to reddish-brown hematite that is as fg disseminations (<1-20%), mottled/stratified, pervasive/stratified and an instance of fracture-related (hematite vein?) at 78.30m...

Sl 62 - 98Sl -1 - 20.01 - 0.08

from 74.17 - 75.50m greenish clayey mst...strongly reduced with minor weak reddish-brown patchy and wispy oxidation...v. micaceous...from 75.40 – 75.50m grades into a slt-fg sst...from 75.50 – 75.74m mg-cg sst also has a reduced appearance due to greenish mud laminae and fg diss organics...

from 78.30 - 78.60m sst is broken and fractured and has a blocky appearance...fracturing is at 70-90° TCA…

from 78.60 - 79.08m greenish to reddish-brown granular mst...hosts abundant intermixed mg-cg qtz and fsp grains...mst is moderately weathered and broken locally...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

43.87 0.55 392043.32 Sm

44.41 0.54 392143.87 Sm

66.48 0.62 392265.86 Sm

67.11 0.63 392366.48 Sm

67.61 0.50 392467.11 Ml

68.11 0.50 392567.61 Ml

68.61 0.50 392668.11 Ml

69.11 0.50 392768.61 Ml

69.61 0.50 392869.11 Ml

70.11 0.50 392969.61 Ml

70.61 0.50 393070.11 Ml

71.11 0.50 393170.61 Ml

RB-09-245

Hole No: RB-09-246




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

26-Sep-09 -


7.69 14.53 HF Reddish-brown to tan-buff…cg-vcg sst and granule to pebble cgl with lesser interbedded clayey-silty mst…weak to moderate kaolinite alteration of fsp’s…fsp’s are a peachy pink colour locally….sst ranges from weakly to very strongly oxidized and is locally reduced (from 13.78 – 14.53m)…hematitization is reddish-brown to reddish and mottled, mottled-pervasive, pervasive and locally fracture-related (rare)…interval is moderately to strongly broken and fractured and has a blocky appearance…fracturing is dominantly 70 – 80° TCA, although it ranges from 60 – 90° TCA throughout…vuggy…hematitization is most intense towards the top of the ddh and weakens with depth and is reduced towards the base of the interval…

Su 41 - 85Su -1 - 40.02 - 0.04

from 8.23 – 8.33m, 9.10 – 9.54 and 10.05 – 10.21m reddish-brown to greenish clayey mst sections…dominantly reduced with minor remnant, patchy oxidation…

from 12.70 – 12.75m and 13.40 – 13.68m are greenish silty mst sections…micaceous…

from 7.69 – 8.23m sst has a strong reddish-brown to reddish hematite alteration that appears to be both fracture-related and patchy in nature…moderate mottling/bleaching locally…

from 8.33 – 12.00m sst hosts moderate to strong reddish-brown hematite alteration that is both pervasive/stratified and mottled…instances of fracture related hematite occur throughout sub-interval and are locally very strong (8.53m, 8.76m and 10.02m)…

from 12.00 – 13.78m cg – vcg sst is only weakly oxidized (weak, reddish-brown mottled hematite)…from 13.68 – 13.78m sst is broken and partially disaggregated (immediately down-hole from a mst section)…

from 13.78 – 14.53m, mg – cg sst has a reduced appearance…sst hosts minor fg disseminated organic detritus throughout…hosts a weak, greenish alteration(?) that is locally stratified…minor reddish-brown mst laminae…<1% fg disseminated oxidized sulphides (py) throughout…oxidized sulphides are most abundant from 13.94 – 14.00m…greenish alteration is most significant from 14.34 – 14.48m…

lower contact is sharp and core is rounded

14.53 26.56 HF Reddish-brown clayey-silty mst with lesser interbedded slt and fg-vcg sst...dominantly strongly oxidized with minor wispy and patchy greenish reduction locally throughout and local reduced sections…mst is locally nodular (reddish-brown to buff coloured carbonate caliche)…

Mst 54 - 81Mst -1 - 40.03 - 0.11

from 14.53 – 18.72m is reddish-brown clayey-silty mst that is locally nodular (only caliche recovered)….stongly oxidized with minor patchy and wispy reduction locally…sub-interval is highly weathered and broken and locally partially disaggregated…from 14.53 – 14.70m mst is greenish and strongly reduced…from 18.20 – 18.63m slt and fg-mg sst that is strongly oxidized…minor patchy and wispy reduction…from 18.27 – 18.40m sst is fractured sub-parallel TCA…

from 18.72 – 19.38m greenish to reddish-brown cg-vcg sst with significant intermixed greenish mud…sst hosts moderately strong reddish-brown mottled/pervasive hematite locally…in areas where sst is significantly muddy, sst is weakly consolidated…

from 19.38 – 19.63m granular mst …mst is dominantly oxidized with minor greenish reduced patches and wisps throughout…

RB-09-246



Litho UnitMagnetic


14.53 26.56 from 20.53 – 21.10m mst hosts minor reddish-brown carbonate nodules that range in size from 0.5 – 3cm diameter…from 20.75 – 22.35m mst, slt and minor fg muddy sst are more strongly reduced with only minor weak patchy remnant oxidation present…has a greenish appearance…

from 23.11 – 23.17m, 23.20 – 23.25m, 23.50 – 23.62m and 24.87 – 25.23m mst hosts interbedded cg-vcg sst…from 21.93 – 22.35m greenish slt and fg-cg sst…

from 24.87 – 25.05m sst is broken and fractured at 35 – 40° TCA and sub-parallel TCA…reddish-brown to tan-buff cg-vcg sst that hosts abundant reddish-brown mst rip-up clasts…weak to moderate reddish-brown stratified and pervasive hematite alteration…interbedded sst’s at 80 – 90° TCA…

from 25.25 – 25.65m mst is more strongly reduced…from 25.25 – 25.49m greenish stratified reduction overprinting oxidation…from 25.49 – 25.59m mst is completely reduced…at 25.59 – 25.62m is a thin, tan-buff cg-vcg sst section…

from 25.65 – 26.56m reddish-brown strongly oxidized silty mst…massive and featureless…partially broken and weathered…


26.56 28.71 HF Reddish-brown to buff with lesser greenish…cg-vcg sst…massive…minor to moderate kaolinite alteration of fsp’s throughout…fsp’s are a pink to peach colour…hosts minor fg oxidized sulphides, locally up to 1%...sst hosts a weak to moderate reddish-brown mottled/pervasive hematite...sst is locally bleached (buff colour) and reduced (pale green) oxidation is locally mottled…

Sst 62 - 85Sst -1 - 30.03 - 0.09

from 26.56 – 27.01m reddish-brown to greenish, slt and fg-mg sst…strongly oxidized with patchy greenish reduction overprinting oxidation…gradation from overlying mst section…

at 27.13m sst is fractured at 30° TCA…

lower contact is sharp (core is rounded at contact)

28.71 33.43 HF Reddish-brown clayey-silty mst and slt-fg sst with lesser interbedded cg-vcg sst sections…mst and slt are strongly oxidized and reddish-brown in colour with minor reduction throughout as stratifications, wisps and spots…a single, strongly reduced section occurs at the upper contact (from 28.17 – 28.23m) and is greenish in colour…moderately weathered throughout…

Mst 54 - 83Mst -1 - 40.04 - 0.12

from 28.71 – 31.25m dominantly slt-fg sst with lesser mst…strongly oxidized with local stratified, wispy, bedding plane reduction…hosts lesser interbedded tan-buff to reddish-brown cg-vcg sst…sst sections have a weak mottled and mottled/pervasive hematite alteration throughout, host minor reddish-brown mst rip-up clasts and minor to moderate kaolinite altertation of fsp’s…from 30.00 – 30.89m reddish-brown, massive, silty mst with local charcoal grey blotches (reduction related?)…from 30.42 – 30.76m mst is fractured parallel TCA…possible weathering or coring artifact(?) as mst is moderately weathered and partially disaggregated…

from 31.25 – 33.43m reddish-brown clayey-silty mst with local charcoal grey blotches and spots throughout that are locally overprinted by greenish reduction blotches…from 33.00 – 33.07m and 33.15 - 33.17m sst hosts moderate reddish-brown pervasive hematite…mst is at 85° TCA…

from 33.41 – 33.43m is strongly reduced…

lower contact is sharp, reduced and core at contact is rounded (coring artifact)

33.43 42.43 HF Greenish to tan-buff to reddish-brown cg-vcg sst and local granule-pebble cgl sections with minor silty mst sections locally…micaceous…hosts minor fg diss organic detritus that is often stratified throughout…fsp’s are a peachy-orange colour…minor kaolinite alteration of fsp’s throughout…interval has a greenish alteration that often appears to parallel stratified organic detritus…sst hosts a weak, reddish-brown hematite alteration that is both mottled and pervasive/stratified locally throughout…from 33.43 – 36.84m greenish alteration is most prominent…from 36.84 – 42.43m sst is more reduced and hematitization is rare…hosts rare reddish-brown mst rip-up clasts…minor (<1%) fg diss oxidized sulphides locally throughout…interval is badly broken and fractured throughout and core has a blocky appearance…fracturing is at 65 – 80° TCA…

Sst 52 - 80Sst -1 - 20.02 - 0.05

RB-09-246



Litho UnitMagnetic


33.43 42.43 from 36.00 – 36.28m reddish-brown to greenish silty mst that has a granular texture…bedded at ~85° TCA…sub-interval is more oxidized than reduced…reduction mottles oxidation…from 36.25 – 36.28m mst is completely reduced…

core is badly broken from 39.38 – 39.42m, 39.62 – 39.69m, 39.73 – 39.62m, 40.37 – 40.42m, 41.59 – 41.67m (diss mst section) and 41.87 – 42.00m (broken vcg sst and disaggregated mst section)…

from 42.15 – 42.36m sst is strongly reduced with moderate to strong, stratified/pervasive, greenish reduction…stratifications are at ~80-90° TCA…


42.43 54.09 HF Domiantly reddish-brown, strongly oxidized clayey mst with local nodular sections and lesser reddish-brown to greenish slt-fg sst locally…interval is strongly oxidized (reddish-brown colour) with only minor greenish reduction as wisps and spots except from 42.43 – 42.84m (contact between slty mst and overlying sst) is completely reduced…from 52.58 – 54.09m is more reduced than oxidized (greenish reduction mottling clayey-silty mst)…interval is moderately weathered making the distinction between structure and weathering/coring artifacts difficult…

Ml 54 - 88Ml -1 - 40.15 - 0.23

from 44.37 – 44.83m reddish-brown slt-fg sst…completely oxidized…

from 49.59 – 49.99m and 51.54 – 51.74m are nodular-rich sections…

from 52.49 – 54.09 is competent and not weathered…dominantly reduced with minor remnant oxidation locally…dominantly clayey-silty mst and minor slt…at 53.54m fractured at ~35° TCA

54.09 54.80 HF Greenish-grey…mg-cg sst…hosts abundant fg diss organic detritus that is stratified throughout…micaceous…fg diss py throughout that is locally oxidized…stratifications range from ~75-85° TCA…grades into a granule-pebble cgl at base of interval (from 54.75 – 54.80m) with more abundant fg diss py…lower contact is sharp at ~85° TCA…core at contact is rounded

Sl 65 - 73Sl -10.07 - 0.10

54.80 60.53 RB Greenish to black…dominantly silty mst and shl with locally abundant carbonate veinlets…from 54.80 – 57.00m is greenish coloured and dominantly clayey mst whereas from 57.00 – 60.53m is more charcoal-grey to black, slt-shl with lesser interbedded mst…carbonate-rich sections and veins occur sporadically throughout…

RB 48 - 77mst/shl/slt -10.09 - 0.16

from 54.93 – 55.01m greenish, pitted cgl…very calcareous


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

8.29 0.55 29807.74 Su

40.11 0.53 298139.58 HF Sst

40.64 0.53 298240.11 HF Sst

41.45 0.46 298340.99 HF Sst

RB-09-246

Hole No: RB-09-247



Total Depth (m): 24

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

27-Sep-09 -

0.00 6.65 OB Overburden. HF sst and exotic (granodiorite) cobbles and pebbles. OB

6.65 11.81 HF Reddish-brown to tan-buff mg-vcg sst and minor reddish-brown to greenish clayey-silty mst locally...sst is moderately to badly broken and fractured and has a blocky appearance...fracturing measures 75-90° TCA with most between 80-90° TCA...sst is characterized by a weak to strong reddish-brown to reddish hematite alteration that is mottled, pervasive, blotchy and is as fg diss accumulations (~1-5%) from 5.65-~6.20m...sst is moderately vuggy throughout...minor kaolinite alteration of fsp’s and as pore-fill (bright white specs)...

Su-D 54 - 88Su-D -1 - 40.02 - 0.06

from 7.24 - 7.37m and 10.03 - 10.09m sst is badly broken...

from 7.58 - 7.69m strong, pervasive, reddish-brown hematite blotch…

from 7.78 - 8.02m dark grey to reddish-brown to greenish...silty mst section...micaceous qtz granules and pebbles locally throughout...broken and partially disaggregated…

from 8.23 - 8.30m greenish to reddish-brown clayey mst with granules to pebbles of qtz, fsp and lithic fragments throughout...disaggregated…

from 8.59 - 9.16m sst is badly broken and partially disaggregated...locally strongly hematized (reddish-brown pervasive hematite from 8.69 - 8.82m)…

from 11.64 - 11.71m sst is badly broken and partially disaggregated…

from 11.44 - 11.53m greenish clayey mst...broken and disaggregated…

lower contact is sharp at ~85° TCA...sst at contact is strongly hematized

11.81 13.72 HF Dominantly reddish-brown clayey mst...strongly oxidized with a darky grey patchy to wispy overprinting (reduction related?)... minor greenish reduction locally as spots and wisps...from 11.81 - 11.93m greenish and strongly reduced...mst is moderately weathered and partially disaggregated...

Su-Ѳ 59 - 82Su-Ѳ -1 - 40.09 - 0.16

lower contact is reduced and gradational

13.72 15.14 HF Tan-buff to reddish-brown to greenish...mg-cg sst...sst is locally muddy (significant greenish intermixed mud) and hosts greenish mst rip-up clasts locally... sst exhibits bedding plane reduction... characterized by a moderately strong reddish-brown mottled and stratified/pervasive hematite throughout...sst is moderately to badly broken throughout and has a blocky appearance...sst is broken at 75-80° TCA throughout...from 14.49 – 14.83m sst is badly broken...

Su-D' 51 - 74Su-D' -1 - 20.03 - 0.06

from 13.72 - 13.81m sst hosts significant intermixed greenish mst…

from 13.81 - 13.93m sst hosts greenish mst rip-up clasts as it grades into sst…

lower contact is sharp at ~80° TCA and is strongly reduced

15.14 24.00 HF Reddish-brown clayey to silty mst with minor reddish-brown interbedded slt-fg sst and mg-cg sst locally...mst is free of carbonate caliche...mst is dominantly oxidized with only minor greenish reduced sections, spots and wisps...mst is moderately weathered and disaggregated throughout...

Mu-C 61 - 92Mu-C -1 - 40.08 - 0.12

from 15.14 - 15.21m mst is strongly reduced (pale green) has a granular texture (gradation from overlying sst mbr)…

from 17.66 - 17.75m mst is strongly reduced (pale green) and has a granular texture…

RB-09-247



Litho UnitMagnetic


15.14 24.00 from 18.14 - 18.63m tan-buff cg-vcg sst bed with abundant peachy-pink fsp’s...moderate kaolinite alteration as pore-fill...minor fg py accumulations...from 18.17 - 18.33m minor reddish-brown stratified and mottled hematite...mst contacts with sst (18.08 - 18.14m and 18.63 - 18.66m) are greenish and reduced...sst is at ~77° TCA...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

6.59 0.55 39326.04 Su

RB-09-247

Hole No: RB-09-248




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

30-Sep-09 -

0.00 6.03 OB Overburden. HF cobbles and pebbles. OB

6.03 9.73 HF Reddish-brown...clayey-silty mst that locally has a granular texture...dominantly oxidized with rare greenish reduction spots and wisps...mst hosts dark-grey patches throughout (reduction-related?)...strongly weathered and disaggregated...from 6.00 – 9.00m, 1.24m of lost core...

Su-θ 72 - 90Su-θ -1 - 40.08 - 0.11

from 7.09 - 7.14m tan-buff to reddish-brown cg sst that resembles underlying sst mbr...weak reddish-brown mottled hematite…from 7.14 - 7.20m mst is strongly reduced…

lower contact is sharp at ~90° TCA and is strongly reduced…

9.73 10.01 HF Tan-buff to reddish-brown to greenish...slt-fg sst and mg-cg sst...interval is characterized by a weak to moderately strong, reddish-brown mottled and mottled/stratified hematite alteration and well developed bedding plane reduction (often associated with abundance of mst-slt in sst)...both oxidation and reduction are being mottled...slt and sst are moderately broken and fractured(?) throughout and have a blocky appearance...possible fracturing at 70-85° TCA throughout...

Su-D' 68 - 91Su-D' -1 - 20.05 - 0.08

from 9.73 - 9.94m is dominantly slt that is strongly reduced…


10.01 25.37 HF Dominantly reddish-brown clayey-silty mst with local, reddish-brown, interbedded, slt-fg sst and lesser reddish-brown to tan-buff cg sst locally...mst is dominantly oxidized and reddish-brown in colour with only minor greenish reduction as spots, wisps and sections (restricted to contact with cg sst sections)...a dark grey, patchy overprinting is present locally (reduction-related?)...mst/slt is moderately weathered and disaggregated throughout...

Mu-C 65 - 91Mu-C -1 - 40.06 - 0.15

at 14.29 - 14.35m, 15.00 - 15.18m, 15.74 - 16.69m and 23.83 - 24.10m tan-buff to reddish-brown cg sst sections...sst is characterized by a weak to moderate reddish-brown mottled hematite...sst sub-intervals are moderately broken and fractured and sst has a blocky appearance...from 15.04 - 15.08m sst is fractured sub-parallel TCA...from 15.97 - 16.05m and 16.50 - 16.57m sst is badly broken and fractured...from 24.00 - 24.10m hosts abundant reddish-brown mst rip-up clasts...sst sections are at 55-80° TCA...lower contact is sharp at ~82° TCA and is reduced...from 25.28-25.37m mst has a silty - granular texture

25.37 27.48 HF Tan-buff to greenish to reddish-brown...fg-mg sst that grades into cg-vcg sst...hosts abundant peach coloured fsp’s and lithic fragments...sst is characterized by a weak to moderately strong reddish-brown mottled/blotchy hematite alteration and blotchy greenish reduction...sst is moderately fractured and broken throughout giving core a blocky appearance...fracturing measures 70-85° TCA...cg-vcg sst hosts greenish mst rip-up clasts throughout...

Mu-B 68 - 89Mu-B -1 - 20.01 - 0.03

from 25.37 - 26.38m mottled/blotchy oxidation and reduction is strongest…

from 26.38-27.48m sst is only weakly oxidized (weak reddish-brown mottled hematite)...cg-vcg sst does not exhibit green, blotchy reduction…lower contact is sharp and broken and underlying mst is strongly reduced

27.48 31.88 HF Reddish-brown to dark greenish to pale green in colour...clayey to silty mst and slt… Mu-A 67 - 94Mu-A -1 - 40.02 - 0.09

RB-09-248



Litho UnitMagnetic


27.48 31.88 from 27.48 - 30.54m dominantly reddish-brown, strongly oxidized, clayey mst...dark grey patches and wisps overprinting (reduction related?) throughout…from 27.48 - 27.66m strongly reduced greenish mst…

from 27.72 - 27.85m mst is granular (hosts abundant fg-vcg grains of qtz, fsp and lithic fragments) and is a muddy...from 27.80 – 27.85m mst is weakly consolidated...mst grades into a slt at 30.09m and is more competent (less weathered than mst)...reduction (green) spots and wisps increase towards end of sub-interval...reduction becomes more prominent...from 30.54 - 31.88m mst-slt is dark greenish to black colour...dark colour the result of significant organic content...anomalous radiometrics associated with organic-rich mst/slt (up to 94 CPS with handheld GR-135)...organic-rich laminae in both mst and sst...laminae are at 80-90° TCA...from 31.73 - 31.84m greyish, mg sst section with abundant stratified organic detritus...sst bedded at 85° TCA…lower contact is sharp at ~85° TCA

31.88 38.46 HF Tan-buff to greenish to reddish-brown...cg-vcg sst and lesser slt-fg sst and mg sst...sst/slt is moderately to badly broken throughout and core has a blocky appearance for most of interval…

Mu-α 59 - 88Mu-α -1 - 10.04 - 0.14

from 31.88 - 35.05m tan-buff to greenish, cg-vcg sst to granule cgl...hosts abundant peach coloured fsp’s/lithic fragments...sst coarsens with depth...from 31.88 - 33.14m hosts moderate organic detritus (fg diss)...from 31.88 - 32.35m sst hosts a weak reddish-brown mottled Hm and moderately strong greenish reduction that is locally mottled...from 33.14 - 35.05 vcg sst-granule cgl hosts abundant greenish mst rip-up clasts...sst is often weakly consolidated and partially disaggregated in areas that host abundant mst...abundance of mst chips gives sub-interval its greenish colour...from 35.05 - 38.46m greenish to tan-buff to reddish-brown slt-fg sst and mg-vcg sst...from 35.05 - 35.54m mg-cg sst has a weak mottled/blotchy hematite locally...from 35.54 - 36.07m sst is unoxidized to weakly oxidized and hosts minor reddish-brown and greenish mst rip-up clasts...from 36.07 - 36.17m sst hosts a purplish, mottled/pervasive hematite ( mottled/overprinted by greenish reduction spots and patches)...from 36.17 - 36.30m sst is moderately to strongly reduced...from 36.30 - 37.75m greenish slt-fg sst that coarsens to mg-cg sst with depth (becomes mg at ~36.80m)...strongly reduced with only minor weak reddish-brown stratified hematite...stratifications are at ~90° TCA...from 37.75 - 38.46m reduction is weaker and stratified...from 38.41 - 38.46m is a very well cemented, qtz-rich, cg-vcg sst layer (poor visible porosity) with <1% fg diss py and tr cpy(?)...bands of dark grey-black (organic-rich?) locally...lower contact is sharp at ~85° TCA

38.46 43.95 HF Reddish-brown...clayey-silty mst with minor slt-fg sst and mg sst...mst hosts rare carbonate caliche except from 41.78 -42.00m where there are moderate small (≤1cm diameter) buff coloured caliche...mst is strongly oxidized with only minor greenish reduction as spots, patches and sections (restricted to areas in contact with sst)...mst hosts moderate dark grey patches overprinting oxidation (reduction related?)...

Ml 59 - 87Ml -1 - 40.05 - 0.12

from 40.33 - 40.50m tan-buff, fg-mg sst with patchy, mottled, reddish-brown hematite and greenish reduction...from 40.42 - 40.50m sst is fractured at 25° TCA...sst is at ~85° TCA…from 40.50 - 40.67m mst is greenish and reduced …

from 43.71 – 43.95m mst is reduced... from 43.88 - 43.95m mst has a granular texture…


43.95 47.12 HF Greenish to greyish...cg-vcg sst and cgl (granule-pebble-cobble cgl)...sst/cgl has a reduced appearance throughout...hosts (tr-<1%) fg py and oxidized sulphides throughout...weak kaolinite alteration of fsp’s and as pore-fill throughout...from 43.95 - 44.70m weak reddish-brown mottled hematite...from 44.13 - 44.50m sst is moderately reduced with greenish mottled/pervasive reduction...sst and cgl are locally pitted...sst/cgl is non to weakly calcareous...sst and cgl are locally broken and fractured...fracturing is at 70-90° TCA with most at 80-90° TCA...

Sl 62 - 85Sl -1 - 10.07 - 0.09

cgl is highly broken and partially disaggregated from 46.28 - 46.47m, 46.53 - 46.61m, 46.68 - 46.83 and 46.98 - 47.03m…

RB-09-248



Litho UnitMagnetic


43.95 47.12 lower contact is sharp at 85° TCA and base of mbr (from 46.90 - 47.12m) hosts greenish clasts from underlying RB Fm

47.12 77.63 RB Teal green to charcoal grey-black...silty mst, shl and slt...calcareous...local limey brecciated zones (abundant calcite veinlets and RB Fm clasts)...calcite veins locally...veins dominantly at ~90° TCA...charcoal grey-black colour due to significant organic content...local fg pyritic veins (mm scale)...mst, slt and shl are badly broken and partially disaggregated throughout making the distinction between structure and weathering/coning artifacts difficult...fracturing of slt/shl is dominantly ~80-90° TCA however instances of fracturing sub-parallel TCA are not uncommon throughout...

RB 51 - 90mst/slt/shl -10.03 - 0.16

from 47.12 - 48.47m silty mst is pale green in colour and has a vuggy appearance...EOH

1.24m of core is missing from 6.00 - 9.00m; 0.32m of core is missing from 9.00 - 12.00m; 0.35m of core is missing from 12.00 - 15.00m; 0.67m of core is missing from 15.00 - 18.00m; 0.35m of core is missing frm 36.00 - 39.00m; 0.15m of core is missing from 39.00 - 42.00m; 0.20m of core is missing from 42.00 - 45.00; 0.75m of core is missing from 45.00 - 48.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

30.42 0.47 393329.95 Mu

RB-09-248

Hole No: RB-09-249




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

05-Oct-09 -

0.00 7.10 OB Overburden. Exotic (felsic volcanics) cobbles. OB

7.10 7.37 HF Reddish-brown silty mst...oxidized with the exception of 7.32-7.35m where a greenish, reduced band exists...lower contact is sharp and underlying sst is broken

Mu-C 69 - 80Mu-C -1 - 40.07 - 0.08

7.37 12.84 HF Reddish-brown to tan-buff to greenish...cg-vcg sst and lesser slt-fg sst with minor interbedded silty mst...sst is locally muddy and poorly consolidated...sst is characterized by a weak to moderately strong, reddish-brown, blotchy/mottled and mottled/pervasive hematite alteration and patchy to stratified greenish reduction...sst hosts peachy-pink coloured fsp’s...weak to moderate kaolinite alteration of fsp’s (bright white specs)...sst is moderately broken and core has a blocky appearance from 8.08 - 8.79m...reduction, overall, increases with depth...fracturing throughout ranges from 55-90° TCA and sub-parallel TCA with most fracturing measuring 55-75° TCA...

Mu-B 59 - 83Mu-B -1 - 40.04 - 0.16

from 7.37 - 7.60m sst is fractured sub-parallel TCA and core is badly broken…

from 8.28 - 8.36m reddish-brown silty mst with minor greenish, wispy reduction...underlying sst is rounded (coring artifact)…

from 8.79 - 9.56m completely oxidized...reddish-brown slt-fg sst...from 9.32 - 9.56m granular mst (similar to zones that were selectively sampled in 2007 drill campaign...from 9.56 - 9.62m muddy sst is strongly reduced...reduction dissipates with depth in sst over ~10cm into unaltered sst...

from 10.89 - 10.96m muddy sst is both oxidized and reduced...at 10.92m strongly oxidized fracture(?) at ~90° TCA and from 10.90 – 10.94m is oxidized...from 10.89 - 10.90m and 10.94 - 10.96m reduction along margins of oxidation…

from 11.21 - 11.24m sst is fractured parallel TCA...muddy and reduced…

from 11.30 - 11.40m sst is muddy, strongly reduced, badly broken and partially disaggregated…

from 12.80 - 12.84m sst is muddy (significant intermixed greenish mud) and weakly consolidated…

lower contact is sharp (although becomes more muddy at contact) and partially disaggregated

12.84 17.02 HF Reddish-brown clayey-silty mst and slt...strongly oxidized...mst is moderately weathered, broken and partially disaggregated locally, but for most part, mst is fairly intact…

Mu-B 71 - 97Mu-B 40.04 - 0.14

from 15.33 - 15.49m mst is fractured sub-parallel TCA…

from 16.76 - 17.02m dark grey patches (reduction related?) overprint oxidation…

lower contact is gradational into underlying sst

17.02 20.24 HF Tan-buff to greenish to reddish-brown...cg-vcg sst with lesser interbedded clayey silty mst...sst hosts peachy-pink lithic fragments and minor kaolinite alteration of fsp’s...sst is moderately broken throughout and core has a blocky appearance...fracturing is at 75-90° TCA throughout...sst is weakly to moderately reduced giving sst a greenish appearance...a weak to moderately strong, reddish-brown mottled and patchy hematite alteration exists locally throughout but reduction is more prominent...moderate greenish mst rip-up clasts locally...sst is locally pitted (dissolution of mst?)...

Mu-B 60 - 89Mu-B -1 - 30.03 - 0.08

from 17.02 - 17.69m sst is virtually unoxidized and only weakly reduced...<1 - 1% fg diss py and oxidized sulphides throughout…

from 17.69 - 19.14m interbedded tan-buff to reddish-brown cg-vcg sst and reddish-brown to greenish clayey-silty mst that is locally granular…

RB-09-249



Litho UnitMagnetic


17.02 20.24 lower contact is sharp at ~70° TCA

20.24 20.46 HF Reddish-brown clayey-silty mst…dark grey-black patches overprinting oxidation…contact with overlying sst Mbr is strongly reduced from 20.24 – 20.28m…lower contact is sharp at ~85° TCA

Mu-B 77 - 85Mu-B -1 - 40.08 - 0.14

20.46 29.11 HF Greenish to tan-buff cg-vcg sst that locally grades to cgl with minor slt-fg sst...sst is moderately to strongly reduced throughout...exhibits fining upwards sequences (right way up)...sst is moderately broken and fractured throughout and locally has a blocky appearance...fracturing is at 55-90° TCA with most measuring 70 - 80° TCA...sst hosts a weak reddish-brown, mottled and stratified hematite alteration locally throughout...from 22.63 - 22.81m and 24.00 - 24.53m mottled hematite is most predominant (although weak)...from 26.29 - 26.76m hematite is stratified...

Mu-B 64 - 85Mu-B -1 - 10.03 - 0.08

from ~21.00 - 22.11m cg-vcg sst and cgl hosts abundant greenish mst rip-up clasts...sst/cgl is locally weakly consolidated and partially disaggregated as a result of abundance of mst chips...mst is micaceous…

from 24.47 - 24.83m sst hosts a spotty green alteration (chlorite?)...at 24.79m sst is fractured at ~55° TCA and core from 24.79 - 24.83m is broken…

from 24.83 - 29.11m sst is more strongly reduced...sst hosts abundant fg diss organic detritus that is locally stratified...very micaceous...from 24.83 - 25.35m sst is a dark greenish colour and is very strongly reduced...from 24.83 - 25.16m slt-fg sst that grades into a mg-cg sst at ~25.35m...reduction lessens (weakens and is less abundant) with depth but is prominent until ~28.25m...from 28.25 - 29.11m vcg sst resembles sst from 20.46 - 24.79m that hosts abundant peachy coloured fsps and lithic fragments with moderate greenish mst chips but with more fg diss organic detritus...

from 28.96 - 29.03m cgl is broken…

lower contact is sharp at ~88° TCA and from 29.03 - 29.11m cg-vcg sst is very strongly reduced (dark greenish colour)

29.11 30.91 HF Reddish-brown clayey mst...mst is strongly oxidized with only minor weak greenish reduction throughout as greenish spots and wisps...patchy charcoal grey overprinting throughout and is often surrounding greenish reduction…reduction related (?)...mst is only weakly weathered and is fairly intact...

Mu 66 - 83Mu -1 - 40.12 - 0.18

from 30.76 - 30.91m is a pale green colour and is strongly reduced…

lower contact is sharp at ~45° TCA and mst

30.91 34.95 HF Pale to dark green to reddish-brown interbedded silty mst, slt, fg-vcg sst...interval is strongly reduced with local patchy reddish-brown oxidation...from 30.91-33.34m is dominantly reduced and oxidation becomes more prominent from 33.34 - 34.50m where oxidation and reduction are approximately equal...dominantly mst-slt with lesser interbedded dark green, strongly reduced mg-cg sst...rare instances of buff coloured carbonate caliche (4cm diameter)...sst is commonly bedded parallel to sub-parallel TCA (sst for half core and mst for other half)...

Ml 62 - 90Ml -1 - 20.05 - 0.10

from 32.57 - 32.85m is a greenish, cg sst that is locally conglomeratic (granule and pebble sized clasts)...bedded at ~90° TCA…

lower contact is sharp at ~85° TCA and is pitted

34.95 39.72 HF Reddish-brown clayey to silty mst that hosts rare carbonate caliche...caliche are buff coloured and small (<1cm diameter)...mst is strongly oxidized with only minor reduction throughout as greenish wisps and patches...a dark charcoal-grey-black patchy overprinting locally (reduction related?)...mst is weakly to moderately weathered...core is fairly intact....upper and lower contacts are reduced (pale greenish colour)...

Ml 73 - 86Ml -1 - 40.12 - 0.16

from 34.95 - 35.01m mst is strongly reduced (upper contact)…

from 39.20 - 39.72m silty mst has minor interbedded fg-cg sst...sub-interval is strongly reduced and is greenish in colour…

lower contact is gradational (interbeds of slt/fg sst grades into cg sst)…

39.72 40.38 HF Greyish to greenish…cg-vcg sst and cgl (granule-pebble)...sst is pitted...cgl is bleached with abundant kaolinite as pore filling...siliceous...non-calcareous…cgl at base of interval…

Sl 80 - 85Sl -10.05 - 0.06

from 39.72 - 39.98m greenish cg sst that is locally pitted…

RB-09-249



Litho UnitMagnetic


39.72 40.38 from 39.98 - 40.62m is tight, very siliceous cgl...from 40.26 - 40.38m greyish vcg sst…vuggy/pitted...non-calcareous…


40.38 49.52 RB Teal green to dark, charcoal grey/black to grey-green...clayey-silty mst, shl and slt-fg sst calcareous...hosts abundant calcite veinlets…veinlets locally brecciate mst-slt...locally very organic-rich (results in dark-black colour)…

RB 52 - 80mst/shl/slt -10.04 - 0.10

from 40.38 - 43.76m greenish, reduced clayey mst with local minor interbedded slt-fg sst...dominantly greenish and reduced except from 40.51 - 42.51m where mst has minor to moderate reddish-brown patchy oxidation...from 42.41 - 43.76m mst is a teal-green colour...

from 43.76 - 49.52m charcoal-grey-black to green-grey mst-slt-shl with local brecciated horizons (calcite veinlets brecciating RB Fm slt-fg sst)...very calcareous...EOH

0.15m of core is missing from 9.00 - 12.00m; 0.15m of core is missing from 12.00 - 15.00m; 0.85m of core is missing from 15.00 - 18.00m; 0.28m of core is missing from 21.00 - 24.00m; 0.08m of core is missing from 24.00 - 27.00m; 0.24m of core is missing from 27.00 - 30.00m; 0.10m of core is missing from 30.00 - 33.00m; 0.10m of core is missing from 33.00 - 36.00m; 0.08m of core is missing from 36.00 - 39.00m; 0.70m of core is missing from 39.00 - 42.00m; 0.63m of core is missing from 42.00 - 45.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-249

Hole No: RB-09-250




Core Size: BQTK

Date Drilled: 05-Oct-09

License: 007897M




mE / mN



Test Depth (m)



Member

07-Oct-09 -


8.88 10.53 HF Reddish-brown clayey-silty mst...strongly oxidized throughout with only minor greenish reduction as wisps and spots...reduction is more abundant towards base of interval...mst is locally moderately weathered...no carbonate-caliche present…

Mst 83 - 96Mst -1 - 40.04 - 0.11

from 9.96 - 10.05m mst is fractured…

from ~10.20 - 10.53m mst becomes slt-fg sst as it grades into underlying sst Mbr…

lower contact is gradational and reduced

10.53 13.24 HF Reddish-brown to tan-buff to greenish mg-vcg sst...hosts abundant peachy-pink fsps and minor kaolinite alteration of fsps (bright white specs)...sst is characterized by a weak to moderately strong reddish-brown mottled-pervasive and blotchy hematite...sst is somewhat broken and fractured throughout...fracturing measure 60-75° TCA...hosts minor greenish mst rip-up clasts throughout...mud chips are abundant from 10.96 - 11.13m...

Sst 77 - 99Sst -1 - 30.04 - 0.07

from 11.00 - 11.05m is a reddish-brown clayey mst at ~85° TCA…

from 10.53 - 10.61m sst is strongly reduced and is muddy as it grades into sst from overlying mst...pale green in colour…

from 11.20 - 11.34m sst is a reddish-brown colour (strongly oxidized)...from 11.34 - 11.40m sst is strongly reduced and greenish in colour...possible fracture at 11.34m at 90° TCA…

from 13.03 - 13.24m sst is badly broken…


13.24 17.57 HF Reddish-brown clayey-silty mst with lesser slt-fg sst and minor buff coloured mg-cg sst locally...interval is strongly oxidized with pale green reduction locally (contacts with mg-cg sst sections)…

Mst 72 - 95Mst -1 - 40.09 - 0.25

from 14.47 - 14.95m completely oxidized, reddish-brown slt-fg sst...fractured at 14.77m and 14.87m at 45° and 35° TCA respectively…

from 17.06 - 17.36m is moderately to strongly reduced...from 17.24-17.30m is mg sst with blotchy-stratified reddish-brown oxidation...

from 17.56 - 17.57m mst is silty and strongly reduced...


17.57 20.63 HF Reddish-brown to tan-buff cg-vcg sst...hosts abundant peach-pink fsps throughout...minor kaolinite as alteration of fsps and as pore fill (bright white specs)...sst is characterized by a weak to moderately strong reddish-brown mottled and mottled-stratified hematite alteration throughout...sst is moderately fractured...fractures measure 30-65° TCA with most measuring 45-60° TCA...lower contact is sharp at ~40° TCA

Sst 72 - 85Sst -1 - 20.04 - 0.05

20.63 24.90 HF Reddish-brown clayey-silty mst with lesser slt-fg sst...strongly oxidized with only minor greenish reduced spots, patches and sections throughout...mst has a dark charcoal grey patchy overprint locally...mst/slt is moderately weathered and broken and is difficult to determine structure from coning/weathering artifact...

Mst 67 - 81Mst -1 - 40.10 - 0.21

from 20.63 - 20.68m greenish and reduced (contact with overlying sst Mbr)…

RB-09-250



Litho UnitMagnetic


20.63 24.90 from 22.78 - 22.89m buff to greenish mg sst…


24.90 35.43 HF Tan-buff to reddish-brown to greenish...cg-vcg sst with lesser interbedded clayey-silty mst and slt-fg sst...sst hosts abundant peachy-pink fsp’s throughout...interval is characterized by a weak to strong reddish-brown oxidation that is mottled, patchy and mottled/stratified...from 24.90 - 29.26m is dominantly interbedded mst, sst and slt with moderate to strong oxidation and reduction, whereas from 29.26 - 35.47m is more massive sst that is oxidized and is coarser grained...

Mu-B 61 - 85Mu-B -1 - 30.04 - 0.11

from 24.90 - 29.26m reddish-brown to greenish to tan-buff cg sst interbedded with clayey-silty mst and slt-fg sst...mst is locally granular...oxidation is more abundant than reduction...local wispy dark reddish-brown bedding plane oxidation...from 24.90 - 24.99m sst section is broken...from 26.03 - 26.10m sst is fractured at ~30° TCA...from 27.03 -27.33m mst is granular (abundant intermixed mg-cg grains of qtz and fsp) and mst has a patchy dark grey alteration overprinting oxidation...bedding instances measure 55-60° TCA throughout sub-interval...

from 29.26 - 35.48m tan-buff to greenish to reddish-brown cg-vcg sst that locally grades to cgl towards base of interval...characterized by the abundance of peach-coloured fsps, a weak to moderate reddish-brown mottled hematite and moderate greenish reduction throughout...sst is locally pitted (dissolution of CaCO3 as sst effervesces with 10% HCL)...

from 30.02 - 30.34m slt-fg sst hosts wispy bedding plane oxidation and moderate yellowish limonite alteration overprinting throughout sub-interval...from ~34.60 - 35.00m sst becomes vcg to conglomeratic (granule-pebble cgl) and hosts greenish mst rip-up clasts...from 35.00 - 35.30m sst is dominantly cg but contains granules and pebbles throughout as well as abundant greenish mst rip-up clasts...

from 35.30 - 35.43m sst hosts moderate fg diss organic detritus that is stratified...strongly resembles underlying sst Mbr aside from tan-buff colour (underlying sst is green and strongly reduced)…

lower contact is sharp and appears to be erosional at ~40° TCA

35.43 35.89 HF Brownish clayey mst...very micaceous...strongly oxidized...lower contact is gradational into underlying slt-sst mbr

Mst 79 - 83Mst 30.20 - 0.21

35.89 42.07 HF Greenish to greyish to tan-buff to black...fg-cg sst that grades to cgl at base if interval...interval is characterized by the abundance of fg diss organic detritus that is stratified throughout and the overall reduced appearance...micaceous to very micaceous... interval is moderately broken throughout...fractures measure ~40-60° throughout and often parallel stratified organic detritus...

Sst 67 - 91Sst -10.01 - 0.10

from 35.89 - 38.00m fg-mg micaceous sst with abundant stratified organic detritus throughout…

from 38.00 - 38.31m charcoal grey to black to grey-green silty mst-slt...organic rich...micaceous...bedded at 60° TCA…

from 38.31 - 42.07m cg-vcg sst...intensity of reduction (greenish colour and abundance of organic detritus) decreases with depth...from ~40.60 - 42.07m sst is dominantly a tan-buff colour rather than greenish...greenish mst rip-up clasts are more abundant towards base of interval...at 41.64 - 41.68m is a large green mst chip...from 41.84 - 42.07m sst and cgl is fractured, broken and partially disaggregated...

lower contact is sharp and broken and underlying mst is strongly reduced, greenish and is “puggy”

42.07 45.77 HF Reddish-brown clayey-silty mst...strongly oxidized with minor to moderate green-grey reduction as spots, wisps and patches...interval is more strongly oxidized at the top, with reduction spots, wisps and patches becoming more abundant with depth...mst is locally badly weathered and disaggregated...

Mst 59 - 86Mst -1 - 40.08 - 0.12

from 42.07 - 42.12m mst is puggy and strongly reduced and greenish in colour...from 42.12 - 42.18m mst is a dark greyish colour (charcoal grey patches)…

from 42.07 - 43.06m mst is strongly oxidized with only rare reduction patches and wisps…

from 45.49 - 45.59m mst is fractured parallel TCA…

RB-09-250



Litho UnitMagnetic


42.07 45.77 lower contact is sharp and strongly reduced (pale green colour) from 45.73-45.77m...contact is at ~27° TCA

45.77 53.19 HF Greenish to reddish-brown interbedded clayey-silty mst (that is commonly granular) with lesser slt-fg sst and mg-vcg sst...interval is dominantly strongly reduced with lesser patchy and wispy reddish-brown oxidation throughout...sst sections are dominantly strongly reduced and are dark green in colour...mst is also has a dark grey patchy overprinting throughout...mst is commonly granular with intermixed mg-vcg grains of qtz and fsp intermixed...mst is weakly to moderately weathered and broken throughout...possible fracturing of mst throughout (which may be weathering/coring artifacts) measure25-65° TCA and sub-parallel TCA...

Ml 62 - 75Ml -1 - 20.07 - 0.12

from 46.36 - 46.46m sst is fractured parallel TCA and is strongly reduced…

from 51.91 - 53.19m reduction is a pale green...from 52.13 - 52.23m and 52.88 - 53.00m strongly reduced sections…

from 53.05 - 53.19m greenish to reddish-brown slt…


53.19 58.34 HF Dark greenish cg-vcg sst that grades to cgl with minor interbedded mst-slt at the base of interval...strongly reduced (dark green)...hosts moderate to abundant grey-green mst rip-up clasts (RB Fm?) throughout...reduction is both stratified and pervasive...sst/cgl hosts minor fg py (tr-1%) throughout and local oxidized sulphides (tr-<1%)...sst hosts minor to moderate kaolinite alteration of fsps throughout...

Sl 49 - 96Sl -10.05 - 0.12

from 53.19 - 55.77m greenish cg sst with minor interbedded silty mst-slt (from 53.49 - 53.62 and 54.10 - 54.35m)...hosts abundant greenish-grey mst rip-up clasts from 55.50 - 55.77m)...locally pitted (dissolution of mst)…

from 55.77 - 58.34m greenish cgl that hosts abundant greenish-grey mst as rip-up clasts and as mst sections...cgl is moderately to badly broken throughout and is locally disaggregated…

lower contact is sharp at ~30° TCA, strongly reduced and hosts more abundant fg py than rest of cgl

58.34 68.45 RB Teal-green to charcoal-grey-black to grey-green to reddish-brown clayey-silty mst, slt-fg sst and shl...calcareous...local brecciated horizons (calcite veinlets brecciating mst, slt, and shl)…

RB 57 - 93mst/shl/slt -1 - 20.06 - 0.12

from 58.34 - 62.49m dominantly teal green and strongly reduced with lesser reddish-brown oxidation (wisps, spots, patches and sections)...oxidation is weak and minor from ~60.00 – 61.00m and non-existent from ~61.00m onwards...from 61.84 - 62.43m granular mst with interbedded cg sst (each bed ~0.5-1.0 cm thick)...hosts fg diss py (<1-1%) and mst/sst is teal green in colour...

from 62.49 - 68.45m is organic rich, charcoal grey-black to green-grey silty mst, shl and slt-fg sst...local brecciated horizons...calcite veinlets brecciating mst, slt, and shl...moderately broken throughout...EOH

RB-09-250



Litho UnitMagnetic



EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-250

Hole No: RB-09-251



Total Depth (m): 71

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

08-Oct-09 -


5.70 9.29 HF Reddish-brown to tan-buff cg-vcg sst...fsp’s are a peachy-pink colour...minor to moderate kaolinite alteration of fsp’s...sst is characterized by a moderate to very strong reddish-brown to reddish hematite alteration that is mottled/pervasive, mottled/stratified, blotchy and fracture-related...appears to be two generations of hematite (older, dark reddish-brown to brown and a younger red hematite that is as fg diss accumulations (~1-10%)...interval is moderately broken and fractured throughout at 35-65° TCA with most between 40-60° TCA...

Su-D 68 - 90Su-D -1 - 40.02 - 0.05

from 5.70 - 6.66m sst is characterized by a reddish to reddish-brown mottled/pervasive hm alteration...appears that a younger, reddish hematite overprinted older reddish-brown hematite…

at 6.35m sst is fractured at ~35° TCA...at 6.38m an underdeveloped fracture parallels previous fracture…

from 6.66 - 9.29m sst is dominantly as fg diss accumulations (younger, reddish hematite)...at 7.00m sst is fractured, broken and partially disaggregated...fracture surface has strong reddish hematite...at 7.41m an intense, reddish blotchy hematite on fracture surface...fracturing measures ~60° TCA...from 7.43 - 7.49m intense reddish hematite blotch...from 7.66 - 7.72m, 7.76m and 8.28m very strongly hematized fracture (hematite vein?) with complete replacement of host by hematite...sst is fractured at ~45° and 75° TCA...intense, corrosive-style hematite blotch at 8.59 - 8.63m...

from 8.70 - 9.29m sst hosts wispy reddish hematite following bedding planes... from 9.02 - 9.29m hematite is more brownish than reddish...hosts minor fg diss organic detritus that is stratified…

from 9.18-9.29m sst is greenish to black colour and is strongly reduced…


9.29 36.60 HF Dominantly reddish-brown clayey-silty mst that is locally nodular with lesser massive reddish-brown slt-fg sst and reddish-brown to greenish blotchy fg-cg sst...moderate dark greyish wisps and patches overprinting oxidation locally…

Mu-C 63 - 105Mu-C -1 - 40.03 - 0.15

from 9.29 - 20.00m mst is nodular, dominantly reddish-brown and strongly oxidized with lesser greenish reduction spots, wisps and patches...from ~15.44 - 17.67m mst is moderately to strongly reduced...mst throughout sub-interval hosts moderate to abundant tan-buff and reddish-brown carbonate caliche and caliche fragments...in caliche-rich areas mst is usually broken and disaggregated...from 18.98 - 19.14m mst is also strongly reduced...

from ~20.00 - 32.25m reddish-brown clayey-silty mst, slt-fg sst and local greenish to reddish-brown to tan-buff mg-vcg sst sections...sub-interval is free of carbonate caliche, is strongly oxidized with only minor greenish reduction as spots and wisps...when in contact with mg-vcg sst, mst is often greenish and reduced...moderate dark grey patches overprinting oxidation throughout...mst and sst are moderately broken and fractured...fracturing measures ~30-60° TCA and sub-parallel parallel TCA...blotchy sst sections are at 22.52 - 22.71m (fractured sub-parallel TCA and is bedded at ~62° TCA), 23.52 - 23.71m and 24.84-25.03m (fractured at 24.89m at ~35° TCA)...slt-fg sst and mg sst throughout sub-interval locally has wispy and blotchy oxidation and reduction...

from 32.25 - 36.60m reddish-brown clayey-silty mst with moderate dark grey patches and wisps overprinting oxidation (reduction related?) and minor greenish reduction as spots and wisps...locally moderately weathered and broken…

RB-09-251



Litho UnitMagnetic


9.29 36.60 lower contact is sharp and broken

36.60 38.63 HF Tan-buff to blotchy green to reddish-brown...cg-vcg sst and local granule-pebble cgl...sst/cgl hosts abundant peach-coloured fsp’s...minor to moderate kaolinite alteration of fsp’s...tr fg oxidized and sulphides throughout…

Sst 62 - 75Sst -1 - 10.02 - 0.03

from 36.60 - 37.43m sst is characterized by moderate reddish-brown blotchy hematite and greenish blotchy reduction...hosts abundant greenish mst rip-up clasts throughout...from 37.09 – 37.13m greenish mst section...sst is fractured at 37.41m at ~45° TCA along a mst laminae...from 36.60 - 36.70m sst is quite muddy (abundant intermixed greenish mud)...

from 37.43 - 38.63m sst hosts only a weak mottled reddish-brown hematite locally...from 37.81 - 37.89m and 38.00 - 38.04m greenish clayey mst section…

lower contact is sharp and reduced (underlying mst is greenish and reduced)...contact measures ~67° TCA

38.63 39.73 HF Reddish-brown clayey-silty mst...grades into slt at approx 39.62m...mst is strongly oxidized (no reduction visible throughout)...lower contact is gradational

Mu-B 67 - 85Mu-B 40.10 - 0.14

39.73 54.44 HF Dominantly greenish mg-vcg sst with lesser reddish-brown fg-mg massive sst that has greenish wispy bedding plane reduction and minor reddish-brown clayey-silty mst locally...interval is dominantly reduced, but oxidized sections do occur locally…

Sst 53 - 84Sst -1 - 40.02 - 0.11

from 39.73 - 42.36m dominantly reddish-brown slt-fg sst with lesser clayey-silty mst locally...wispy and blotchy bedding plane reduction locally...from 44.41 - 42.36m fg-mg sst is very micaceous and hosts abundant fg diss and wispy organic detritus that is stratified throughout...sst is greenish to greyish in colour (resembles St Mbr)...from 41.98 - 42.36m sst is muddy but stratified organic detritus is visible...

from 42.36 - 47.99 greenish to tan-buff coloured...dominantly cg-vcg sst that grades into cgl at base of sub-interval and lesser mg sst (with abundant fg stratified organics and abundant mica)...moderate kaolinite alteration of fsp’s...locally pitted (dissolution of mst)...hosts greenish mst chips throughout which are abundant at base of interval...from 42.61 - 42.80m and 43.23 - 43.56m mg-cg sst hosts abundant stratified organics...is very micaceous and hosts wispy brownish bedding parallel oxidation (minor)...from 42.80 - 43.23m a weak reddish-brown mottled oxidation... from ~44.45 - 45.85m cg-vcg sst is tan-buff in colour and is virtually unoxidized...from 46.48 - 47.99 greenish vcg sst that grades into a granule-pebble cgl at ~47.45m...characterized by abundance of greenish mst rip-up clasts and its greenish appearance throughout...from 47.08 - 47.99m sst/cgl is highly broken and partially disaggregated...appears to be bedded at ~68° TCA although core in area is badly broken...

from 47.99 - 48.29m greenish to reddish-brown clayey mst with minor interbedded greenish cg sst...at 48.12m sst is fractured at ~47° TCA…

from 48.29 - 54.44m greenish to tan-buff...dominantly cg-vcg sst with lesser fg-mg sst...hosts moderate kaolinite alteration of fsp’s throughout...minor greenish mst rip-up clasts...locally pitted (dissolution of mst)...interval is characterized by a greenish reduction throughout that is pervasive, pervasive/stratified and locally spotty...sub-interval is moderately broken and fractured throughout...fractures measure 40-60° TCA throughout...from 48.36 - 49.36m and 50.27 - 51.30m is a spotty green alteration...from 48.93 - 49.05m sst is fractured at ~20° TCA...from 49.28 - 49.33m is a broken cgl and mst section...from 49.44 - 49.49m sst hosts large mud chip (>3cm diameter) that has an epidote-like green alteration...from 49.52 - 49.58m possible crush zone as sst is completely disaggregated and is somewhat muddy...from 51.36 - 52.87m sst is strongly reduced...from 51.36 - 52.20m greenish fg-mg sst with moderate to strong greenish reduction...pervasive/stratified reduction...from 52.20m onwards is cg-vcg sst with moderate to strong pervasive/stratified and stratified reduction...from 52.87 - 54.44m sst is less strongly reduced but local sections of moderate to strong, pervasive/stratified reduction occurs from 53.00 - 53.35m...from 54.06 - 54.10 sst is broken (cobbles)...

lower contact is sharp and appears to be ~85° TCA (but may be broken)

RB-09-251



Litho UnitMagnetic


54.44 57.28 HF Dominantly reddish-brown clayey mst...strongly oxidized throughout with significant dark (charcoal grey) patches and wisps throughout...minor greenish reduction as wisps and spots...from 54.44 - 55.20m mst is more strongly reduced, is greenish in colour and has significant charcoal-grey patches with minor remnant reddish-brown oxidation...from 54.60 - 54.72m mst has moderate to strong, yellowish, patchy limonite alteration...rare instances of small (<0.5 cm diameter) carbonate nodules locally...

Mst 62 - 81Mst -1 - 40.08 - 0.09

lower contact is sharp at ~50° TCA and mst is reduced from 57.19 - 57.28m and from 57.25 – 57.28m has a granular texture (intermixed qtz and fsp grains)

57.28 58.66 HF Reddish-brown cg-vcg sst...hosts pinkish to pale peach fsp’s throughout...minor kaolinite alteration of fsp’s throughout...interval is characterized by weak to moderate reddish-brown hematite that is mottled and stratified…

Sst 62 - 79Sst 1 - 20.03 - 0.04

from 57.77 - 57.83 sst is fractured at 45° TCA and a pale green mst bed (~1 cm thick) from 57.77 - 57.78m…

lower contact is sharp at ~60° and has patchy greenish reduction for approx last 5cm of interval

58.66 60.78 HF Reddish-brown to greenish clayey-silty mst...interval is dominantly reddish-brown and oxidized but is strongly reduced (pale green) as it grades into underlying sst...mst is only weakly weathered and is fairly intact…

Ml 60 - 81Ml -1 - 40.06 - 0.14

from 58.66 - 60.20m clayey to silty mst is reddish-brown and oxidized with patchy, wispy greenish reduction...charcoal-grey patches also overprint oxidation…

from 60.20 - 60.78m greenish, strongly reduced silty mst grades into a slt-fg (muddy) sst…

lower contact is gradational and reduced

60.78 66.55 HF Greyish to greenish...dominantly cg-vcg sst and cgl with lesser fg-mg sst at beginning of interval (from 60.78 - 62.76m)…

Sl 60 - 82Sl -1 - 10.03 - 0.09

from 60.78 - 62.76m fg-mg sst hosts a weak reddish-brown mottled/pervasive hematite alteration and mottled greenish reduction…

from 62.76 - 66.55m greyish cg-vcg sst and cgl...locally pitted...weak to moderate kaolinite alteration of fsp’s throughout...hosts fg py (tr - ~10% in matrix of basal cgl)...py is locally nodular...sub-interval is moderately to badly broken and core has a blocky appearance for most of sub-interval...cgl is locally highly broken and partially disaggregated...cgl locally has a bleached appearance...from 65.75 - 65.89m sst-granule cgl is badly broken and partially disaggregated..from 65.90 - 66.55m sst hosts teal green mst rip-up clasts (RB Fm) throughout...from 65.90 - 66.20m cgl is dark green...from 66.20 - 66.55m cgl has a bleached appearance...


66.55 71.00 RB Charcoal-grey to teal green to dark greenish-grey...clayey to silty mst, slt and shl...local carbonate caliche, calcite veins/veinlets and local brecciated horizons (CaCO3 veins brecciating RB Fm)…

RB 53 - 83mst/shl/slt -10.05 - 0.11

from 66.55 - 67.13m teal green clayey mst with calcite veinlets at ~75-90° TCA…

from 67.13-67.40m mst is a brownish colour…

from 67.40 - 71.00m charcoal grey shl with local mst and slt...local brecciated horizons...EOH

RB-09-251



Litho UnitMagnetic



HOLE GEOCHEMISTRY


(m)(m) (m)

7.76 0.51 39347.25 Su

8.27 0.51 39357.76 Su

8.78 0.51 39368.27 Su

53.42 0.74 393752.68 HF Sst

RB-09-251

Hole No: RB-09-252




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

10-Oct-09 -

0.00 4.26 OB Overburden. Exotic (granite and granodiorite) pebbles and cobbles. OB

4.26 9.84 HF Greyish to yellowish...cg-vcg sst that locally grades to granule-pebble cgl...abundant cg-vcg fsp’s that are a pale peach colour...moderate kaolinite alteration of fsp’s throughout...pitted...moderate organic trash throughout (fg diss organic detritus that is locally stratified and larger organic fragments)...a yellowish alteration (limonite?) overprints locally throughout but is most strong from 4.26 - 5.93m...interval is moderately to badly broken and fractured throughout...core has a blocky appearance for most of interval...fractures measure 45-80° TCA and sub-parallel TCA...

Su 50 - 81Su -10.01 - 0.04

from 4.39 - 4.56m large, partially rounded organic trash and broken and fractured sst...yellowish alteration (limonite?) overprints organic trash and sst…

from 5.45 - 5.92m sst is fractured sub-parallel TCA and core is moderately broken...moderate yellowish alteration overprinting sst…

at 7.26 sst is fractured at ~40° TCA...organic trash along fracture...yellowish alteration (limonite?) is moderate on surface…

from 9.00 - 9.35m sst is badly broken and is partially disaggregated from 9.00 - 9.13m…

from 9.35 - 9.54m reddish-brown clayey mst...strongly weathered…


9.84 27.34 HF Reddish brown clayey-silty mst (that is locally nodular) and massive slt-fg sst with lesser tan-buff to reddish-brown to greenish mg-cg sst...strongly oxidized with only minor greenish reduction as wisps and sections (when in contact with mg-cg sst)…

Mu-C 61 - 83Mu-C -1 - 40.03 - 0.14

from 9.84 - 15.85m clayey-silty mst is very nodular (abundant reddish-brown to buff coloured carbonate caliche) is badly broken and partially disaggregated throughout...strong reddish-brown carbonate caliche throughout…

from 15.85 - 27.34m dominantly reddish-brown silty mst and slt-fg sst with lesser tan-buff to reddish-brown to greenish mg-cg sst locally...mst-slt-fg sst are strongly oxidized with minor greenish wispy reduction locally and 3-5cm bands in contact with mg-cg sst sections...mst-slt-fg sst has moderate charcoal-grey patches overprinting...moderately strong, wispy to patchy yellowish alteration (limonite?) locally throughout is most visible from 19.40 - 20.00m...

mg-cg sst sections occur at 18.49 - 18.57m, 20.06 - 20.35m, 20.43 - 20.49m and 21.80 - 23.16m (hosts greyish, fg stratified alteration...doesn’t appear to be organic)…

from 22.88 - 22.96m fractured at ~20° TCA…

from 23.09 - 23.16m sst is strongly reduced and is greenish in colour…

from 23.68 - 23.82m broken and fractured sub-parallel TCA…

lower contact is sharp at ~65° TCA...from 27.32 - 27.34m is reduced

27.34 35.12 HF Tan-buff to greenish cg-vcg sst that is locally conglomeratic...hosts abundant peachy-pink fsp’s throughout...weak to moderate kaolinite alteration of fsp’s throughout...hosts minor greenish and reddish-brown mst chips throughout...tr to 1% oxidized sulphides (py?) throughout...weak to strong greenish reduction that is mottled and pervasive...

Sst 63 - 90Sst -1 - 10.03 - 0.08

RB-09-252



Litho UnitMagnetic


27.34 35.12 from 27.34 - 29.79m sst is weakly to strongly reduced and is locally dark green in colour with weak reddish-brown mottled hematite locally...hosts minor reddish-brown mst rip-up clasts throughout…

from 29.79 - 29.86m reddish-brown clayey-silty mst...strongly oxidized...from 29.86 - 29.89m sst is strongly reduced…

from 29.89 - 35.15m sst is less strongly reduced and is locally a tan-buff colour…

at 32.27m sst is 0.5cm greenish mst bed/laminae at ~85° TCA that is strongly reduced and reduction bleeding into adjacent sst from 32.25 - 32.29m...fracture(?)…

from 34.20 - 34.45m sst is fractured sub-parallel TCA and core is broken...a yellowish alteration (limonite? - similar to what was seen further up-hole) along fracture surface that is locally a rusty colour (Fe-carboante?)…

from 34.52 - 35.01m sst is fractured and broken...core has a blocky appearance...fracturing at ~80-90° TCA…

from 35.01 - 35.12m sst is partially disaggregated…

lower contact at ~85° TCA and underlying mst is reduced

35.12 42.12 HF Reddish-brown to greenish clayey-silty mst, slt-fg sst with greenish, mg-cg sst that locally has wispy reddish-brown bedding plane oxidation...sst/mst are locally interbedded...grades to cgl at base of interval…

Sst 59 - 85Sst -1 - 40.09 - 0.11

from 35.12 - 37.86m dominantly reddish-brown slt-fg sst and lesser clayey-silty mst that is strongly oxidized with minor greenish reduction as spots and patches...from 35.12 - 35.23m mst is strongly reduced (contact with overlying sst) and has an anomalous lime-green colour (limonite overprinting?)...

from 37.86 - 42.12m greenish slt-fg sst and mg-cg sst grades to cgl towards base of sub-interval (41.46 - 42.12m)...sst locally hosts reddish-brown wispy bedding plane oxidation and mottled oxidation (less common)...from 39.96 - 40.76m is a reddish-brown clayey-silty mst that is strongly oxidized with charcoal grey-purple patches overprinting...

from 40.73 - 40.76 mst is strongly reduced...mst is at ~60° TCA…

from 41.36 - 42.12m sst/cgl is strongly reduced and is dark green in colour...moderately broken throughout and locally has a blocky appearance…

from 41.77 - 41.84m greenish granular mst section at ~80° TCA…


42.12 48.19 HF Reddish-brown, clayey to silty mst that is nodular throughout most of interval...strongly oxidized throughout with minor to moderate, wispy, greenish reduction...dark purplish to charcoal-grey patches throughout...carbonate caliche is white to buff coloured and are dominantly <1.5cm diameter, but are locally >3cm in diameter)...core is badly broken and locally weathered and partially disaggregated in caliche-rich sections...

Ml 52 - 84Ml -1 - 30.06 - 0.11

from 47.79 - 48.22m mst is strongly reduced…

from 46.32 – 48.19m mst is caliche free…

lower contact is sharp, reduced and broken

48.19 50.03 HF Greenish to greyish cg-vcg sst and cgl...interval is strongly reduced throughout...hosts minor to moderate green-grey and teal green (RB Fm?) mst rip-up clasts throughout...tr - <1% fg oxidized sulphides throughout...non-to weakly calcareous...reduction is both pervasive and pervasive-stratified...stratifications are at ~85-90° TCA...pitted (dissolution of mst)...

Sl 56 - 73Sl -10.05 - 0.11

from 48.36 - 48.48m sst/cgl is moderately broken and core has a blocky appearance…

at 48.44m sst is fractured at ~30° TCA...EOH

RB-09-252



Litho UnitMagnetic



HOLE GEOCHEMISTRY


(m)(m) (m)

8.84 0.71 39388.13 Su

RB-09-252

Hole No: RB-09-253




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

11-Oct-09 -

0.00 6.00 OB Overburden. HF sst cobble and an exotic pebble. OB

6.00 13.85 HF Greenish to tan-buff to reddish-brown, mg-vcg sst with minor reddish-brown to greenish clayey mst sections (minor)...sst is characterized by a greenish reduction that is pervasive, stratified and pervasive/stratified...weak to moderate reddish-brown mottled/pervasive and mottled hematite...sst hosts tr - 1% oxidized sulphides throughout...sst becomes vcg towards base of interval and hosts abundant greenish mst rip-up clasts...sst host abundant peach to pinkish coloured fsp’s...weak to moderate kaolinite alteration of fsp’s throughout...interval overall exhibits a coarsening with depth sequence (normally graded)...sst is moderately broken and fractured throughout with fractures measuring ~60-90° TCA and sub-parallel TCA...

Sst 59 - 90Sst -1 - 10.03 - 0.09

from 6.00 - 10.48m sst is dominantly fg-mg and has is both oxidized and reduced...from 10.48 - 13.85m sst is generally reduced to unoxidized...from 10.48 - 12.27m moderate to strong pervasive reduction…

from 10.96 - 11.19m sst is fractured sub-parallel TCA…

from 11.73 - 12.00m sst is moderately broken and fractured sub-parallel TCA…

from 12.74 - 13.15m sst is fractured sub-parallel TCA...from 12.74 - 12.83m core/sst is badly broken...from 13.03-13.08 is a greenish, clayey mst…

from 13.49 - 13.85m sst is greenish and hosts abundant greenish rip-up clasts…


13.85 32.57 HF Reddish-brown clayey-silty mst and slt-fg sst with lesser blotchy (reddish-brown to buff to greenish) fg-mg sst and local mg-cg sections...interval is dominantly strongly oxidized with minor greenish reduction as spots and wisps and small sections (often in contact with blotchy sst sections)...mst is mostly intact (weakly weathered), but is locally badly weathered and broken...

Mst 56 - 94Mst -1 - 40.03 - 0.12

from 15.75 - 15.87m and 15.96 - 16.03m tan-buff, mg-cg sst with blotchy reddish-brown hematite and greenish mst laminae (minor)...bedded at 85-90° TCA...from 15.70 - 15.75m, 15.94 - 15.96m and 16.04 - 16.09m greenish reduction…

from 22.17 - 24.19m buff to reddish-brown to greenish...blotchy mg-cg sst with local interbedded greenish mst...blotchy reddish-brown oxidation and greenish reduction...from 22.69 - 22.86m sst is fractured sub-parallel TCA...from 23.03 -24.00m cg sst hosts abundant greenish mst rip-up clasts...from 23.38 - 23.64m sst is fractured sub-parallel TCA...from 24.00 - 24.19m sst has a weak reddish-brown hematite and is lacking abundant mst chips...from 24.19 – 24.22m (underlying mst ) is strongly reduced...bedded at ~75-90° TCA...

from 24.30 - 26.83m weak to moderately strong wispy-patchy yellowish alteration (limonite?)…

from 26.83 - 28.21m greyish to green-grey...fg-mg sst...characterized by abundance of fg stratified organics throughout...resembles St Mbr...v. micaceous...stratifications range from ~75-90° TCA...from 28.21 – 28.48m (underlying mst) is strongly reduced...from 28.21 - 28.23 mst has a “puggy” appearance

32.57 39.24 HF Reddish-brown clayey-silty mst that is locally nodular...mst is strongly oxidized with only minor greenish reduction as spots and patches...carbonate caliche is buff to tan in colour and range from mm scale size to >3.5cm diameter...hosts charcoal grey to purplish patches locally...from 36.04 - 37.01m patches are abundant...mst is only weakly weathered and is fairly intact...

Ml 62 - 85Ml -10.02 - 0.11

RB-09-253



Litho UnitMagnetic


32.57 39.24 from 35.90 - 39.24m mst is virtually caliche free…

at 38.66m grades into a slt - fg sst…

from 38.66 - 39.00m dominantly oxidized with patchy greenish reduction…

from 39.00 - 39.42m fg sst is strongly reduced and greenish in colour...


39.24 42.64 HF Greenish to greyish...fg-vcg sst that grades to cgl at base of interval...locally has a bleached appearance...locally pitted...siliceous…

Sl 60 - 85Sl -10.02 - 0.11

from 41.85 - 41.95m pale green silty mst section at ~85° TCA…

from 42.51 - 43.32m cg sst- cgl are badly broken and cgl is partially disaggregated...hosts moderate teal green mst rip-up clasts throughout (RB Fm)...tr - 1% fg py throughout and is fairly abundant (matrix) at contact…

lower contact is sharp at ~80° TCA...cgl is weakly calcareous and has a bleached appearance

42.64 48.12 RB Charcoal grey to dark green-grey to teal green clayey-silty mst, slt and shl… RB 56 - 85mst/slt/shl -10.13 - 0.14

from 42.64 - 45.34m is teal green clayey mst...patchy yellowish alteration (limonite?)...from 45.12 - 45.23m limey horizon is broken...abundant calcite veinlets brecciating mst...1 - 2 % py locally…

from 45.34 - 48.14m dominantly charcoal grey to dark green-grey shl with lesser slt...local limey horizons comprised of calcite veinlets brecciating shl and slt...interval is moderately broken throughput...local sparry calcite veinlets...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

26.83 0.90 393925.93 HF Mst

27.43 0.60 394026.83 Hf Mst

RB-09-253

Hole No: RB-09-254



Total Depth (m): 50

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

13-Oct-09 -

0.00 8.58 OB Overburden. HF sst cobbles and boulders. OB

8.58 22.22 HF Reddish-brown clayey-silty mst, slt-fg sst and lesser blotchy, reddish-brown to tan-buff mg-vcg sst and cgl locally...mst and slt-fg sst is dominantly strongly oxidized with only minor greenish reduction as wisps, spots and local sections (in contact with blotchy sst...mst is weakly to moderately weathered throughout...mst locally has charcoal grey patches overprinting oxidation...local patchy, yellowish alteration (limonite alteration) locally...

Mu 62 - 91Mu -1 - 40.06 - 0.15

from 8.58 - 9.00m tan-buff mg-cg sst with peachy-pink fsp’s...hosts greenish mst laminae (bedding parallel reduction)...minor fg diss organics are locally stratified...bedded at 65° TCA…

from 9.18 - 9.61m more of a reddish-brown mottled oxidation with patchy greenish reduction...from 9.61 - 10.48m cg sst hosts a weak, reddish, mottled hematite alteration...from 9.95 - 9.99m sst is muddy...from 9.96 - 9.97m is a green mst section at ~85° TCA...from 9.97 - 9.99m sst is muddy and weakly consolidated...from 9.32 - 9.65m sst is fractured sub-parallel TCA...from 10.28 - 10.37m sst is badly broken...

from 17.50 - 17.80m cg-vcg sst hosts a weak to moderate reddish-brown oxidation that is mottled and pervasive...local ~1cm thick bands of a beige clay (dickite?)...sst is at ~65 TCA…

from 18.78 - 18.02m tan-buff granule-pebble-cobble cgl...hosts greenish mst rip-up clasts…

from 20.67 - 22.22m slt-fg sst...micaceous...reddish-brown with minor blotchy and patchy reduction from 20.67 - 21.54m...from 21.54 - 22.22m slt-fg sst is a dark greenish colour and appears to have stratified organics throughout but difficult to determine for sure due to dark colour...


22.22 24.52 HF Greenish to tan-buff...cg-vcg sst that is conglomeratic towards base of interval...hosts greenish mst rip-up clasts throughout...rip-up clasts are abundant from 23.64 - 24.52m...interval is characterized by a weak to moderately strong greenish reduction that is pervasive, mottled and locally spotty (from 22.95 - 23.64m)...interval is also characterized by abundance of peachy-pink fsp’s...minor kaolinite alteration of fsp’s...minor fg diss organic detritus...minor mica...interval exhibits a coarsening with depth sequence...

Mu 59 - 88Mu -10.03 - 0.07


24.52 36.56 HF Dominantly reddish-brown clayey-silty mst that is locally nodular with minor interbedded, tan-buff to reddish-brown, cg-vcg sst...mst locally has a granular texture (intermixed mg-cg qtz and fsp grains)...mst is strongly oxidized throughout with minor greenish reduction as patches, wisps and local sections...purplish to charcoal grey patches also overprint locally...weakly to moderately weathered throughout...

Ml 56 - 80Ml -1 - 40.03 - 0.16

from 29.14 - 31.35m mst hosts abundant carbonate caliche...caliche are tan-buff to reddish-brown in colour and range in size from 4cm diameter to ~2-3cm diameter...outside this sub-interval, caliche are minimal…

from 34.50 - 34.76m is a tan-buff to reddish mg-cg sst with moderate peach-pink fsp’s throughout...hosts reddish-brown mottled to blotchy oxidation...sst is at ~60° TCA and underlying mst is greenish and strongly reduced…

lower contact is sharp and mst is strongly reduced from 36.41 - 36.56m

RB-09-254



Litho UnitMagnetic


36.56 42.57 HF Greyish to greenish...cg-vcg sst and cgl...sst/cgl is lacking pink fsp’s and instead, there is moderate to strong kaolinite alteration of fsp’s...sst/cgl hosts minor green-grey to teal green (RB Fm) mst rip-up clasts locally...sst/cgl is locally pitted (dissolution of mst)...moderate greenish reduction locally throughout is both pervasive and pervasive/stratified...hosts tr-1% py locally...py is locally nodular...fg diss sulphides throughout (tr-<1%)...sst/cgl is locally broken and fractured...fracturing measures 55-90° TCA...locally has a bleached appearance...

Sl 53 - 94Sl -10.03 - 0.16

lower contact is sharp and erosional(?) with significant fg py at contact with underlying RB Fm mst

42.57 50.00 RB Charcoal grey to dark green-grey to teal green...dominantly shl with lesser clayey mst and slt...shl-slt is badly broken and partially disaggregated throughout…

RB 53 - 87shl/mst/slt -10.06 - 0.12

from 42.57-43.40m clayey mst (teal green to pale green to brownish)...from 42.57 - 42.74m teal-green, clayey mst-shl...from 42.74 - 42.82m pale green to brownish clayey mst…

from 47.82 - 43.40m teal green to black to brownish clayey mst…

from 43.40 - 50.00m is dominantly charcoal grey to dark green-grey shl-slt...hosts wispy and random calcite veinlets locally...veinlets are locally brecciating slt/shl...shl often has conchoidal and vitreous fractures...interval is organic rich...minor, tiny carbonate nodules (caliche) throughout...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-254

Hole No: RB-09-255



Total Depth (m): 47

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

14-Oct-09 -

0.00 4.98 OB Overburden. Exotic (granodiorite) cobble. OB

4.98 11.13 HF Reddish-brown clayey-silty mst with lesser massive slt-fg sst...strongly oxidized throughout with only minor greenish reduction as rare spots and a single greenish blotch was observed (mg sst lense in mst)…

Mu-C 54 - 92Mu-C 40.06 - 0.13

from 8.77 - 9.00m mst hosts abundant, large (2.0 - 3.5cm diameter) tan-buff to reddish-brown carbonate nodules...completely disaggregated (only caliche recovered)...mostly caliche fragments...

from 11.02 - 11.13m is strongly reduced and pale green in colour…

lower contact is gradational (silty mst- muddy sst into sst)

11.13 22.31 HF Dominantly tan-buff to reddish-brown to greenish, blotchy cg-vcg sst with lesser reddish-brown clayey-silty mst and massive slt-fg sst…

Mu 54 - 96Mu -1 - 40.03 - 0.11

from 11.13 - 12.89m tan buff cg sst hosts blotchy reddish-brown mottled and mottled/pervasive hematite and stratified and blotchy greenish reduction...hosts minor fg organic detritus that is locally stratified...from 11.47 - 11.73m sst is fractured sub-parallel TCA...sst is at ~90° TCA...

from 12.89 - 14.19m reddish-brown, strongly oxidized clayey mst...charcoal grey to purplish patches overprinting throughout...mst is moderately weathered…

from 14.19 - 14.84m reddish-brown, massive slt-fg sst...completely oxidized except for minor greenish spots towards base of sub-interval…

from 14.84 - 16.62m tan-buff cg sst with local weak, reddish brown mottled and bedding plane oxidation...minor greenish reduction throughout is locally spotty...from 15.57 - 15.65m is muddy sst to granular mst that is both oxidized and reduced...sst is at ~77° TCA...

from 16.62 - 18.21m reddish-brown silty to granular mst...strongly oxidized with charcoal grey to purplish patches overprinting throughout...patches are more abundant and larger towards base of sub-interval…

from 18.21 - 22.31m reddish-brown to greenish to tan-buff...mg-cg sst that is characterized by a blotchy to wispy and mottled, reddish-brown oxidation and greenish patchy to bedding parallel reduction...from 20.10 - 20.76m reddish-brown silty mst-slt with greenish and charcoal grey wisps and patches and minor yellowish-green wispy limonite(?)...mst/slt is at ~77° TCA...from 21.31 - 21.41m is a brownish slt at ~85° TCA...from 22.01 - 22.10m sst hosts abundant greenish mst rip-up clasts...

lower contact is sharp and is largely marked by lack of oxidation in underlying sst as sst itself is similar to that which is underlying

22.31 27.95 HF Dominantly tan-buff cg sst and lesser greenish fg-mg sst… Sst 57 - 89Sst -1 - 20.01 - 0.18

from 22.31 - 25.17m tan-buff, cg-vcg sst...characterized by the abundance of cg-vcg fsp grains...unoxidized...weak to moderate kaolinite alteration of fsp’s...locally conglomeratic...hosts minor greenish mst rip-up clasts which are most abundant towards base of sub-interval...locally pitted (dissolution of mst rip-up clasts)...weakly calcareous...local fracturing...fracturing measures ~65-70° and ~90° TCA throughout...from 24.60 - 24.69m sst hosts a weak reddish-brown pervasive hematite...at 24.64m sst is fractured at 90° TCA...from 24.87 - 24.97m possible fault zone(?)...sst/cgl is fractured at ~40° TCA and greenish mst (from 24.87-24.97m) is clayey and has a sheared fabric...fabric is parallel to fracture direction...sst is at ~75° TCA...

RB-09-255



Litho UnitMagnetic


22.31 27.95 from 25.17 - 27.95m greenish to tan-buff, fg-cg sst...from 25.17 - 25.93m greenish to reddish-brown slt...micaceous...grades into a fg sst at ~25.93m...from 25.93 - 26.36m greenish fg-mg sst with weak reddish-brown mottled oxidation locally...well developed bedding plane reduction...from 26.36 - 27.95m sst grades into a mg-cg sst...reduction throughout that is locally stratified...

lower contact is sharp and erosional at ~67° TCA and underlying sst is strongly reduced

27.95 38.21 HF Dominantly reddish-brown clayey-silty mst (that is locally granular) and slt-fg sst with lesser interbedded mg-vcg sst with blotchy reddish-brown oxidation and greenish reduction…

Ml 56 - 91Ml -1 - 40.10 - 0.16

from 27.95 - 28.06m greenish clayey mst...strongly reduced…

from 28.06 - 30.92m reddish-brown clayey-silty mst, slt and granular mst...from 28.06 - 29.33m strongly oxidized, massive, clayey-silty mst and local slt...from 29.72 - 29.80m green-grey mg sst with reduced, greenish mst from 29.67-29.72m and 29.80 - 29.84m...from 29.33 - 30.92m granular mst...hosts abundant fg-cg angular qtz and fsp grains...hosts greenish and charcoal grey patches throughout and minor limonite alteration locally...

from 30.92 - 32.53m interbedded granular mst, muddy sst and sst...greenish to reddish-brown in colour...from 32.53 - 33.09m pale, reddish-brown and wispy to blotchy greenish cg sst...sst is at ~70° TCA…

from 32.53 - 38.21m dominantly reddish-brown clayey-silty mst that is strongly oxidized...hosts local patchy and wispy greenish and charcoal grey reduction...minor limonite alteration locally...from 37.79 - 37.92m reddish-brown mg sst...from 37.92 – 38.21m is strongly reduced slt-fg sst...


38.21 41.79 HF Greyish to greenish...mg-vcg sst that grades into cgl towards base of sub-interval...pitted...has a bleached appearance for most of interval...strong kaolinite alteration of fsp’s throughout...minor fg diss organic detritus throughout...minor weak greenish pervasive and stratified reduction locally...

Sl 54 - 97Sl -10.03 - 0.05

from 40.63 - 41.79m greenish to greyish, cg-vcg sst and cgl...is moderately to badly broken and has minor greenish granular mst-slt sections locally...hosts tr-1% py throughout...py becomes more abundant (1-2%) and is locally nodular towards base of interval...hosts teal green mst chips (RB Fm) at base of interval...

lower contact is sharp and erosional

41.79 47.00 RB Charcoal grey to dark green-grey to teal green...dominantly clayey-silty mst, slt and shl...calcareous...local limey horizons, calcite veinlets and minute carbonate caliche...badly broken throughout…

RB 58 - 84mst/slt/shl -10.07 - 0.14

from 41.79 - 42.33m teal green clayey mst…

from 42.33 - 47.00m charcoal grey-black to dark green-grey in colour...organic-rich...from 42.33 - ~44.45m dominantly clayey-silty mst with lesser shl...from ~44.45 - 47.00m dominantly shl with lesser slt...hosts abundant calcite veinlets and veinlets locally brecciate shl-slt...shl locally has conchoidal fracture and is vitreous (coal fragments?)...EOH

RB-09-255



Litho UnitMagnetic



EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

41.81 0.58 394141.23 Sl

RB-09-255

Hole No: RB-09-256



Total Depth (m): 70

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

19-Oct-09 -

0.00 8.05 OB Overburden. HF sst and exotic (felsic intrusive) cobbles. OB

8.05 13.08 HF Reddish-brown to tan-buff to greenish...mg-cg sst with stratified oxidation and reduction (reddish-brown and greenish)...interbedded clayey-silty mst is dominantly strongly oxidized with lesser greenish reduction as spots and wisps and sections (when in contact with sst)...stratifications are dominantly at ~45-50° TCA throughout (following bedding)...

Su-D' 62 - 81Su-D' -1 - 30.03 - 0.08

lower contact is sharp at ~45° TCA...underlying mst is strongly reduced

13.08 28.13 HF Dominantly reddish-brown clayey-silty mst, massive slt-fg sst and granular mst that is strongly oxidized with minor charcoal grey patches and minor greenish reduction (local spots and sections)…

Mu-C 64 - 91Mu-C -1 - 40.03 - 0.14

from 13.08 - 13.46m clayey-silty mst…

from 13.46 - 16.05m dominantly slt-fg sst and minor mst…

from 16.05 - 17.14m granular mst...from 17.00 - 17.14m is reduced with minor patchy oxidation…

from 17.14 - 19.90m tan-buff to reddish-brown cg-vcg sst with abundant peach-pink fsp’s throughout...hosts minor fg organic detritus throughout that is locally stratified...hosts a weak reddish-brown, mottled and mottled/pervasive hematite alteration locally throughout...from 19.82 - 19.90m sst is weakly reduced and has a pale green reduction overprinting...sst is bedded at ~80° TCA...

from 19.90 - 20.84m clayey-silty mst…

from 20.84 - 23.52m silty mst to slt-fg sst...from 22.04 - 22.14m and 23.26 - 23.47m is greenish slt-fg sst...bleached appearance…

from 23.52 - 28.13m dominantly granular mst with lesser clayey-silty mst...from 27.86 - 28.13m silty mst to muddy sst is strongly reduced…

lower contact is gradational into underlying sst mbr

28.13 34.03 HF Tan-buff to greenish to reddish-brown...dominantly cg-vcg sst that is locally conglomeratic with lesser fg-mg sst near beginning of interval...interval is characterized by a weak, mottled, reddish-brown hematite and a weak greenish reduction that is both blotchy and mottled locally throughout...peach coloured fsp’s...moderate to strong kaolinite alteration of fsp’s...hosts pale green mst rip-up clasts...

Mu-B 54 - 83Mu-B -1 - 10.02 - 0.12

from 28.13 - 29.17m sst is greenish and hosts significant intermixed greenish mud...has patchy reddish-brown oxidation…

from 32.32 - 32.36m greenish silty to granular (some vcg of fsp and qtz) mst at 70° TCA…

from 32.48 - 32.63m is greenish silty mst intermixed with cg sst (broken) - large mst chips(?)…

from 33.56 - 33.67m greenish silty mst with patchy reddish-brown oxidation…

lower contact is sharp and underlying mst is oxidized...sst at contact is rounded (coring artifact)

34.03 35.34 HF Reddish-brown to brownish clayey-silty mst...local charcoal grey to purplish patches overprinting oxidation...minor limonite alteration locally...partially weathered and disaggregated...massive...lower contact is sharp at ~50° TCA

Mu-B 61 - 88Mu-B 40.13 - 0.15

RB-09-256



Litho UnitMagnetic


35.34 40.16 HF Greenish to greyish to tan-buff...mg-cg sst that grades to cgl at base of interval...cgl hosts greenish mst rip-up clasts...interval is characterized by the abundance of stratified fg organic detritus throughout...organic detritus is most abundant from 35.34 - 38.57m...interval hosts a greenish reduction throughout that is stratified and pervasive locally throughout...tr-4% py (fg diss) throughout...sst is micaceous...moderate to strong kaolinite alteration of fsp’s throughout...

Mu-B 75 - 121Mu-B -1 - 00.04 - 0.11

from 35.34 - 35.46m a weak to moderate, reddish brown hematite alteration appears to be bleeding into sst from overlying mst...from 35.34-36.22m is mottled hematite…

from 35.58 - 35.61m reddish-brown clayey mst bed at 50° TCA…

from 37.97 - 38.57m sst hosts abundant fg diss organic detritus (1-2cm thick black stratified bands) and local weak, reddish-brown, mottled/stratified hematite...from 38.36 - 38.48m moderate to strong reddish stratified hematite…

at 39.42 - 40.16m cgl...hosts minor green-grey mst rip-up clasts...tan-buff in colour...from 39.90 - 40.06m sst/cgl is broken and a granular, green-grey mst from 39.94 - 40.00m...cgl is locally pitted (dissolution of mst)…


40.16 53.34 HF Dominantly reddish-brown clayey to silty mst with lesser interbedded granular mst, mg-vcg sst (locally muddy) and cgl…

Ml 58 - 106Ml -1 - 40.05 - 0.15

from 40.16 - 45.10m reddish-brown clayey-silty-granular mst...strongly oxidized with minor greenish wispy reduction locally throughout…

from 45.10 - 46.23m greenish to reddish-brown blotchy granular mst to muddy sst that grades into an true sst/cgl at 45.53m...from 45.90 - 45.97m greenish mst section...broken...from 46.08 - 46.23 sst is badly broken and has a bleached appearance…

from 46.23 - 49.64m reddish-brown to greenish clayey-silty-granular mst with local interbedded mg-cg sst (locally muddy)...both oxidized and reduced and has a blotchy appearance...local charcoal grey patches throughout…

from 49.64 - 50.62m reddish-brown granular mst with minor charcoal grey and greenish wisps and patches…

from 50.62 - 53.34m reddish-brown clayey-silty mst...strongly oxidized with minor reduction as spots, wisps and local stratifications...from 53.29 - 53.34m mst is reduced…

lower contact is sharpe at ~45° TCA

53.34 59.22 HF Greyish to greenish...cg-vcg sst and cgl...sst locally has a bleached appearance...moderate to strong kaolinite alteration of fsp’s throughout...tr-<1% py and oxidized sulphides throughout...py is locally nodular...py is most abundant in basal cgl (2-5%) and is a matrix constitute...moderately fractured and broken throughout...fractures are at ~40-50° TCA throughout...local weak to moderate, greenish, pervasive and stratified reduction...

Sl 62 - 85Sl -10.03 - 0.11

from 53.34 - 53.74m greenish slt-fg sst…

from 57.42 - 58.12m sst and cgl are badly broken and fractured...(0.65m lost from 56.00-59.00m)…

from 59.00 - 59.22m sst is greenish and reduced...hosts abundant py (1-5% locally)...py is most abundant at contact with RB Fm mst…


59.22 70.00 RB Charcoal grey to dark greenish grey to teal green...clayey-silty mst, slt and shl...badly broken and partially disaggregated throughout...calcareous...hosts calcite veinlets and local brecciated horizons...hosts buff coloured carbonate caliche…

RB 54 - 85mst/slt/shl -10.03 - 0.18

from 59.22 - 60.02m teal green to green-grey clayey mst...from 59.72 – 60.02m hosts calcite veins and carbonate nodules…

from 60.02 - 70.00m charcoal grey to black to dark green-grey...shl with lesser slt...calcite vein rich horizons, carbonate caliche and caliche fragments...local brecciated horizons throughout...EOH

RB-09-256



Litho UnitMagnetic


1.87m of core is missing from 8.00 - 11.00m; 0.10m of core is missing from 17.00 - 20.00m; 0.10m of core is missing from 32.00 - 35.00m; 0.65m of core is missing from 56.00 - 59.00

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

36.96 0.62 394236.34 Mu

37.38 0.42 394336.96 Mu

38.50 0.50 394438.00 Mu

RB-09-256

Hole No: RB-09-257



Total Depth (m): 53

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

21-Oct-09 -

0.00 6.00 OB Overburden. HF sst cobbles. OB

6.00 7.86 HF Reddish-brown to tan-buff...cg-vcg sst and granule-pebble cgl...abundant peach coloured fsp’s throughout...weak to moderate kaolinite alteration of fsp’s throughout...hosts minor reddish-brown mst rip-up clasts throughout...pitted (dissolution of mst)...interval is characterized by a weak reddish-brown mottled hematite and a spotty, greyish to brownish, alteration locally throughout (weaker mottled hematite?)...sst is moderately broken and fractured throughout and core has a blocky appearance for most of interval...fractures measure 75-90° TCA throughout...rare instances of an intense, reddish-brown, blotchy to spotty hematite that has a corrosive appearance locally...

Su-D 66 - 82Su-D -1 - 20.02 - 0.05

from 6.57 - 6.65m, 6.87 - 6.91m and 7.12 - 7.17m sst is badly broken…

from 7.26 - 7.34m is a reddish-brown slt-fg sst section…

from 7.72 - 7.81m sst/cgl is greenish and reduced...kaolinite alteration more intense in this sub-interval…

from 7.81 - 7.86m cgl is strongly oxidized (reddish-brown hematite)…


7.86 30.20 HF Dominantly reddish-brown clayey-silty mst and massive slt-fg sst that is strongly oxidized with only minor greenish reduction as spots, wisps and blotches (and sections/bands when in contact with cg sst)...lesser fg-cg blotchy sst...interval is fairly intact (weakly weathered) except for local sections...

Mu-A 62 - 91Mu-A -1 - 40.01 - 0.13

from 7.86 - 11.04m clayey-silty mst that is badly broken and partially disaggregated...from 7.86 - 8.12m mst is an anomalous teal green (similar to RB Fm mst) and reddish-brown to charcoal grey colour...from 9.00 - 9.09m mst hosts sub-angular qtz and fsp clasts (<0.5 - ~2cm diameter)...from 9.09 - 9.89m strongly weathered and disaggregated clayey mst with minor greenish wispy reduction...from 9.89 - 10.01m and 10.71 - 11.04m carbonate caliche rich sections...completely disaggregated and only caliche recovered...caliche are reddish-brown to tan-buff in colour and range from <0.5 -~3.5cm diameter...

from 11.04 - 14.02m reddish-brown slt-fg sst and minor mst...minor patchy and wispy reduction locally...from 13.97 -14.02m clayey mst is strongly reduced (in contact with underlying sst)…

14.02 - 18.26m dominantly patchy/blotchy reddish-brown to tan-buff to greenish fg-cg sst with lesser reddish-brown slt-fg sst and minor silty mst...from 14.02 - 15.15m and 16.77 - 18.62m blotchy sst sections...sst is fractured at ~20-25° TCA at 14.70m and 14.78m (parallel fractures)...from 16.96 - 17.17m sst is muddy (abundant intermixed greenish mud and mst rip-up clasts)...sst is moderately broken and disaggregated...from 17.17 - 18.26m sst is moderately broken and fractured and core has a blocky appearance...locally hosts abundant greenish mst rip-up clasts...

18.26 - 25.73m reddish-brown clayey-silty to granular mst...strongly oxidized with only minor wispy greenish reduction and charcoal-grey patches locally…

from 25.73 - 29.62m reddish-brown slt-fg sst with local bedding plane and blotchy reduction and lesser tan-buff greenish and reddish-brown, blotchy fg-cg sst...blotchy sst from 26.26 - 26.44m and 27.63 - 28.58m...the later sub-interval coarsens to cg sst with abundant greenish mst chips towards base of sub-interval and is weakly consolidated...from 28.58 - 29.03m reddish-brown, very muddy, cg sst to granular mst...from 29.03 - 29.62m silty mst-slt...reddish-brown and massive...(Mu B?)

from 29.62 - 30.20m reddish-brown clayey mst...massive...at ~85° TCA...(Mu (A or B?))

RB-09-257



Litho UnitMagnetic


30.20 33.73 HF Tan-buff to greenish to reddish-brown...mg-cg sst with lesser vcg sst to cgl at base of interval… Sst 69 - 85Sst -1 - 20.03 - 0.15

from 30.20 - 30.33m sst is characterized by the abundance of stratified fg organic detritus...very micaceous...greenish reduction (and lesser reddish-brown oxidation) is also stratified locally throughout...from 30.20 - 30.58m sst is tan-buff to grey, host moderate stratified organics and has a minor stratified oxidation and reduction...from 30.58 - 30.93m same sst as previous sub-interval but has moderate reddish-brown oxidation (pervasive and stratified)...

from 30.93 - 33.33m tan-buff to greenish mg-cg sst...hosts moderate to abundant stratified organic detritus...micaceous...moderate stratified reddish-brown oxidation and greenish reduction...organic detritus is locally abundant...from 31.35 - 31.53m greyish to charcoal grey, fg-mg sst that is organic rich...from 32.29 - 33.38m sst is fractured parallel TCA and is moderately reduced and greenish in colour...from 33.33 - 33.73m tan-buff vcg sst-cgl...abundant peach-pink fsp’s...pitted...core is moderate broken and has a blocky appearance...hosts minor to moderate reddish-brown to greenish mst rip-ups towards base of interval...


33.73 45.57 HF Dominantly reddish-brown clayey-silty granular mst and massive slt-fg sst that is strongly oxidized with minor greenish blotches and bands (contacts with cg sst), bleached patches and purplish to charcoal grey patches...lesser blotchy reddish-brown to greenish mg-cg sst...

Ml 63 - 89Ml -1 - 40.03 - 0.14

from 33.73 - 37.79m reddish-brown clayey-silty mst and massive slt-fg sst...with minor bleached looking patches...rare greenish reduction blotch...moderate purplish to charcoal grey patchy overprinting…

from 37.79 - 39.71m tan-buff to reddish-brown to greenish mg-cg sst…

from 37.79 - 38.08m weak reddish-brown mottled/pervasive oxidation…

from 38.08 - 39.71m greenish to tan-buff...mg-cg sst...local stratified and pervasive greenish reduction...locally hosts moderate-fg diss organic detritus that is often stratified...locally pitted...minor greenish mst rip-up clasts throughout...from 39.61 - 39.71m sst is more strongly reduced (dark green bands of reduction)...

from 39.71 - 45.57m dominantly reddish-brown clayey-silty granular mst with lesser interbedded, dark greenish, cg sst and blotchy reddish-brown, greenish and tan-buff, mg-cg sst...from 40.58 - 40.77m, 40.96 - 41.12m and 42.42 - 42.83m are blotchy sst sections...from 43.63 - 44.50m blotchy mst/sst...from 43.63 - 44.02m blotchy mst...at 44.02m has graded into a mg sst...from 44.02 - 45.57m dominantly sst with local muddy (often greenish) sections...from 45.22 - 45.57m greenish silty mst...


45.57 49.02 HF Greyish to greenish...cg-vcg sst and cgl...minor pink-peach fsp’s throughout...moderate to strong kaolinite alteration of fsp’s...local weak, greenish, pervasive reduction locally...locally has a bleached appearance...minor green-grey mst rip-up clasts throughout...locally pitted (dissolution of mst)...tr to 1% py locally...py is locally nodular but is most often diss...interval is moderately broken and fractured throughout...fracturing measures 65-75° TCA throughout...

Sl 64 - 74Sl -10.06 - 0.11

from 47.26 - 49.02m cgl and sst is moderately to badly broken and is locally completely disaggregated...possible crush zone (48.00 - 48.49m)…

lower contact is sharp at ~80° TCA...greenish in colour...very well cemented but is lacking abundance of py often seen at contact with RB Fm

49.02 53.00 RB Charcoal grey to dark green-grey clayey mst, shl and slt with lesser teal green clayey mst at contact...moderate calcite veinlets...minor buff coloured carbonate caliche...organic rich...badly broken and partially disaggregated throughout…

RB 50 - 86mst/shl/slt -10.06 - 0.14

from 49.02 - 50.29m teal green clayey mst…

from 50.29 - 53.00m charcoal grey-black and dark green-grey...dominantly shl with lesser clayey mst and slt...local calcareous sections (calcite veinlets and minor carbonate caliche)...EOH

RB-09-257



Litho UnitMagnetic


0.90m of core is missing from 6.00 - 9.00m; 0.57m of core is missing from 9.00 - 12.00m; 0.07m of core is missing from 15.00 - 18.00m; 0.15m of core is missing from 30.00 - 33.00m; 0.10m of core is missing from 33.00 - 36.00

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-257

Hole No: RB-09-258




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

22-Oct-09 -

0.00 5.40 OB Overburden. Exotic (granite) cobbles and boulders. OB

5.40 13.24 HF Reddish-brown to tan-buff...cg-vcg sst that locally grades to cgl...hosts abundant peach-pink fsp’s throughout...weak to moderate kaolinite alteration of fsp’s...interval is characterized by a moderate to strong, reddish-brown hematite that is pervasive, blotchy, fracture-related and as fg disseminations locally throughout...from 5.40 - 7.00m sst exhibits only rare instances of hm (small weak spots of reddish-brown)...

Su 63 - 97Su -1 - 40.03 - 0.05

from 5.40 - 7.00m yellowish to tan-buff cg-vcg sst...yellowish colour result of abundant yellow-beige clay alteration throughout (dickite?)...minor kaolinite alteration of fsp’s...minor fg organic detritus that is stratified...from 6.00 - 6.24m sst is fractured sub-parallel TCA and has some granular mud debris in area...sst is moderately fractured and broken...fractures measure 50-65° TCA and yellowish-beige clay development is most abundant along these fracture surfaces...

from 7.00 - 12.46m sst/cgl is moderately to strongly hematized...moderately fractured throughout...fractures measure 30-55° TCA and most hematite alteration appears to originate from these fractures and bleed out into adjacent sst; however pervasive and blotchy hematite is also present locally throughout...strongly hematitized fractures locally have an oily appearance and some also have a corrosive appearance (complete replacement)...sst hosts minor reddish-brown to greenish mst rip-up clasts throughout...from 7.20 - 9.05m a spotty green-grey alteration... from 9.86 - 9.91m large reddish mst chip with greenish wispy reduction...from 9.98 - 10.16m is strongly oxidized cgl with large mud chips...weakly cemented...possible Fe-carbonate alteration (orangish alteration)...from 12.08 - 12.23m sst fractured parallel TCA...

from 12.46 - 13.08m tan-buff cg-vcg sst...unoxidized…

from 13.08 - 13.14m sst is strongly oxidized (corrosive)...from 13.14-13.19m, sst is disaggregated to weakly consolidated and from 13.19 - 13.24m sst/cgl is charcoal grey-black colour (organic-related?)…


13.24 23.29 HF Dominantly reddish-brown clayey-silty mst (that is locally nodular) and minor slt-fg sst...interval is strongly oxidized with only minor greenish reduction locally as wisps and local bands towards base of interval...interval is moderately broken and weathered, especially in caliche-rich sections...local charcoal grey patches locally...

Mu 54 - 95Mu 40.03 - 0.13

from 15.38 - 16.67m caliche-rich section...caliche is buff to tan coloured and ranges in size from <1 - >3.5cm diameter...dominantly only caliche recovered (minimal mst)...caliche is minor throughout rest of interval…

from 21.95 - 22.11m greenish mg sst with green mst laminae...bedded at ~50° TCA…

from 22.11 - 23.29m mst and slt host large greenish blotches locally…


23.29 27.99 HF Reddish-brown to tan-buff...cg-vcg stratified sst...sst is characterized by a weak to moderate reddish-brown mottled/stratified and mottled/pervasive hematite alteration with lesser greenish stratified reduction locally...stratifications are at ~45-55° TCA throughout and are parallel to bedding...sst hosts moderate greenish mst rip-up clasts locally..fracturing also follows bedding...moderate kaolinite alteration of fsp’s both as pore fill and fsp alteration...

Mu-C' 61 - 89Mu-C' -1 - 20.02 - 0.04

RB-09-258



Litho UnitMagnetic


23.29 27.99 from 25.61 - 26.41m sst hosts moderate pervasive hematite with local greenish bands (5-10cm thick) locally…

from 27.71 - 27.99m mg-cg sst is unoxidized with moderate greenish stratified/pervasive reduction throughout…

lower contact is sharp and reduced at ~52° TCA

27.99 37.76 HF Reddish-brown clayey-silty granular mst and slt-fg sst...strongly oxidized throughout with only greenish reduction as wisps and spots...minor charcoal grey patches...rare yellowish limonite alteration patches locally…

Mst 59 - 91Mst 3 - 40.08 - 0.14

from 37.37 - 37.76m reddish-brown with charcoal grey patches and minor bleached, muddy sst interbedded with granular to silty mst...silty mst grades into true sst at ~37.76m…

lower contact is gradational into underlying sst

37.76 40.96 HF Tan-buff to greenish to reddish-brown blotchy mg-vcg sst...interval is characterized by a blotchy and stratified reddish-brown oxidation and greenish reduction locally throughout and minor greenish clayey-silty mst...sst hosts peachy-pink fsp’s and weak to moderate kaolinite as pore-fill and as alteration of fsp’s...

Sst 64 - 78Sst -1 - 20.02 - 0.09

from 37.76 - 38.09m sst hosts minor interbedded clayey-silty mst at 60° TCA...mst sections are ~1-3cm thick...blotchy oxidation and reduction of ssts...blotchy oxidation-reduction continues to approx 39.17m…

from 39.17 - 40.17m sst is neither oxidized nor reduced, except from 39.51 - 39.62m sst is is weakly oxidized (contact with underlying mst)...minor intermixed greenish mud...from 39.62 - 39.81m greenish silty mst...from 40.00 - 40.17m greenish clayey-silty mst with minor broken and partially disaggregated sst...

from 40.17 - 40.96m blotchy mottled/stratified oxidation and stratified reduction throughout...oxidation and reduction are weak…


40.96 42.42 HF Reddish-brown clayey to silty mst that grades to slt-fg sst towards base of interval...micaceous...becoming very micaceous towards base of interval as it grades into underlying sst...strongly oxidized with minor greenish, wispy and blotchy bedding plane reduction locally (rare in mst, but becomes more significant in sst)...stratifications measure ~45-55° TCA throughout...

Mst 79 - 92Mst -1 - 40.10 - 0.14

lower contact is gradational into underlying sst and is marked by increasing amounts of stratified organic detritus that also increases towards base of interval

42.42 48.00 HF Greenish-grey to tan-buff to reddish-brown...mg-vcg sst...sst is locally very micaceous and hosts abundant fg diss and stratified organic detritus...a weak reddish-brown mottled and mottled/pervasive hematite locally...moderate greenish reduction is locally stratified/pervasive and locally pervasive...

Sst 64 - 91Sst -1 - 40.02 - 0.13

from 42.42 - 43.44m gradation from overlying mst/slt section...fg sst grading to mg sst and mst/slt (from 43.01 - 43.08m and 43.29 - 43.44m)...mst /slt is reddish-brown and completely oxidized...msts are at ~40° TCA...from 43.08 - 43.29m sst hosts a weak reddish-brown mottled/pervasive hematite and abundant fg stratified organic detritus (at ~40° TCA)...

from 43.44 - 46.04m sst hosts fg organic stratified detritus that is locally abundant...sst has an overall green-grey appearance (result of abundant organics and weak to moderate, greenish reduction)...a weak, reddish-brown mottled and mottled/pervasive hematite is present locally and overprints reduction...from 43.91 - 44.36m sst hosts abundant stratified organics and is dark green-grey in colour as a result...from 44.23 - 44.35m sst is muddy and hosts reddish-brown mst laminae...mst is at 50° TCA...from 44.88 - 46.04 weak to moderate greenish pervasive/stratified and stratified reduction is prominent...

from 46.06 - 48.00m cg-vcg sst is tan-buff in colour with only a weak greenish stratified reduction locally...sst is characterized by abundance of peach-pink fsps...moderate kaolinite of fsp’s...minor fg organic detritus that is diss...hosts minor greenish mst rip-up clasts throughout...locally pitted (dissolution of mst)...

RB-09-258



Litho UnitMagnetic


42.42 48.00 lower contact is sharp and broken (?) and underlying mst is strongly reduced

48.00 52.68 HF Reddish-brown clayey-silty mst-slt...strongly oxidized throughout with only local blotchy reduction towards base of interval...mst is locally badly broken and disaggregated from 49.96 - 50.78m (coring artifact?)…

Mst 62 - 88Mst -1 - 40.04 - 0.13

from 48.00 - 48.10m greenish and strongly reduced mst (upper contact)…

from 48.93 - 49.16m fg sst section...oxidation is mottled…

from 49.16 - 49.33m mst/slt is fractured parallel TCA…

from 51.70 - 52.68m gradation into underlying sst...granular mst becomes increasingly sandy until ~52.25m where it is a muddy sst...from 52.49 - 52.61m is strongly reduced

52.68 57.03 HF Greenish to greyish to tan-buff cg-vcg sst that locally is conglomeratic...interval is characterized by a weak to moderate greenish reduction that is stratified, pervasive and locally mottled...reduction is strongest towards top of interval and overall tends to decrease with depth...sst hosts minor to moderate fg organic detritus that is locally stratified...moderate to strong kaolinite alteration of fsp’s...locally hosts greenish mst chips...sst is locally pitted (dissolution of mst)...weakly calcareous...tr-<1% oxidized sulphides (py?)...

Sst 57 - 91Sst -1 - 00.01 - 0.07

from 52.68 - 55.20m weak to moderate greenish reduction throughout...from 55.20 - 57.03m only weakly reduced (local greenish stratified reduction)...tan-buff to greyish colour…


57.03 60.63 HF Reddish-brown clayey mst that is strongly oxidized with greenish-grey reduction patches from 57.03 - 59.13m...from 58.66 - 59.00m minor limonite specks and wisps...from 59.00 - 59.13m greenish, strongly reduced granular mst to muddy sst...gradational into underlying sst...

Ml 64 - 86Ml -1 - 40.03 - 0.10

from 59.13 - 60.63m reddish-brown to tan-buff cg sst with weak to moderate reddish-brown mottled and mottled/stratified oxidation...sst is locally fractured at ~55° TCA…

DDH was supposed to continue on until RB Fm, but as drill string became stuck in ddh and core barrel (including core from 61.00 – 63.00m) was lost in the ddh...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

5.90 0.50 39455.40 Su

6.40 0.50 39465.90 Su

6.91 0.51 39476.40 Su

RB-09-258

Hole No: RB-09-259




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

24-Oct-09 -


6.90 15.25 HF Reddish-brown clayey-silty mst and massive slt-fg sst...strongly oxidized throughout with minor greenish reduction as spots and wisps locally throughout...from 7.80 - 11.02m mst is nodular...carbonate caliche is tan-buff to reddish-brown and ranges in size from <1cm->3.5cm diameter...caliche is minimal to rare outside this sub-interval...

Mu 75 - 110Mu -1 - 40.08 - 0.20

from 11.17 - 12.40m is slt-fg sst that is strongly oxidized...interval is locally weathered and disaggregated…from 15.04 - 15.25m (lower contact) is strongly reduced and greenish in colour…

lower contact is sharp with underlying sst at ~50° TCA

15.25 31.47 HF Interbedded clayey-silty to granular mst and slt-fg sst that is dominantly strongly oxidized with lesser mg-vcg sst and local cgl…

Mst 67 - 110Mst -1 - 40.01 - 0.13

from 15.25 - 23.09m dominantly tan-buff cg-vcg sst with local weak reddish-brown mottled and stratified/pervasive hematite with lesser intense, dark grey to reddish-brown hematitic bands and blotches (have an oily sheen-manganese stain?)...minor stratified and diss organic detritus...from 15.25 - 15.58m mg-cg sst is interbedded with greenish silty mst beds (15.32 - 15.40m and 15.51 - 15.58m)...beds are at ~45° TCA and are strongly reduced...sst hosts a weak reddish-brown mottled/blotchy hematite...from 17.30 - 18.36m reddish-brown, strongly oxidized clayey mst...from 18.36 - 18.74m reddish-brown to greenish slt-fg sst...from 18.74 - 19.08m reddish-brown clayey-silty mst...from 19.05 - 19.08m is somewhat ‘puggy’...from 19.07 - 19.08m is greenish and reduced...from 21.77 - 22.10m sst is fractured numerous times sub-parallel TCA to ~20° TCA...contact with underlying mst appears to be erosional and at ~50° TCA...from 23.09 - 26.13m reddish-brown to greenish...clayey-silty granular mst with local blotchy to stratified greenish reduction and charcoal grey patches...from 23.80 - 24.17m greenish to tan-buff to reddish-brown granular mst to muddy sst...blotchy greenish reduction...hosts abundant peach-pink fsps...sub-interval is fractured sub-parallel TCA...becomes increasingly sandy (granular mst to muddy sst) towards base of sub-interval as it grades into underlying sst...from 26.07 - 26.13m is greenish and reduced...from 26.13 - 28.04m tan-buff cg-vcg sst with minor chlorite...hosts minor weak reddish-brown mottled oxidation locally...minor fg organic detritus throughout that is both diss and stratified...moderate kaolinite alteration of fsp’s throughout...sst hosts significant greenish mst chips at base of interval...sst is at ~50° TCA...rare instances of bedding are at ~55-60° TCA...tr to <1% fg oxidized sulphides throughout (py?)... from 28.04 - 31.47m reddish-brown silty mst, slt-fg sst...strongly oxidized with only minor reduction locally as wisps and blotches that are bedding-parallel...contact with underlying sst is reduced from 31.45 - 31.47m and contact is at ~65° TCA

31.47 34.66 HF Tan-buff to greenish mg-vcg sst and cgl...sst hosts abundant peach-pink fsp’s...weak to moderate kaolinite alteration of fsp’s throughout...characterized by a weak to moderate greenish reduction that is locally spotty and, less commonly, stratified to pervasive...hosts minor fg organic detritus that is diss and stratified...a weak to moderate reddish-brown blotchy/stratified oxidation locally that appears to be fracture/bedding parallel (32.11m, 32.50m and 32.97m) and often is with a reddish-brown to greenish silty mst-slt at ~45° TCA...

Sst 72 - 86Sst -1 - 20.01 - 0.04

RB-09-259



Litho UnitMagnetic


31.47 34.66 from ~32.25-32.44m and 33.03-33.50m a spotty green alteration…

from 34.15 - 34.25m greenish clayey mst at ~60° TCA with weak remnant mottled oxidation…

from 34.25 - 34.55m sst/cgl hosts abundant greenish mst chips…

from 34.55 - 34.67m (lower contact) reddish-brown clayey mst at ~60° TCA

34.66 38.00 HF Dominantly greyish, reduced mg sst that is characterized by abundance of fg organic detritus that is stratified throughout, the abundant mica (white) and the overall reduced appearance...moderate kaolinite alteration of fsp’s throughout...tr-<1% oxidized sulphides...stratifications are at ~30-50° TCA...

Sst 78 - 94Sst -10.01 - 0.04

from 37.00 - 37.65m a pale, weak, reddish-brown pervasive oxidation overprinting…

at ~37.70m grades into vcg sst-granule cgl that has a reduced appearance�

38.00 41.74 HF Tan-buff to reddish, cg-vcg sst and cgl that locally has a weak to moderate reddish-brown hematite that is as fg disseminations (~1-5%)…

Sst 78 - 92Sst -1 - 20.01 - 0.04

from 38.56 - 38.66m sst hosts interbedded greenish and reddish-brown silty mst…

from 40.77 - 41.10m polymictic granule-pebble cgl that is unoxidized…

from 41.52 - 41.74m sst is moderately broken and fractured...fractures measure 35-45° TCA…

lower contact is sharp and appears to be erosional at ~30° TCA

41.74 52.50 HF Dominantly reddish-brown, strongly oxidized, clayey-silty granular mst with minor slt-fg sst towards base of interval...minor to abundant green-grey to charcoal grey patches and spots throughout...minor to rare carbonate caliche throughout (buff to reddish-brown in colour and small, ~<0.5 – 1.0cm diameter)...

Ml 64 - 94Ml -1 - 40.08 - 0.15

from ~42.40 - 43.20m mst is almost completely a greyish colour resulting from abundant patches throughout…from 44.91 - 45.30m very granular mst to muddy sst...moderate to strongly reduced…

lower contact is sharp and reduced

52.50 57.70 HF Greyish to greenish cg-vcg sst and cgl and minor greenish slt-fg sst...sst has an overall bleached and reduced appearance...moderate to strong kaolinite alteration of fsp’s...minor fg diss organic detritus...greenish reduction/alteration is locally pervasive, stratified and spotty in nature...a weak reddish-brown mottled oxidation is present locally...reduction/alteration exists from 52.50 - 54.34m...from 54.34m onwards, sst/cgl is neither oxidized nor reduced but does have a bleached appearance locally...

Sl 57 - 83Sl -10.01 - 0.07

from 57.01 - 57.70m sst has a weak greenish alteration...siliceous...pitted...hosts minor teal green mst rip-up clasts throughout (RB Fm)...hosts ~1% fg py at contact with RB Fm (last ~10cm of interval)…lower contact is sharp at ~60° TCA

57.70 61.93 RB Teal green to charcoal grey to green-grey...dominantly clayey mst with lesser shl towards base of interval…

RB 65 - 77mst/shl -10.04 - 0.11

from 57.70 - 59.23m teal green clayey mst...minor patchy limonite alteration locally...minor calcite veining…from 59.23 - 60.03m charcoal grey to dark green grey...organic rich clayey mst…

from 60.03 - 60.25m green grey clayey mst with minor, small (<0.5 – 1.0cm diameter), buff coloured carbonate caliche…from 61.25 - 61.93m green-grey shl...calcareous...abundant calcite veinlets...EOH

RB-09-259



Litho UnitMagnetic


1.50m of core is missing from 8.00 - 11.00m; 0.45m of core is missing from 11.00 - 14.00m; 0.35m of core is missing from 17.00 - 20.00m; 0.10m of core is missing from 20.00 - 23.00m; 0.15m of core is missing from 26.00 - 29.00m; 0.05m of core is missing from 29.00 - 32.00m; 0.35m of core is missing from 41.00 - 44.00m; 0.05m of core is missing from 44.00 - 47.00m; 0.20m of core is missing from 47.00 - 50.00m; 0.20m of core is missing from 56.00 - 59.00m

EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

33.82 0.61 394933.21 HF Sst

40.92 0.49 395040.43 HF Sst

RB-09-259

Hole No: RB-09-260



Total Depth (m): 41

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

25-Oct-09 -


7.82 9.28 HF Reddish to reddish-brown cg sst…weak to moderate kaolinite alteration of fsp’s…sst is characterized by a weak to moderate reddish hematite that is pervasive and stratified throughout…sst is locally fractured….fractures measure ~85-90° TCA…at 8.64m and 8.68m sst is fractured at 40-45° TCA…

Su 67 - 90Su 0 - 30.01 - 0.04

from 8.16 – 8.28m sst has a bleached to unoxidized appearance…

lower contact is sharp at ~90° TCA and underlying mst is partially reduced

9.28 14.57 HF Brick red…clayey-silty mst, slt-fg sst…very strongly oxidized with only minor greenish reduction as spots, wisps and local patches…mst hosts a purplish patchy alteration locally throughout (reduction related?)…mst is moderately broken and fractured throughout (coring artifact?)…

Mu 68 - 94Mu 40.06 - 0.14


from ~13.80 – 14.16m granular mst with bedding-parallel, blotchy reduction locally…


14.57 26.95 HF Reddish-brown to reddish to tan-buff…mg-vcg sst that locally grades to cgl…hosts abundant peach-pink fsp’s throughout…moderate kaolinite alteration of fsp’s…minor to locally abundant reddish-brown and greenish mst chips…sst is locally vuggy (dissolution of mst)…sst/cgl is characterized by a weak to strong reddish-brown hematite alteration that is pervasive/stratified, mottled, mottled/pervasive and locally as fg diss accumulations…minor greenish reduction locally as bedding-parallel stratified bands and blotches…

Sst 53 - 84Sst -1 - 40.01 - 0.06

from 14.57 – 15.90m mg-cg sst…weak to moderate reddish hematite that is mottled and as fg disseminations (~5-30%)…bedding-parallel stratified bands to blotches…

from 15.90 – 19.21m hematite is dominantly as fg disseminations and stratifications…locally hosts abundant reddish-brown mst chips that are also stratified…from 17.35 – 17.42m greenish to reddish-brown silty mst – slt at ~85° TCA…from 17.55 – 17.85m brick red slt-fg sst (massive) and strongly oxidized…

from 19.21 – 26.95m hematite alteration is mottled/pervasive, pervasive/stratified and mottled…from 21.02 – 21.81m mg, very micaceous sst hosts abundant stratified fg organic detritus…moderately to strongly hematitized (pervasive/stratified) with local bedding parallel reduction bands…sub-interval resembles St Mbr except for hematite alteration…stratifications are at ~75-85° TCA…from~22.10 – 26.95m weak t moderate, mottled hematite…from ~22.10 onwards, hematite alteration overall decreases with depth…from 24.69 – 26.95m sst is practically unoxidized with only minor local weak mottled hematite…

lower contact is sharp at ~90° TCA and is strongly oxidized

26.95 35.55 HF Dominantly reddish-brown clayey-silty to granular mst and slt-fg sst with lesser mg-vcg sst…mst/slt is dominantly strongly oxidized throughout…minor greenish reduction as spots and wisps…a more prominent charcoal grey patchy reduction throughout is locally abundant…

Ml 62 - 90Ml -1 - 40.06 - 0.13

from 27.00 – 27.04m clayey mst is oxidized…from 27.04 – 27.13m strongly reduced clayey mst…from 27.13 – 28.65m reddish-brown silty to granular mst and slt-fg sst…strongly oxidized with minor greenish and charcoal grey wisps and patches…from 28.43 – 28.65m fg sst is fractured sub-parallel TCA…

RB-09-260



Litho UnitMagnetic


26.95 35.55 from 28.65 – 30.00m greenish to greyish mg-vcg sst that locally hosts abundant greenish mst chips and locally has intermixed greenish mud…from 29.36 – 29.47m sst is fractured sub-parallel TCA…from 28.87 – 28.92m sst is fractured at ~20° TCA…

from 30.00 – 35.55m reddish-brown to charcoal grey…silty to granular mst…from 33.00 – 33.24m slty mst fractured sub-parallel TCA…from 35.04 – 35.55m mst has graded into a greenish slt-fg sst…

lower contact is sharp and core is rounded (coring aftifact)

35.55 36.34 HF Greyish to greenish…cgl with lesser cg-vcg sst…very siliceous…has a bleached appearance locally…tr-<1% fg diss py…locally hosts minor green-grey mst rip-up clasts…at 35.73m and 35.76m cgl is fractured at ~20° TCA and from 35.76 – 35.83m cgl is badly broken and partially disaggregated…minor greenish stratified reduction locally…locally pitted…sst is weakly calcareous…

Sl 67 - 87Sl -10.04 - 0.07


36.34 41.00 RB Charcoal grey to teal green to dark green-grey…clayey mst, slt and shl…calcareous…locally hosts white-buff calcite veins and veinlets and lesser carbonate caliche…

RB 67 - 84mst/slt/shl -10.03 - 0.10

from 36.34 – 37.48m dominantly clayey mst…from 36.34 – 36.61m dominantly teal green clayey mst…local charcoal grey laminations…from 36.61 – 37.23m charcoal grey clayey mst…from 37.23 – 37.48m teal green clayey mst…

from 37.48 – 38.10m greenish cgl…somewhat resembles cgl in Sl Mbr except greener and more colourful clasts…from 37.78 – 37.86m brownish ‘puggy’ mst…

from 38.10 – 38.94m teal green clayey mst with charcoal grey-black patches…local yellowish limonite alteration…from ~38.90 – 38.94m tan-buff carbonate caliche…

from 38.94 – 41.00m charcoal grey to green-grey shl and slt…very calcareous…hosts moderate white-buff calcite veins and veinlets…veins are dominantly at ~75-90° TCA…locally has a conchoidal fracture and a vitreous surface…organic-rich..EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-260

Hole No: RB-09-261



Total Depth (m): 51

Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

26-Oct-09 -


6.57 14.18 HF Reddish to reddish-brown to tan-buff…mg-vcg sst...moderate to strong kaolinite alteration of fsp’s...abundant pale peach to pink fsp’s...sst is characterized by a weak to strong reddish to reddish-brown hematite alteration that is as fg diss accumulations, mottled/pervasive, stratified/pervasive and fracture related...core is moderately fractured and broken throughout and locally has a blocky appearance...fracturing measures ~65-90° TCA with most measuring 80-90° TCA...

Su-D 52 - 88Su-D 0 - 40.01 - 0.10

from 7.20 - 7.26m sst fractured sub-parallel TCA…

from 7.67 - 9.00m sst is moderately fractured and broken and core has a blocky appearance...from 8.49 - 8.70m fractured sst that is very strongly oxidized, locally has complete replacement of sst by hematite...from 8.87 - 9.00m sst rubble partially rounded...

from 9.00 - 9.38m silty mst-slt...reddish-brown...strongly oxidized...mst/slt is at ~77° TCA…

from 9.92 - 10.44m reddish-brown slt-fg sst...moderate-strong reddish-brown mottled/pervasive and stratified oxidation…

at 10.71m and 10.94m strongly oxidized fracture…

from ~9.85 - 14.18m sst is dominantly weakly oxidized (weak mottling and fg diss reddish hematite)...minor strongly hematitized fractures (10.71m, 10.94m and 13.00m) and rare blotches...from ~13.10 - 14.18m very weak mottled oxidation…

from 14.15 - 14.18 strongly oxidized

lower contact is sharp at ~70° TCA...minor fg py at contact

14.18 28.67 HF Reddish-brown clayey-silty mst and slt-fg sst that is strongly oxidized with only minor reduction locally (bedding parallel bands/blotches)...lesser reddish-brown to tan-buff to greenish fg-cg sst...interval is fairly intact but badly broken sections do exist locally...

Mu 52 - 93Mu -1 - 40.03 - 0.13

from 14.18 - 16.07m reddish, strongly oxidized silty mst-slt with purplish patches locally...minor greenish reduction from 14.56 - 14.80m with reddish-brown, broken, mg-cg sst (broken sst - interbedded?)...sub-interval is broken, weathered and partially disaggregated...

from 16.07 - 18.00m gradational sequence from fg sst to cg-vcg sst towards base of sub-interval...from 16.07 - 16.85m strongly oxidized, reddish-brown slt-fg sst...from 16.85 - 18.00m fg-vcg sst hosts a moderate reddish-brown pervasive/stratified and mottled/pervasive hematite alteration...minor greenish stratified to blotchy bedding parallel reduction from 16.85 - 17.15m...sequence becomes vcg at ~17.50m...

from 18.00 - 28.67m clayey-silty mst, slt-fg sst (massive and strongly oxidized) with lesser mg-vcg sst locally (which commonly has a mottled to stratified oxidation with bedding parallel reduction bands)...from 18.94 - 19.51m granular slt to muddy sst is completely oxidized...from 21.83 - 22.10m greenish mg sst…local bedding parallel reduction bands and a weak, mottled, reddish-brown hematite...mst in contact with sst is also reduced...sst is at ~85° TCA...

from 24.93 - 25.62m reddish-brown to greenish, blotchy slt-fg sst with minor interbedded mg-cg sst...from 25.62 - 25.98m cg sst with abundant reddish-brown mst rip-up clasts...from 25.98 - 26.52m reddish-brown to tan-buff cg sst with reddish-brown to greenish mst chips locally...sst is at ~75° TCA and has a weak mottled reddish-brown hematite...

RB-09-261



Litho UnitMagnetic


14.18 28.67 lower contact is gradational into underlying sst

28.67 37.30 HF Tan-buff to greenish to reddish-brown…cg-vcg sst and granule/pebble cgl...abundant peach-pink fsp’s...weak to moderate kaolinite alteration of fsp’s throughout...locally hosts a spott, greenish alteration…

Sst 61 - 93Sst -1 - 40.01 - 0.11

from 28.67 - 32.62m reddish-brown to greenish to tan-buff…fg-vcg sst that locally has blotchy oxidation-reduction that is often bedding-parallel…locally grades to granule-pebble cgl and hosts abundant greenish mst chips in these areas...hosts minor to moderate fg stratified organic detritus...from 32.41 - 32.45m cgl is badly broken and disaggregated...from 32.51 - 32.62m reddish-brown, micaceous slt...

from 32.62 - 35.00m tan-buff cg-vcg sst and granule-pebble cgl…weakly oxidized to unoxidized...from ~33.00 - 33.85m hosts a weak mottled oxidation locally and a green-grey, spotty alteration locally...from 34.16 - 34.20m reddish-brown slt-fg sst at ~85° TCA...from 34.20 - 35.00m is tan-buff cg-vcg sst-cgl that is characterized by an abundance of peach-pink fsp’s...local minor green mst chips…sst/cgl is bedded at ~80° TCA...

from 35.00 - 35.35m reddish-brown silty mst-slt...from 35.35 - 37.30m fg-cg sst with local cgl fragments...hosts minor fg stratified organic detritus...moderate kaolinite alteration of fsp’s...locally hosts blotchy to stratified reddish-brown oxidization and green-grey mst chips...

lower contact is sharp at ~87° TCA and underlying mst is reduced

37.30 45.09 HF Reddish-brown clayey-silty mst that is locally granular with lesser mg-cg sst that is locally interbedded...interval is both oxidized and reduced...oxidation is prominent for upper half of interval whereas reduction is dominant for lower half of interval...

Ml 54 - 96Ml -1 - 40.05 - 0.24

from 37.30 - 39.03m clayey-silty mst, slt-fg sst…from 38.14-39.03m strongly oxidized with minor greyish wisps and patches…

from 39.03 - 39.51m mst-slt hosts buff coloured caliche...from 39.03 - 39.27m is strongly reduced…

from 39.51 - 39.91m greenish to reddish-brown interbedded slt-fg sst and mg-cg sst...bedding-parallel oxidation and reduction...bedding appears to be at ~80-90° TCA... sst is at ~70° TCA...minor limonite locally...minor buff coloured carbonate caliche…

from 39.91 - 45.09m reddish-brown to greenish to greyish…clayey-silty to granular mst…local greenish reduced sections, spots and wisps and greyish patches throughout...lesser blotchy, greenish to reddish-brown fg sst...from 44.91 - 45.09m strongly reduced, greenish slt

45.09 48.31 HF Greenish to tan-buff…cg-vcg sst and cgl...hosts peach-pink fsp’s...moderate kaolinite alteration of fsp’s throughout…locally hosts a greenish reduction that is pervasive, stratified, mottled and locally spotty...locally pitted…weakly calcareous…tr-<1% oxidized sulphides...tr py…py is more abundant at lower contact...

Sl 61 - 91Sl -1 - 00.01 - 0.09

from 45.57 - 45.70m, 45.87 - 46.17m and 47.26 - 48.00m spotty green alteration…

lower contact is sharp at ~90° TCA and has abundant (~10%) nodular py in sst at contact surface

48.31 51.00 RB Charcoal grey to teal green to olive green…clayey-silty mst and shl… RB 52 - 77mst/shl -10.07 - 0.15

from 48.31 - 49.09m teal green clayey mst

from 49.09 - 49.37m olive green silty mst with carbonate nodules and calcite veinlets...buff to white calcareous sections…

from 49.37 - 51.00m charcoal grey…dominantly shl...calcite veins and veinlets and lesser carbonate caliche...moderately broken...EOH

RB-09-261



Litho UnitMagnetic



EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

7.10 0.53 39486.57 Su

RB-09-261

Hole No: RB-09-262




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

28-Oct-09 -

0.00 8.42 OB Overburden. HF sst and exotic cobbles, pebbles and 'puggy' material OB

8.42 20.33 RB Charcoal grey to green-grey…slt and shl...interval is badly broken and is dominantly rubble...very difficult to determine structure from coring artifact...ddh was difficult to drill...broken and disaggregated nature of core makes it difficult to get accurate measurements of features...

RB 48 - 90slt/shl -10.10 - 0.16

from 8.42 - ~9.80m greenish grey shl to slt...calcareous…from ~9.67 - 9.80m slt-shl is cut by abundant buff-coloured calcite veinlets…

from ~9.80 - ~17.05m charcoal-grey to black… slt and shl...organic rich… locally has conchoidal fracture and a vitreous appearance...locally muddy…

from ~17.05 - ~18.20m green-grey slt...relatively competent (fairly intact)...locally broken and fractured...local buff calcite veins/veinlets…

from ~18.20 - 20.33m greyish to green grey…slt-shl rubble…from ~20.00 - ~20.18m carbonate rich horizon that is broken…EOH


HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-262

Hole No: RB-09-263




Core Size: BQTK


License: 007897M




mE / mN



Test Depth (m)



Member

29-Oct-09 -

0.00 9.11 OB Overburden. HF sst and exotic boulers. OB

9.11 18.80 RB Charcoal grey to black…shl and slt...core is badly broken throughout most of interval...calcareous...locally hosts abundant white to buff calcite veins/veinlets...interval is dominantly rubble that was slightly rounded during coring and thus is quite difficult to determine structure from coring artifact...core locally has a conchoidal fracture and a vitreous/shiny appearance along fracture surface...

RB 62 - 90shl/slt -10.07 - 0.20

from ~15.74 - ~17.47m charcoal grey slt-shl…relatively intact (only moderately broken)…

from 18.00 - 18.15m and ~18.40 - 18.70m abundant black, organic rich shl fragments - crush zone(?)...EOH


EOH

HOLE GEOCHEMISTRY


(m)(m) (m)

RB-09-263

…A4

APPENDIX 4. BOREHOLE RADIOMETRIC PROBE SPECIFICATIONS

Altius Resources Inc. / JNR Resources Inc.

General Information Overview The 2GHF-1000 triple gamma probe measures natural gamma radiation using three different type detectors. The 2GHF is from the DX series of probes which utilizes a faster FSK communications scheme and more versatility in interchangeability with multiple measurements. The probes most sensitive detector is a photo multiplier tube and 1.5” NaI crystal assembly. This detector is the same one used in the standard MSI HLP mining probe. Two different pairs of geiger-mueller tubes are installed in the probe above the NaI detector. These g-m tube pairs have been used successfully to determine ore grade in very high concentrations of U3O8. The count rate output of the ZP1200 g-m tube pair is about 1% of the NaI detector. The output of the ZP1320 g-m tube pair is about half of the ZP1200 tube pair. By having three different detector sensitivities, the 2GHF-1000 probe can be used in exploration and production projects with a wide variation in ore grade. Accurate concentrations can be measured in uranium ore grades ranging from less than 0.1% to as high as 20% U3O8. Data is logged from all five detectors on a single pass in the hole. The data is digitized in the probe and sent to the surface by 2SMA-1000 FSK modem/power supply. Theory of Operation The 2GHF measurements utilize proven methods for obtaining natural gamma ray flux via the use of a PMT/NaI Xtal scintillator and G-M tube pairs. As the sensitivity of the detectors is drastically different from one detector to another the probe is able to detect and output gamma count rates even though one or more detectors may be outputting the maximum counts the detector is capable of. The output of the detectors are pulses, which are in turn shaped, discriminated and then counted by a processor. This data is then combined digitally and sent through the cable line via, the FSK modem. Specifications Diameter 1.5 inches 38mm Length 64.5 inches 1.186 meters Temp 14 to 122 Deg. F -10 to 50 Deg. C Power 100V DC via a 2SMA modem section Approx. 110ma. Total probe string 150mA PMT/Xtal detector from bottom 6.0” .152 meters ZP1320 detector from bottom 23.0” .584 meters ZP1200 detector from bottom 26.5” .673 meters Combination 2SMA & 2GHF probes 71.0” 1.803 meters Dose rate range ZP1320 3 X 10\-3 to 2 X 10\2 mGy/h Dose rate range ZP1200 10\-3 to 10\2 mGy/h **NOTE** - The preceding product description and specifications were provided by Mount Sopris Instrument Co., Inc. Part No. 7000-0179A.

…A5

APPENDIX 5: CROSS-SECTIONS

494,000mE 5

0m

RL

80

mR

L49

RB‐09‐226

40m

Mu

St

Su

OB

0 5 10 15 20 25

S C A L E 1 / 5 0 0

METERS

For Radiometric Profile1mm = 10 CPS

Upper Humber River, NL

Date Drawn:


Rocky Brook Property

Wigwam Brook Area

A. Devereaux

0° A, Devereaux

10-Jan-2010

Area:

Projection:

NTS Sheets:

2x

12H06

Vertical Exaggeration:

1:500

DDH ID:

Logged By:

Drawn By:Projection Azimuth:

Scale:

RB-09-226

51m

RB‐09‐227

OB

Sm

St

Mm

493,320 4

0m

RL

70

mR

L493,260mE

0 5 10 15 20 25

S C A L E 1 / 5 0 0

METERS



Date Drawn:



Wigwam Brook Area

A. Devereaux

0° A, Devereaux

10-Jan-2010

Area:

Projection:

NTS Sheets:

2x

12H06


1:500

DDH ID:

Logged By:


Scale:

RB-09-227

RB‐09‐228

51m

St

Mu

OB

Su

493,500mE 493,560mE 4

0m

RL

70

mR

L

0 5 10 15 20 25

S C A L E 1 / 5 0 0

METERS



Date Drawn:



Wigwam Brook Area

A. Devereaux

0° A, Devereaux

10-Jan-2010

Area:

Projection:

NTS Sheets:

2x

12H06


1:500

DDH ID:

Logged By:


Scale:

RB-09-228

51.19m

RB‐09‐229

OB

Su

Mu

St

Mm

Sm

493,420mE 7

0m

RL

40

mR

L

0 5 10 15 20 25

S C A L E 1 / 5 0 0

METERS



Date Drawn:



Wigwam Brook Area

A. Devereaux

0° A, Devereaux

10-Jan-2010

Area:

Projection:

NTS Sheets:

2x

12H06


1:500

DDH ID:

Logged By:


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RB-09-229

RB‐09‐230

OB

101m

RB

Sl

Su

Mu

St

Mm

Sm

Ml

50mR

L492,940mE 493,000mE

20mR

L493,060mE

-10mR

L


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RB-09-230

0°


Wigwam Brook Area

0 5 10 15 20 25

S C A L E 1 / 5 0 0

METERS


RB‐09‐231

OB

Su

Mu

St

50m

5,473,080mN493,140mE 4

0m

RL

70

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L

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032°

82.5m

Sl

Sm

Ml

St

Mu

Mu20

OB

RB‐09

‐232

30

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L 6

0m

RL

5,472,120mN 493,000mE

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RB-09-232

302°

70

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L493,080mE5,472,080mN

40

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L

40.58m

RB-09-233

Mu10

Mu20

Mu25

Su10

Su20

Su22

Su30

OB

0 5 10 15 20 25

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Goose Anomaly Area

302°

41.58mMu10

Mu18

Mu18

Mu

Mu25

Su10

Su20

Su22

Su30

OB

RB‐09‐

234

5,472,020mN 4

0m

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70

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L493,120mE

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RB-09-234

RB‐09‐23

5

OB

Su30

Su22

Su20

Mu25

Mu20

Mu20

40.2m

Mu10

5,472,040mN 4

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70

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L493,120mE

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RB-09-235

RB‐09‐236

OB

Su30

Su20

Su10

Mu25

Mu20

Mu10

Mu7

40.22m

40

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L5,472,100mN

70

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L493,100mE

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RB-09-236

RB‐09‐2

37

OB

OB

OB

26m

St

493,300mE 4

0m

RL

70

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L5,472,580mN

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RB-09-237

RB‐09‐238

OB

Flt(?)

Mu

Flt(?)

23.143m

St

5,472,620mN 4

0m

RL

70

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L493,340mE

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RB-09-238

RB‐09‐23

9

OB

Su

Mu

St

Mm

Sm

75.25m

60

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L 3

0m

RL

5,472,660mN 493,360mE

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RB-09-239

302°

OB

Su

Mu

St

49.92m

RB‐09‐

240

493,240mE5,472,640mN 4

0m

RL

70

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L

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RB-09-240

RB‐09‐24

1

OB

Mu

St

59.98m

493,260mE5,472,660mN 4

0m

RL

70

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L

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RB-09-241

RB‐09

‐242

OB

Su

Mu

41.76m

St

493,200mE5,472,660mN 4

0m

RL

70

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L

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RB-09-242

RB‐09‐243

Mu

OB

Su

59.49m

St

Mm

Sm

493,220mE 3

0m

RL

60

mR

L

0 5 10 15 20 25

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RB-09-243

0°

30.22m

OB

St

Mm

Sm

RB‐09‐244

70

mR

L 4

0m

RL

493,000mE492,940mE

0 5 10 15 20 25

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RB-09-244

RB‐09‐245

OB

Mu20

Mu10

Sm

Ml

Sl

80.16m

493,020mE5,472,160mN 3

0m

RL

60

mR

L

0 5 10 15 20 25

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RB-09-245

302°

60.53m

RB‐09‐246

OB

Sst

Ml

Sl

RB

Su

Mst

Sst

Mst

496,780mE 49 4

0m

RL

70

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L

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RB-09-246

0°

RB‐09‐247

OB

Su‐D

24m

Su‐0

Su‐D'

Mu‐C

496,760mE 5

0m

RL

80

mR

L

0 5 10 15 20 25

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RB-09-247

RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN

30mR

L 60m

RL

0mR

L

5,477,440mN 496,760mE

0 5 10 15 20 25

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Birchy Hill Brook AreaRB-09-248

RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN

30mR

L 60m

RL

0mR

L

5,477,440mN 496,760mE

0 5 10 15 20 25

S C A L E 1 / 5 0 0

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RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN 30m

RL

60mR

L 0m

RL

5,477,440mN 496,760mE

0 5 10 15 20 25

S C A L E 1 / 5 0 0

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RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN

30mR

L 60m

RL

0mR

L

5,477,440mN 496,760mE

0 5 10 15 20 25

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RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN

30mR

L 60m

RL

0mR

L

5,477,440mN 496,760mE

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RB‐09‐248

Mu‐a

Su‐0

OB

Su‐D'

Mu‐B

Mu‐A

Mu‐C

77.63m

Ml

Sl

RB

496,700mE5,477,380mN

30mR

L 60m

RL

0mR

L

5,477,440mN 496,760mE

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RB‐09‐251

OB

Su‐D

Mu‐C

Sst

Mu‐B

Sst

Mst

Sst

Ml

71m

Sl

RB

496,820mE

10

mR

L

496,760mE

40

mR

L 7

0m

RL

10

0m

RL

5,477,400mN496,700mE

0 5 10 15 20 25

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RB-09-249

0°

RB‐09‐249

OB

Mu‐C

Mu‐B

Mu‐B

Mu‐B

Mu‐B

Mu‐B

49.52m

RB

Mu

Ml

Ml

Sl

496,580mE 4

0m

RL

70

mR

L

0 5 10 15 20 25

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RB-09-249

0°

RB‐09‐250

OB

Mst

Sst

Mst

Sst

Mst

Mu

Mu‐B

Sst

Mst

Ml

Sl

68.45m

RB

5,477,480mN 4

0m

RL

70

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L496,620mE

0 5 10 15 20 25

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RB-09-250

035°

RB‐09‐251

OB

Su‐D

Mu‐C

Sst

Mu‐B

Sst

Mst

Sst

Ml

71m

Sl

RB

496,760mE 4

0m

RL

70

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L5,477,400mN

0 5 10 15 20 25

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035°

RB‐09‐252

OB

Su

50.03m

Mu‐C

Sst

Sst

Ml

Sl

497,020mE 50m

RL

80mR

L496,960mE

0 5 10 15 20 25

S C A L E 1 / 5 0 0

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RB-09-252

12-Jan-2010

Mst

RB‐09‐253

Sst

OB

48.14m

RB

Sl

Ml

496,800mE 496,860m 40m

RL

70mR

L

0 5 10 15 20 25

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RB-09-253

RB‐09‐254

OB

Mu

Mu

Ml

50m

RB

Sl

496,660mE 49 40m

RL

70mR

L

0 5 10 15 20 25

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RB-09-254

RB‐09‐255

OB

Mu‐C

47m

Sst

Mu

Ml

Sl

RB

496,540mE 7

0m

RL

496 4

0m

RL

0 5 10 15 20 25

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RB-09-255

RB‐09‐256

OB

Mu‐C

Mu‐B

Su‐D'

Mu‐B

Mu‐B

Ml

Sl

RB

70m

496,560mE 4

0m

RL

5,477,460mN 7

0m

RL

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RB-09-256

RB‐09‐257

OB

Su‐D

53m

Sst

Mu‐A

Ml

Sl

RB

4 4

0m

RL

70

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L496,700mE

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RB-09-257

RB‐09‐258

OB

Su

Mu

Mu‐C'

Mst

Sst

Mst

Sst

Mst

60.63m

Sst

Ml

80

mR

L 5

0m

RL

5,477,360mN496,740mE

0 5 10 15 20 25

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RB-09-258

RB‐09‐259

OB

Mu

Mst

Sst

Sst

Sst

Ml

Sl

61.93m

RB

5,477,540mN 496,540mE 4

0m

RL

70

mR

L

0 5 10 15 20 25

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RB-09-259

052°

RB‐09‐260

41m

Sst

Mu

Ml

Sl

RB

OB

Su

496,520mE 496,580mE 40m

RL

70mR

L

0 5 10 15 20 25

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RB-09-260

RB‐09‐261

OB

Su‐D

51m

Mu

Sst

Ml

Sl

RB

496,480mE 4 4

0m

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L

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RB-09-261

RB‐09‐262

OB

RB

20.33m

497,100mE 90m

RL

5,477,060mN 60m

RL

0 5 10 15 20 25

S C A L E 1 / 5 0 0

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RB-09-262

030°

RB‐09‐263

18.8m

RB

OB

60mR

L 90m

RL

497,100mE

0 5 10 15 20 25

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0°

…A6

APPENDIX 6: 2009 FIVE-METRE SYSTEMATIC DRILL CORE SAMPLING

Five-metre Systematic Drill Core Sampling; 2009 Drilling Campaign

DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour

ApproximateGrain Size

OxidationScore

SampledBy

SampleComments

Counts perSecond (CPS)

MagneticSusceptibility (K)

SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-226 001 7.16 Su greyish cg sst 0 ADgreyish coloured, cg sst with kaolinite alteration of fsp's…blocky core…minor fg diss organic

detritus75 0.01 0.6 2.5 3.3

RB-09-226 002 12.16 Su greyish cg to vcg sst 0 AD some kaolinite alteration…minor organic trash and greenish mst clasts 75 0.00 0.7 2.5 3.4

RB-09-226 003 17.16 Su greyish pebble cgl -1 - 0 AD polymictic cgl…poorly sorted…micaceous…greenish-grey cement 70 0.00 0.3 2.2 1.0

RB-09-226 004 22.16 Su dark green slt -1 AD very micaceous…abundant fg, diss organic detritus 80 0.02 1.0 0.2 0.4

RB-09-226 005 27.16 Mu reddish-brown mst 4 AD completely oxidized…broken and disaggregated 70 0.04 0.7 1.5 1.2

RB-09-226 006 32.16 Mu reddish-brown mst 4 AD completely oxidized…from a caliche-rich section that is broken and disaggregated 65 0.00 0.2 2.0 3.2

RB-09-226 007 37.16 Mu greenish to reddish-brown mst -1 - 4 ADcompletely oxidized mst and greenish, reduced mst with cg sst grains throughout (granular

mst?)…reduction overprinting oxidation65 0.08 0.6 0.0 5.8

RB-09-227 001 9.10 St greyish mst -1 AD abundant kaolinite alteration…micaceous 67 0.01 0.6 3.0 0.0

RB-09-227 002 14.10 St greyish cg sst -1 AD abundant kaolinite alteration…micaceous 60 0.00 1.1 0.7 0.4

RB-09-227 003 19.10 St greyish cg sst -1 AD abundant kaolinite alteration…minor pinkish-peach coloured fsp 74 0.01 1.1 0.0 3.7

RB-09-227 004 24.10 St greyish cg sst -1 AD sst hosts abundant kaolinite alteration…mst (half of sample) is very micaceous 67 0.00 1.5 0.0 4.0

RB-09-227 005 29.10 St greyish fg to mg sst -1 AD hosts fg, stratified organic detritus…very micaceous 75 0.00 0.7 0.0 3.6

RB-09-227 006 34.10 Sm greyish mg sst -1 ADvery micaceous…minor kaolinite alteration…core is stained a reddish-pink colour…abundant fg

organic detritus78 0.00 1.3 1.5 1.5

RB-09-227 007 39.10 Sm greyish to reddish mg to cg sst -1 - 1 AD micaceous…kaolinite alteration of fsp's…minor fg organic detritus 70 0.02 1.0 2.1 1.3

RB-09-227 008 44.10 Sm tan-buff cg to vcg sst 1 ADsst has minor hematite disease…hosts moderate greenish and reddish mst…very

micaceous…some kaolinite alteration65 0.00 1.1 0.0 6.0

RB-09-227 009 49.10 Sm reddish to peachy vcg sst to cgl 1 AD moderate greenish mst rip-up clasts 70 0.00 0.4 1.6 1.1

RB-09-228 001 5.00 Su tan-buff pebble cgl -1 - 0 AD micaceous…moderate beigish clay development (dickite?) 70 0.02 1.1 0.0 6.1

RB-09-228 002 10.00 Su tan-buff cg to vcg sst -1 - 0 ADhosts minor, small, greenish mst rip-up clasts…minor rusty weathering…moderate kaolinite

alteration of fsp's65 0.00 0.4 2.2 1.1

RB-09-228 003 15.00 Mu greenish clayey mst -1 AD disaggregated…minor patchy reddish hematite visible locally 75 0.04 0.6 1.0 1.2

RB-09-228 004 20.00 Mu reddish-brown clayey mst 3 AD minor patchy to wispy reduction throughout…minor reddish carbonate caliche 75 0.04 0.7 1.4 3.5

RB-09-228 005 25.00 St greyish fg to mg sst -1 AD hosts stratified, fg organic detritus…abundant kaolinite alteration throughout…micaceous 65 0.00 1.0 0.8 3.6

RB-09-228 006 30.00 St greyish cg to vcg sst -1 AD hosts moderate kaolinite alteration of fsp's…vuggy texture 65 0.00 0.2 2.6 3.2

RB-09-228 007 35.00 St greyish cg sst -1 ADhosts moderate kaolinite alteration and minor organic detritus…micaceous…minor charcoal

grey mst rip-up clasts70 0.00 0.3 0.0 8.0

RB-09-228 008 40.00 St greyish mg sst -1 AD minor pebbles/granules…minor organic detritus…moderate kaolinite alteration 60 0.00 0.7 0.0 6.0

RB-09-228 009 45.00 St greyish cg to vcg sst -1 ADcg - vcg sst with greyish coloured mst…mst is micaceous…sst hosts minor charcoal grey

intermixed mst60 0.00 1.0 1.4 3.6

RB-09-228 010 50.00 St greyish cg to vcg sst -1 AD hosts charcoal grey mst rip-up clasts…moderate kaolinite alteration of fsp's throughout 80 0.00 0.9 0.0 8.2

RB-09-229 001 5.10 Su buff to grey cg sst 0 ADmoderate to strong kaolinite alteration of k-fsp…abundant beigish-white clay throughout…fsp's

are slightly orange60 0.00 0.6 1.9 0.1

RB-09-229 002 10.10 Su reddish-brown cg to vcg sst 2 AD moderately strong reddish-brown hematite…moderate bright white specks of kaolinite 65 0.00 0.2 2.0 3.2

RB-09-229 003 15.10 Mu greenish silty mst 1 AD minor remnant oxidation patches…micaceous 70 0.00 0.9 0.8 3.6

RB-09-229 004 20.10 Mu greenish silty mst -1 AD micaceous 65 0.07 1.2 0.6 5.9

RB-09-229 005 25.10 Mu greenish clayey to silty mst -1 AD massive…micaceous 65 0.03 1.1 2.4 0.2

RB-09-229 006 30.10 St greyish cg sst -1 AD minor organic trash…moderate kaolinite alteration 80 0.02 0.7 1.4 3.5

RB-09-229 007 35.10 St greyish cg sst -1 AD minor fg organic detritus…minor kaolinite alteration…micaceous 70 0.00 1.0 1.5 1.3

RB-09-229 008 40.10 St greyish cg sst to cgl -1 AD abundant fg py surrounding clast…micaceous…significant kaolinite throughout 75 0.00 0.8 0.1 5.9

RB-09-229 009 45.10 Sm reddish cg sst 2 AD moderate reddish hematite and kaolinite alteration throughout 60 0.00 0.8 1.7 8.0

RB-09-229 010 50.10 Sm reddish cg sst 2 AD minor hematite disease…moderate kaolinite alteration…minor reddish-brown mst 65 0.00 1.0 0.7 5.9

RB-09-230 001 6.50 Su tan-buff cg sst 0 AD micaceous…fg diss organic detritus throughout 70 0.00 0.8 1.5 1.3

Page 1 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-230 002 11.50 Mu rusty-red clayey mst 3 AD minor greenish reduction spots…micaceous 75 0.02 0.8 0.3 3.6

RB-09-230 003 16.50 St? greenish-grey cg to vcg sst -1 - 0 AD greenish mst rip-up clasts and some kaolinite alteration 65 0.00 0.3 2.0 3.3

RB-09-230 004 21.50 St? tan-buff to reddish cg sst 2 AD hematite disease…moderate kaolinite alteration 70 0.03 0.7 0.3 3.6

RB-09-230 005 26.50 St? tan-buff to reddish cg sst 0 - 4 AD large reddish hematite blotch…micaceous…fsp's altered an orangish colour 60 0.08 0.4 0.2 0.1

RB-09-230 006 31.50 Mm? greenish clayey mst -1 AD minor remnant mottled oxidation 60 0.00 0.7 0.0 5.8

RB-09-230 007 36.50 Sm? tan-buff cg sst 0 AD fsp's are a peachy-orange colour…moderate kaolinite alteration of fsp's throughout 70 0.00 0.4 1.7 7.8

RB-09-230 008 41.50 Sm? brick red silty mst to silt 4 AD very strongly oxidized…micaceous 85 0.03 0.6 0.0 8.0

RB-09-230 009 46.50 Sm? tan-buff to reddish-brown cg sst 1 AD minor reddish-brown mst rip-up clasts…micaceous…fsp's are a peachy-orange colour 77 0.02 0.8 1.5 1.3

RB-09-230 010 51.50 Sm? tan-buff cg sst 0 AD moderate kaolinite alteration…minor greyish intermixed mst 75 0.01 1.0 0.9 1.4

RB-09-230 011 56.50 Sm? tan-buff pebble cgl 1 AD minor reddish spotty hematite…moderate kaolinite alteration 80 0.07 0.6 0.9 3.5

RB-09-230 012 61.50 Ml? brick red slt 4 AD very strongly oxidized….massive…featureless 60 0.02 0.7 3.0 0.0

RB-09-230 013 66.50 Sl? tan-buff cg sst 1 AD vuggy…weak reddish-brown mottled hematite 80 0.06 1.3 0.4 1.6

RB-09-230 014 71.50 Sl? tan-buff cg to vcg sst 1 AD hematite disease…fg organic detritus…minor kaolinite alteration 55 0.08 0.8 2.0 3.5

RB-09-230 015 76.50 Sl? tan-buff mg to cg sst 1 AD minor hematite disease…moderate kaolinite alteration…fsp's are a peachy-orange colour 70 0.02 0.6 0.4 1.3

RB-09-230 016 81.50 Sl? reddish-brown to greenish cg sst -1 - 2 AD mstdy…greenish mst rip-up clasts…reddish-brown and greenish intermixed mst 65 0.14 1.1 1.4 3.6

RB-09-230 017 86.50 Sl? tan-buff cg sst 0 AD moderate kaolinite 60 0.24 0.4 1.4 3.3

RB-09-230 018 91.50 Sl? tan-buff cg sst 1 AD fractured…minor greenish intermixed mst…minor fg organic detritus 75 0.19 1.1 0.0 6.1

RB-09-230 019 96.50 RB dark greenish to black clayey mst to silt -1 AD massive…featureless 50 0.12 0.8 0.0 5.9

RB-09-231 001 7.50 Su reddish-brown mg sst -1 - 2 AD reddish-brown mottled/pervasive hematite…micaceous…fg diss organic detritus 70 0.06 0.8 0.8 3.6

RB-09-231 002 12.50 Su tan-buff cg to vcg sst 1 AD moderate kaolinite alteration…weak mottled reddish-brown hematite 65 0.10 0.2 0.2 5.6

RB-09-231 003 17.50 Mu greenish clayey mst -1 AD minor weak remnant oxidation…minor small reddish coloured carbonate caliche 50 0.00 0.6 0.0 1.3

RB-09-231 004 23.00 Mu greenish to brownish clayey mst -1 AD moderate limonite alteration 60 0.02 0.9 0.3 3.7

RB-09-231 005 28.00 St? reddish-brown cg sst 2 AD moderate mottled/pervasive hematite…moderate kaolinite alteration 60 0.03 0.4 1.6 1.1

RB-09-231 006 33.00 St? tan-buff vcg sst 1 AD patchy reddish-brown hematite…moderate kaolinite alteration of fsp's 55 0.02 1.0 2.4 0.2

RB-09-231 007 38.00 St? tan-buff to reddish-brown mg to cg sst 1 AD moderate kaolinite alteration…fg diss hematite (spotty) 60 0.00 0.8 0.4 1.3

RB-09-231 008 42.00 St? tan-buff cg sst 0 AD fg organic detritus…fsp's are a peachy-orange colour…moderate kaolinite alteration of fsp's 70 0.03 1.0 0.0 3.7

RB-09-231 009 47.00 St? tan-buff cg sst 0 AD moderate kaolinite alteration…fsp's are a peachy-orange colour…fg organic detritus 65 0.04 0.2 2.0 3.2

RB-09-232 001 10.00 Mu20 reddish-brown fg sst -1 - 1 AD weak mottled, reddish-brown hematite…ruddy appearance with minor greenish reduction 60 0.00 0.8 0.0 5.9

RB-09-232 002 15.00 Mu20 reddish-brown fg to mg sst -1 - 1 ADweak, mottled, reddish-brown hematite immediately down-hole from fracture and has a spotty

green alteration50 0.02 0.7 2.5 0.1

RB-09-232 003 20.00 Mu reddish-brown slt 3 AD strongly oxidized with minor bleached spots and wisps (white)…massive 60 0.00 1.0 0.7 0.3

RB-09-232 004 25.00 Mu reddish-brown silty mst 3 AD minor small, tan carbonate caliche and minor greenish reduction wisps and spots 60 0.00 0.2 1.5 3.3

RB-09-232 005 30.00 Mu reddish-brown clayey to silty mst 3 AD moderate tan to reddish-brown carbonate caliche…minor greenish reduction wisps and spots 65 0.00 0.4 0.4 1.2

RB-09-232 006 35.00 Mu reddish-brown clayey mst 4 AD strongly oxidized…massive…featureless 65 0.03 0.9 0.0 8.3

RB-09-232 007 40.00 Mu grey-green silty mst -1 AD minor reddish-brown remnant oxidation 55 0.01 0.4 1.4 0.0

RB-09-232 008 45.00 St greyish mg sst -1 AD very micaceous…hosts fg organic detritus that is stratified 65 0.03 0.2 1.0 1.1

RB-09-232 009 50.00 St greyish to reddish-brown cg - vcg sst 2 AD strong reddish-brown hematite patch…micaceous 60 0.04 1.0 0.0 0.4

RB-09-232 010 55.00 St tan-buff cg sst 1 AD spotty hematite disease (small)…moderate kaolinite alteration…micaceous 65 0.05 0.4 0.0 3.5

Page 2 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-232 011 60.00 St reddish-brown cgl 3 AD moderate to strong kaolinite alteration…strong reddish-brown hematite (pervasive) 70 0.04 0.8 1.3 0.2

RB-09-232 012 65.00 Sm reddish-brown vcg sst to cgl 2 AD moderate reddish-brown patchy hematite…moderate kaolinite alteration 60 0.02 0.6 0.3 3.5

RB-09-232 013 70.00 Ml greenish to reddish-brown silty mst -1 AD strongly reduced with moderate patchy, remnant oxidation (reddish-brown)…micaceous 55 0.00 0.8 0.0 3.6

RB-09-232 014 75.00 Sl greenish silty mst -1 AD micaceous…minor weak, remnant reddish-brown mottled hematite 65 0.05 0.4 2.1 1.1

RB-09-232 015 80.00 Sl tan-buff cg to vcg sst 1 AD hosts abundant greenish mst rip-up clasts…minor reddish-brown spotty hematite 70 0.00 0.2 0.5 1.1

RB-09-233 001 5.50 Su tan-buff to greyish cg to vcg sst 1 AD moderate kaolinite alteration of fsp's…vuggy…micaceous 60 0.01 0.8 1.9 0.1

RB-09-233 002 10.00 Su greenish clayey mst -1 - 1 AD strongly reduced with weak remnant reddish-brown oxidation throughout 55 0.02 0.4 0.9 3.4

RB-09-233 003 15.50 Su colourful cgl 0 AD poorly sorted polymictic cgl 60 0.02 0.4 1.6 1.1

RB-09-233 004 20.50 Mu reddish-brown fg sst 2 AD moderate reddish-brown oxidation with well cemented carbonate caliche…minor muscovite 50 0.00 0.6 0.2 0.2

RB-09-233 005 25.50 Mu reddish-brown silty mst 3 AD very minor greenish reduction as wisps…broken and disaggregated 60 0.00 0.6 1.0 1.2

RB-09-233 006 30.50 Mu reddish-brown slt 3 AD micaceous…well oxidized with minor tan-buff, bleached spots 50 0.02 0.6 0.0 8.1

RB-09-233 007 35.50 Mu reddish-brown clayey to silty mst 4 AD strongly oxidized…hosts minor tan-coloured carbonate nodules 50 0.00 0.8 0.0 3.7

RB-09-233 008 40.50 Mu reddish-brown clayey mst 4 AD strongly oxidized 60 0.01 0.2 0.0 7.9

RB-09-234 001 5.00 Su reddish-brown vcg sst 1 AD moderate kaolinite alteration of fsp's…micaceous 66 0.00 0.8 0.0 1.4

RB-09-234 002 10.00 Su tan-buff cg sst 1 - 2 ADminor reddish-brown hematite disease and patchy hematite along fracture surface…moderate

kaolinite alteration of fsp's68 0.01 0.7 1.3 0.2

RB-09-234 003 15.00 Su tan-buff cg sst 1 AD small, reddish-brown hematite disseminations throughout…micaceous 76 0.01 0.6 0.9 3.5

RB-09-234 004 20.00 Su reddish-brown clayey mst -1 - 3 AD moderately strong oxidation with some greenish reduction mottling…broken and disaggregated 74 0.06 0.4 0.4 1.2

RB-09-234 005 25.00 Mu tan-buff mg to cg sst 0 AD k-fsp rich…hosts stratified, fg, organic detritus 69 0.05 0.5 0.3 3.5

RB-09-234 006 30.00 Mu reddish-brown cg sst to cgl 1 AD weak reddish-brown mottled/stratified hematite…micaceous 68 0.01 1.2 0.0 3.9

RB-09-234 007 35.00 Mu reddish-brown silty mst 4 AD strongly oxidized…very micaceous 63 0.02 0.2 0.0 3.4

RB-09-234 008 40.00 Mu reddish-brown slt 4 AD strongly oxidized…hosts carbonate nodules…micaceous 60 0.03 0.6 0.0 1.3

RB-09-235 001 6.00 Su tan-buff cg sst 0 MD pink fsp's…cobbles of sst 65 0.00 0.2 0.0 1.2

RB-09-235 002 11.00 Su reddish-brown mg to cg sst 1 MDmoderate kaolinite alteration of fsp's (bright white specks)…weak reddish-brown hematite

alteration59 0.00 0.4 1.3 0.0

RB-09-235 003 16.00 Su reddish-brown mg to cg sst 2 MD weak to moderate reddish-brown stratified hematite 64 0.00 0.9 0.2 0.3

RB-09-235 004 21.00 Su reddish-brown silty mst 4 MD strongly oxidized 62 0.03 0.8 0.2 0.3

RB-09-235 005 26.00 Su greyish to tan-buff mg to cg sst -1 MD hosts moderate stratified organic detritus 60 0.04 0.3 1.6 1.1

RB-09-235 006 31.00 Mu tan-buff cgl 1 MD weak reddish-brown hematite 65 0.02 0.2 0.5 10.1

RB-09-235 007 36.00 Mu reddish-brown clayey mst 4 MD strongly oxidized 66 0.04 0.4 0.0 1.3

RB-09-236 001 6.00 Su tan-buff to greyish cg sst 0 MD minor kaolinite alteration of fsp's 73 0.00 0.2 0.0 3.5

RB-09-236 002 11.00 Su greenish slt -1 MD strongly reduced with minor reddish-brown remnant oxidation…micaceous 76 0.04 0.8 0.0 1.4

RB-09-236 003 16.00 Mu greenish silty mst -1 MD strongly reduced 74 0.04 0.6 0.1 5.8

RB-09-236 004 21.00 Mu greyish cg sst -1 MD minor fg diss. organic detritus 73 0.02 0.4 0.0 3.5


RB-09-236 006 31.00 Mu reddish-brown slt 4 MD micaceous…completely oxidized 79 0.01 0.8 1.4 3.5

RB-09-236 007 36.00 Mu reddish-brown silty mst 4 MD strongly oxidized 72 0.03 0.5 0.0 8.2

RB-09-237 001 14.00 St? greyish cg sst -1 AD patchy of fg diss py…micaceous 57 0.00 0.9 0.0 3.8

RB-09-237 002 19.00 St? greyish cg to vcg sst -1 AD micaceous…moderate kaolinite alteration…greyish mst rip-up clast 62 0.00 0.8 0.0 3.6

Page 3 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-237 003 24.00 St? greyish cg sst -1 AD bright white specks of kaolinite(?) alt…minor organic trash fragments 65 0.00 0.4 1.4 3.4

RB-09-238 001 8.25 Mu/Fault reddish-brown clayey mst 4 AD hosts reddish-brown carbonate nodules 58 0.05 0.9 3.3

RB-09-238 002 14.00 Mu/Fault reddish-brown clayey mst 3 AD minor pebbles throughout…minor greenish reduction 60 0.03 0.6 0.2 0.2

RB-09-238 003 19.00 St greyish cg to vcg sst -1 AD micaceous…minor fg diss organic stratified detritus and beigish clay (dickite?) 61 0.00 0.5 1.0 1.2

RB-09-239 001 5.00 Su tan-buff cg sst 0 AD minor kaolinite alteration…unoxidized 63 0.01 0.9 0.0 1.5

RB-09-239 002 9.95 Su tan-buff cg sst 0 AD weakly cemented and partially disaggregated…minor reddish-brn mst 60 0.01 0.7 0.8 0.2

RB-09-239 003 15.00 Mu reddish-brown clayey mst 3 AD hosts reddish-brown carbonate caliche…minor greenish reduction 63 0.02 0.5 2.7 1.1

RB-09-239 004 20.00 St greyish mg to cg sst -1 AD micaceous…hosts fg diss organic detritus 62 0.00 0.6 1.0 1.2

RB-09-239 005 25.00 St greyish cg sst -1 AD hosts abundant small charcoal-grey coloured mst rip-up clasts that are stratified 60 0.00 0.9 0.0 6.0

RB-09-239 006 30.00 St greyish cg to vcg sst -1 AD minor kaolinite alteration of fsp's 66 0.00 0.7 0.0 3.6

RB-09-239 007 35.00 St greyish slt -1 AD very micaceous…intermixed greyish mst and sst 65 0.03 0.5 0.3 3.5

RB-09-239 008 40.00 St greyish cg sst -1 AD micaceous…hosts pink fsp's 64 0.01 0.7 0.0 6.0

RB-09-239 009 45.00 St greyish cg sst -1 ADfg diss and wispy organic detritus…minor pink fsp's…oxidized sulphides locally

throughout…micaceous66 0.01 0.9 0.0 1.4

RB-09-239 010 50.00 Sm greyish cg to vcg sst -1 AD pink lithic fragments…minor kaolinite alt of fsp's 60 0.01 0.2 0.2 0.1

RB-09-239 011 55.00 Sm greyish cg to vcg sst -1 ADpink lithic fragments…micaceous…minor kaolinite alt of fsp's…minor dark grey mst rip-up

clasts65 0.01 0.5 0.0 1.3

RB-09-239 012 60.00 Sm greyish cg to vcg sst -1 AD pink lithic fragments…micaceous…minor greenish-grey mst rip-up clasts 63 0.00 0.4 0.0 5.8

RB-09-239 013 65.00 Sm black to dark greenish-grey clayey mst -1 AD very reduced 62 0.04 0.5 0.0 1.3

RB-09-239 014 70.00 Sm greyish mg to cg sst -1 AD micaceous…minor kaolinite alteration 57 0.00 0.4 0.0 3.5

RB-09-239 015 75.00 Sm greyish cg to vcg sst -1 AD micaceous…minor kaolinite alteration 59 0.10 0.6 0.8 0.2

RB-09-240 001 7.50 Su reddish cg sst 3 AD moderately strong reddish-brown patchy hematite throughout…moderate kaolinite alteration 67 0.02 0.3 1.4 0.0

RB-09-240 002 12.50 Mu reddish-brown clayey mst 3 AD strongly oxidized with minor wispy and patchy greenish reduction throughout 72 0.07 0.9 0.3 3.7

RB-09-240 003 17.50 Mu reddish-brown clayey mst 2 ADabundant nodules and nodule-rich fragments with patchy and wispy reduction

throughout…large buff coloured caliche70 0.07 0.8 0.4 1.4

RB-09-240 004 22.50 Mu tan-buff cg sst -1 AD pink lithic fragments…fractured parallel TCA...has a reduced appearance (bleached?) 63 0.02 0.7 0.1 5.8

RB-09-240 005 27.50 St greyish cg sst -1 AD intermixed charcoal grey mst (organic-rich)…micaceous 68 0.03 0.8 0.0 1.4

RB-09-240 006 32.50 St greyish cg sst -1 AD moderate kaolinite alteration of fsp's 62 0.00 0.5 1.9 0.0

RB-09-240 007 37.50 St greyish mg to cg sst -1 AD moderate kaolinite alteration of fsp's…micaceous 69 0.00 0.1 3.7 0.0

RB-09-240 008 42.50 St greyish cg to vcg sst -1 AD micaceous…minor fg oxidized sulphides…minor kaolinite alteration of fsp's throughout 62 0.02 1.0 0.0 3.8

RB-09-240 009 47.50 St greyish cg to vcg sst -1 AD minor peachy coloured fsp's…moderate kaolinite alteration of fsp's 59 0.02 0.2 0.2 0.1

RB-09-241 001 9.00 Mu greyish slt -1 MD micaceous 63 0.04 0.3 0.9 3.4

RB-09-241 002 14.00 Mu reddish-brown silty mst 4 MD nodular…strongly oxidized 61 0.09 0.4 1.6 1.1

RB-09-241 003 19.00 Mu greenish slt to mg sst -1 MD strongly reduced 69 0.04 0.4 3.1 0.0

RB-09-241 004 24.00 Mu greyish cg sst -1 MD weakly consolidated to disaggregated 61 0.04 0.2 0.0 1.2

RB-09-241 005 29.00 St greyish cg sst -1 MD strongly reduced…strong kaolinite alteration of fsp's 63 0.01 0.4 3.3 1.0

RB-09-241 006 34.00 St greyish cg sst -1 MD strong kaolinite alteration of fsp's…strongly reduced 66 0.00 0.7 0.2 0.2

RB-09-241 007 39.00 St greyish cg sst -1 MD disaggregated…strong kaolinite alteration…strongly reduced…poss. fault zone 65 0.00 0.1 0.3 3.3

RB-09-241 008 44.00 St greyish mg sst -1 MD fg organic detritus and blebs…moderate kaolinite alteration 67 0.01 0.9 0.0 0.3

RB-09-241 009 49.00 St greyish cg sst -1 MDorganic stain along fracture (organic fragment)…moderate kaolinite alteration…strongly

reduced64 0.02 0.2 0.0 3.4

Page 4 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-241 010 54.00 St greyish cg sst -1 MD organic detritus throughout…micaceous 62 0.00 0.7 0.0 5.9

RB-09-241 011 59.00 St greyish mg to cg sst -1 MD moderate kaolinite alteration of fsp's…micaceous…strongly reduced 60 0.00 0.7 0.0 3.6

RB-09-242 001 6.00 Su reddish-brown cg sst 3 MD moderate reddish-brown pervasive hematite 64 0.01 0.6 0.0 3.6

RB-09-242 002 11.00 Su reddish-brown cg to vcg sst 3 MD moderately strong reddish-brown pervasive hematite…moderate kaolinte alteration of fsp's 68 0.00 1.1 0.0 3.8

RB-09-242 003 16.00 Mu greenish clayey to silty mst -1 MD strongly reduced with minor remnant oxidation 64 0.04 1.0 0.0 3.8

RB-09-242 004 21.00 Mu greyish mg sst -1 MD abundant fg diss organic detritus…moderate kaolinite alteration 63 0.03 0.5 0.0 8.1


RB-09-242 006 31.00 Mu greenish clayey mst -1 MD strongly reduced 63 0.04 0.4 1.9 0.0

RB-09-242 007 36.00 St greyish cg to vcg sst -1 MD strong kaolinite alteration of fsp's…strongly reduced 72 0.01 0.6 0.0 3.6

RB-09-242 008 41.00 St greyish cg sst -1 MD strong kaolinite alteration of fsp's…strongly reduced 62 0.01 0.2 0.0 7.9

RB-09-243 001 5.13 Su reddish-brown cgl 2 MD moderate reddish-brown hematite 70 0.01 0.7 0.0 1.4

RB-09-243 002 10.00 Mu greenish-grey slt -1 MD strongly reduced 66 0.06 0.6 0.0 3.6

RB-09-243 003 15.00 Mu greenish-grey slt -1 MD micaceous…strongly reduced 65 0.05 0.4 1.9 0.0

RB-09-243 004 20.00 Mu greyish slt -1 MD micaceous…stratified organic detritus 67 0.04 1.0 1.3 0.3

RB-09-243 005 25.00 Mu reddish-brown to greenish clayey mst -1 - 2 MD both oxidized and reduced (approx. equal proportions of each) 68 0.04 0.4 0.0 5.8

RB-09-243 006 30.00 St greyish cg to vcg sst -1 MD moderate kaolinite alteration of fsp's…strongly reduced 63 0.00 0.1 3.3 0.9

RB-09-243 007 35.00 St greyish cg sst -1 MD disaggregated…moderate kaolinite alteration of fsp's…strongly reduced 62 0.01 0.5 0.0 5.9

RB-09-243 008 40.00 St greyish cg sst -1 MD moderate kaolinite alteration of fsp's…reduced 64 0.00 0.6 1.6 1.2

RB-09-243 009 45.00 Mm? reddish-brown cg sst 2 MD moderate reddish-brown mottled hematite 70 0.01 0.3 1.5 3.3

RB-09-243 010 50.00 Sm reddish-brown cg sst 2 MD moderate reddish-brown hematite…pink fsp's throughout 75 0.00 0.9 1.3 5.8

RB-09-243 011 55.00 Sm reddish-brown cg to vcg sst 3 MD moderate reddish-brown hematite…pink fsp's throughout 76 0.01 0.8 4.2 3.3

RB-09-243 012 60.00 Sm reddish-brown cg sst 3 MD hosts abundant reddish-brown mst rip-up clasts 74 0.01 0.8 0.2 0.3

RB-09-244 001 9.00 St greyish mg sst -1 MD broken and partially disaggregated…moderate kaolinite alteration 69 0.01 0.3 1.0 1.1

RB-09-244 002 14.00 St greyish cg to vcg sst -1 MD minor kaolinite alteration…reduced 75 0.01 0.5 0.9 3.5

RB-09-244 003 19.00 Sm tan-buff to reddish-brown cgl 3 MD local strong, reddish-brown patchy hematite 75 0.00 0.7 0.0 5.9

RB-09-244 004 24.00 Sm reddish-brown cg sst 3 MDmoderate reddish-brown stratified hematite and reddish-brown to greenish-grey mst rip-up

clasts68 0.00 0.2 0.9 3.4

RB-09-244 005 29.00 Sm reddish-brown mg sst 3 MD micaceous…moderate reddish-brown pervasive hematite 75 0.01 0.9 0.4 1.4

RB-09-245 001 8.00 Mu reddish-brown fg sst 3 MD hosts abundant tan-buff carbonate caliche and caliche debris (frags, etc) 67 0.02 0.9 0.1 5.9

RB-09-245 002 13.00 Mu greenish slt -1 MD strongly reduced with patchy reddish-brown oxidation 65 0.04 1.0 0.0 3.8

RB-09-245 003 18.00 Mu reddish-brown clayey to silty mst 4 MD completely oxidized 72 0.02 0.5 1.9 0.0

RB-09-245 004 23.00 Mu reddish-brown slt 3 MDstrongly oxidized with minor greenish reduction wisps and spots…hosts minor carbonate

caliche69 0.02 1.5 0.0 4.0

RB-09-245 005 28.00 Mu reddish-brown clayey mst 3 MD strongly oxidized with dark grey patches and wisps (reduction related?) 64 0.03 0.5 0.0 1.3

RB-09-245 006 33.00 Mu reddish-brown clayey to silty mst 4 MD completely oxidized…large carbonate caliche just above sampled area 70 0.02 0.5 1.3 0.1

RB-09-245 007 38.00 Mu greenish to reddish-brown clayey to silty mst -1 - 1 MD dominantly reduced with moderate patchy and wispy oxidation 64 0.03 0.4 2.1 1.1

RB-09-245 008 43.00 Sm greyish to tan-buff cgl -1 MD minor reddish-brown blotchy hematite…minor py 66 0.00 1.3 0.0 10.7

RB-09-245 009 48.00 Sm reddish-brown cg to vcg sst 3 MDmicaceous…moderately strong kaolinite alteration….moderately strong reddish-brown hematite

alteration…hosts reddish-brown mst rip-up clasts72 0.00 0.5 0.0 5.9

RB-09-245 010 53.00 Sm tan-buff cgl 2 MD hosts reddish-brown hematite spots (hematite disease) 69 0.00 1.2 0.0 6.1

Page 5 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-245 011 58.00 Sm reddish-brown cg sst 1 MD micaceous…weak reddish-brown pervasive hematite 71 0.00 0.6 0.0 1.4

RB-09-245 012 63.00 Sm reddish-brown cg to vcg sst 4 MD strong reddish-brown pervasive hematite…moderate kaolinite alteration of fsp's 71 0.00 1.0 0.0 8.4

RB-09-245 013 68.00 Ml greenish clayey mst -1 MD strongly reduced 70 0.02 0.6 0.0 3.6

RB-09-245 014 73.00 Sl tan-buff cg sst 0 MD minor kaolinite alteration of fsp's 69 0.00 0.8 0.0 10.5

RB-09-245 015 78.00 Sl tan-buff cg sst 1 MD minor fg diss reddish hematite…moderate kaolinite alteration of fsp's 71 0.00 0.0 3.7 0.0

RB-09-246 001 8.00 Su reddish cg to vcg sst 3 AD mottled, reddish hematite alteration…fsp's are a peachy-orange colour 77 0.00 0.4 1.9 0.0

RB-09-246 002 13.00 Su tan-buff cg to vcg sst 0 AD moderate kaolinite alteration…broken and fractured 68 0.00 0.8 1.0 1.3

RB-09-246 003 18.00 Mu reddish-brown clayey to silty mst 3 AD strongly oxidized with minor wispy greenish reduction 81 0.01 0.5 0.0 10.4

RB-09-246 004 23.00 Mu reddish-brown silty mst 4 AD strongly oxidized…somewhat granular 63 0.00 0.9 0.0 8.1

RB-09-246 005 28.00 Mu reddish-brown cg sst 2 ADminor greenish reduction…moderate mottled reddish-brown hematite…minor kaolinite


RB-09-246 006 33.00 Mst reddish-brown silty mst 3 AD minor patchy charcoal grey patches 73 0.01 1.2 0.0 6.1

RB-09-246 007 38.00 Sst greyish cg to vcg sst -1 AD pink fsp's…minor kaolinite alteration of fsp's 67 0.00 1.3 1.5 1.5

RB-09-246 008 43.00 Mst reddish-brown clayey mst 4 AD completely oxidized 68 0.04 0.3 1.5 3.3

RB-09-246 009 48.00 Mst reddish-brown clayey to silty mst 4 MD completely oxidized 73 0.04 0.9 0.0 6.0

RB-09-246 010 53.00 Mst greenish-grey slt -1 MD micaceous…strongly oxidized 71 0.09 0.6 1.6 1.2

RB-09-246 011 58.00 RB Fm greyish clayey mst -1 MD -- 79 0.02 0.8 0.2 0.3

RB-09-247 001 6.00 Su tan-buff to reddish-brown cg sst 3 MD strong reddish diss hematite 67 0.00 0.8 0.0 3.7

RB-09-247 002 11.00 Su tan-buff to reddish-brown cg to vcg sst 1 MD moderate kaolinite alteration of fsp's…weak reddish-brown hematite 79 0.00 0.7 0.0 0.3

RB-09-247 003 16.00 Mu reddish-brown silty mst 4 MD strongly hematitized 70 0.03 0.9 3.2 1.2

RB-09-247 004 21.00 Mu reddish-brown granular mst 3 MD minor greenish reduction 77 0.03 0.7 0.3 3.6

RB-09-248 001 6.03 Su reddish-brown clayey mst 4 MD strongly oxidized 65 0.04 0.7 1.0 1.3

RB-09-248 002 11.00 Mu reddish-brown cg sst 2 MD weak to moderate reddish-brown mottled/pervasive hematite 78 0.00 0.5 2.5 0.0

RB-09-248 003 16.00 Mu reddish-brown cg to vcg sst 1 MD weak mottled reddish-brown hematite…minor kaolinite alteration of fsp's 71 0.00 0.1 3.3 0.9

RB-09-248 004 21.00 Mu reddish-brown slt to fg sst 4 MD completely oxidized 70 0.04 0.7 1.4 3.4

RB-09-248 005 26.00 Mu reddish-brown to greenish mg sst -1 - 2 MD blotchy oxidation/reduction…moderate kaolinite alteration of fsp's 68 0.00 0.9 1.0 1.4

RB-09-248 006 31.00 Mu greenish clayey mst -1 MD micaceous…strongly reduced 71 0.04 0.8 1.3 0.2

RB-09-248 007 36.00 Mu tan-buff cg sst 0 MD hosts abundant reddish-brown mst rip-up clasts 71 0.02 1.0 0.0 10.7

RB-09-248 008 41.00 Ml reddish-brown clayey mst 4 MD strongly oxidized 73 0.04 0.5 1.0 1.2

RB-09-248 009 46.00 Sl greyish cg sst to cgl -1 MD moderate kaolinite alteration of fsp's…reduced 74 0.00 0.5 0.0 10.3

RB-09-248 010 51.00 RB Fm dark green-grey shale -1 MD organic-rich 73 0.04 0.6 0.3 3.5



RB-09-248 013 66.00 RB Fm charcoal-grey shale -1 MD organic-rich 71 0.03 1.0 0.0 3.8

RB-09-249 001 7.10 Mst reddish-brown clayey mst 4 MD strongly oxidized 76 0.70 0.8 0.7 0.3

RB-09-249 002 12.00 Sst reddish-brown cg sst 2 MD weak reddish-brown pervasive hematite 70 0.02 0.8 0.4 1.4

RB-09-249 003 17.00 Sst greenish-grey mg - cg sst -1 MD small greenish mst chips…moderately strong kaolinite alteration of fsp's 72 0.00 0.6 0.0 5.9

RB-09-249 004 22.00 Sst greenish vcg sst -1 MD hosts abundant greenish mst chips 74 0.02 0.4 0.3 3.5

Page 6 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-249 005 27.00 Sst greyish mg sst -1 MD tr to 1% oxidized sulphides…micaceous…abundant fg organic detritus 72 0.01 0.6 0.2 0.2

RB-09-249 006 32.00 Ml greenish to reddish-brown fg sst -1 - 1 MD mottled/patchy oxidation/reduction 75 0.05 0.2 0.2 5.6


RB-09-249 008 42.00 RB Fm greenish to reddish-brown clayey mst -1 - 2 MD oxidized and reduced 77 0.04 0.6 1.9 0.1

RB-09-249 009 47.00 RB Fm greenish slt -1 MD calcareous 79 0.03 0.2 1.5 3.3


RB-09-250 002 13.00 Sst reddish-brown cg sst 3 MD moderately oxidized…pink fsp's 83 0.00 0.8 0.0 3.7

RB-09-250 003 18.00 Sst reddish-brown vcg sst 2 MD moderately oxidized..mottled reddish-brown oxidation 81 0.05 0.4 0.7 5.7

RB-09-250 004 23.00 Mst reddish-brown slt 4 MD strongly oxidized 71 0.02 0.4 0.7 5.7

RB-09-250 005 28.00 Sst reddish-brown fg sst 3 - 4 MD mstdy…minor greenish reduction spots 70 0.01 0.8 1.0 1.3

RB-09-250 006 33.00 Sst greyish mg sst -1 - 1 MD moderate kaolinite alteration of fsp's…weak mottled hematite alteration 72 0.01 0.7 1.6 1.2

RB-09-250 007 38.00 Sst charcoal-grey mg sst -1 MD organic rich…micaceous 72 0.03 0.6 0.0 1.3

RB-09-250 008 43.00 Mst reddish-brown silty mst -1 MD strongly oxidized 81 0.03 1.0 0.2 3.7

RB-09-250 009 48.00 Ml reddish-brown to greenish silty mst -1 - 2 MD oxidized and reduced 71 0.03 0.6 0.0 3.6

RB-09-250 010 53.00 Ml greenish silty mst -1 MD strongly reduced with minor remnant oxidation 70 0.03 0.2 0.8 5.6

RB-09-250 011 58.00 Sl greenish cgl -1 MD disaggregated and broken…greenish and reduced 74 0.02 0.4 3.3 1.0

RB-09-250 012 63.00 RB Fm charcoal-grey to black clayey mst -1 MD organic rich 76 0.03 0.6 0.0 1.3

RB-09-250 013 68.00 RB Fm greenish-grey slt -1 MD calcareous 80 0.01 0.7 0.0 1.4

RB-09-251 001 6.00 Su reddish-brown cg sst 3 MD spotty, reddish-brown hematite disease 72 0.01 0.9 0.7 0.3


RB-09-251 003 16.00 Mu greenish clayey mst -1 MD minor tan-buff carbonate caliche…minor oxidation 70 0.01 0.6 1.6 1.2




RB-09-251 007 36.00 Mu reddish-brown clayey to silty mst 4 MD minor greyish patches 71 0.03 0.6 1.0 1.3

RB-09-251 008 41.00 Sst reddish-brown silty mst 4 MD micaceous…strongly oxidized 76 0.03 0.6 1.6 1.2

RB-09-251 009 46.00 Sst greyish cg sst -1 MD moderate to strong kaolinite alteration…weak greenish reduction 75 0.01 0.7 0.4 1.3

RB-09-251 010 51.00 Sst tan-buff mg sst -1 MD minor spotty green alteration 72 0.01 0.0 1.3 5.4

RB-09-251 011 56.00 Mst reddish-brown clayey to silty mst 4 MD greyish patches 74 0.04 0.2 1.4 0.0

RB-09-251 012 61.00 Sl greenish fg to mg sst -1 MD weak reddish-brown hematite…strongly reduced 68 0.03 0.8 0.0 1.4

RB-09-251 013 66.00 Sl greyish to greenish cgl -1 MD broken and disaggregated…mstdy (greenish mst) 67 0.03 0.5 0.0 10.5

RB-09-251 014 71.00 RB Fm charcoal-grey slt -1 MD calcareous…organic-rich…calcite vein 71 0.00 0.3 0.5 1.2

RB-09-252 001 5.00 Sst greyish vcg sst 0 MD moderate kaolinite alteration of fsp's 54 0.00 0.4 0.0 3.6

RB-09-252 002 10.00 Mst reddish-brown clayey mst 3 MD minor greenish reduction…strongly oxidized 69 0.08 0.4 0.5 1.2


RB-09-252 004 20.00 Mst reddish-brown to greenish mg sst -1 - 2 MD weak mottled oxidation and blotchy greenish reduction 70 0.01 0.8 0.8 0.2

RB-09-252 005 25.00 Mst tan-buff mg sst -1 MD moderate to strong kaolinite alteration…minor fg organics 66 0.03 0.4 0.8 0.1

Page 7 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-252 006 30.00 Sst reddish-brown cg to vcg sst 1 MD weak reddish-brown mottled hematite 57 0.03 0.7 0.0 1.4

RB-09-252 007 35.00 Sst reddish-brown slt 4 MD strongly oxidized 59 0.09 0.5 1.4 3.4

RB-09-252 008 40.00 Sst reddish-brown silty mst 3 MD strongly oxidized with minor greenish reduction 57 0.05 0.8 0.4 1.4

RB-09-252 009 45.00 Ml reddish-brown clayey mst 3 MD strongly oxidized with minor greenish reduction 56 0.08 0.8 0.4 1.4

RB-09-252 010 50.00 Sl greyish slt -1 MD calcareous 64 0.09 0.0 0.2 5.5

RB-09-253 001 6.00 Sst tan-buff cg sst 0 MD greenish spotty alteration…moderate kaolinite alteration 63 0.05 0.8 0.0 3.7

RB-09-253 002 11.00 Sst greenish cg sst -1 MD strongly reduced and greenish 64 0.04 0.7 0.0 3.7

RB-09-253 003 16.00 Mst tan-buff to greenish fg to mg sst 0 MD moderate kaolinite alteration of fsp's…minor greenish mst laminae 80 0.04 1.2 0.0 6.1

RB-09-253 004 21.00 Mst reddish-brown to greenish silty mst 3 MD minor wispy greenish reduction 62 0.02 0.4 0.0 0.2

RB-09-253 005 26.00 Mst greenish to reddish-brown clayey mst 2 MD both oxidized and reduced 70 0.07 0.7 0.0 12.8

RB-09-253 006 31.00 Mst reddish-brown clayey mst -1 MD strongly oxidized with greyish patches 59 0.07 0.5 0.2 0.2

RB-09-253 007 36.00 Ml greenish to reddish-brown silty mst -1 MD minor oxidation 70 0.03 0.2 0.0 3.4

RB-09-253 008 41.00 Sl greenish-grey cg to vcg sst -1 MD pale green alteration…minor kaolinite alteration of fsp's 50 0.02 0.9 1.3 0.2

RB-09-253 009 46.00 RB Fm charcoal grey shale -1 MD organic rich 58 0.08 0.4 2.2 1.0

RB-09-254 001 9.00 Mu reddish-brown clayey mst 3 MD strongly oxidized with minor greenish reduction spots and wisps 71 0.09 0.8 0.0 5.9

RB-09-254 002 14.00 Mu reddish-brown slt 4 MD strongly oxidized 71 0.03 0.8 1.5 1.3


RB-09-254 004 24.00 Sst greenish cgl -1 MD abundant greenish mst chips…fg diss py throughout 71 0.00 0.5 1.6 1.2

RB-09-254 005 29.00 Mst greenish silty mst -1 MD strongly reduced 70 0.00 0.8 1.0 1.3

RB-09-254 006 34.00 Mst reddish-brown clayey mst 4 MD strongly oxidized with greyish patches 69 0.03 1.2 0.4 1.5

RB-09-254 007 39.00 Sl greyish cgl -1 MD bleached appearance…moderate to strong kaolinite alteration of fsp's…minor organic detritus 67 0.00 1.0 0.0 8.4

RB-09-254 008 44.00 RB Fm teal green slt -1 MD strongly reduced 69 0.03 0.4 0.0 8.0


RB-09-255 001 5.00 Mu brick red silty mst 4 MD strongly oxidized 79 0.04 0.7 0.0 1.4


RB-09-255 003 15.00 Mu greyish mg sst -1 MD minor greenish alteration…tr oxidized sulphides 70 0.02 0.7 0.0 10.5

RB-09-255 004 20.00 Mu tan-buff mg to cg sst 1 MD weak reddish-brown mottled hematite…moderate kaolinite alteration of fsp's 70 0.01 0.9 0.0 3.7

RB-09-255 005 25.00 Sst tan-buff cgl -1 MD greenish mst chips 78 0.00 0.4 0.0 3.5

RB-09-255 006 30.00 Ml reddish-brown silty mst 4 MD strongly oxidized with purplish-grey patches 68 0.03 0.5 0.0 5.9

RB-09-255 007 35.00 Ml greyish to reddish-brown silty mst 4 MD strongly oxidized with greyish patches 68 0.03 0.7 0.4 1.3

RB-09-255 008 40.00 Sl greyish mg sst -1 MD moderate kaolinite alteration…bleached appearance 72 0.00 0.2 1.6 1.0

RB-09-255 009 45.00 RB Fm teal green clayey mst -1 MD hosts calcite vein 70 0.04 0.7 1.0 1.3

RB-09-256 001 8.05 Su reddish-brown silty mst 4 MD strongly oxidized 74 0.03 0.5 0.0 10.3

RB-09-256 002 13.00 Su tan-buff to reddish-brown cg sst 2 MD weak mottled reddish-brown oxidation 72 0.00 0.4 1.0 1.1

RB-09-256 003 18.00 Mu reddish-brown cg sst 3 MD moderate reddish-brown pervasive hematite 70 0.03 1.0 0.4 1.4


RB-09-256 005 28.00 Mu reddish-brown silty mst 3 MD has a granular texture…minor greenish reduction as spots 71 0.03 0.1 0.1 7.8

Page 8 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-256 006 33.00 Mu tan-buff cg sst -1 - 1 MD weak reddish-brown hematite and minor spotty green reduction/alteration 76 0.00 0.3 1.4 0.0

RB-09-256 007 38.00 Mu greyish mg sst -1 MD very micaceous…abundant fg stratified organics 70 0.02 0.8 1.4 3.5

RB-09-256 008 43.00 Ml reddish-brown silty mst 4 MD strongly oxidized 79 0.06 1.0 0.0 3.8

RB-09-256 009 48.00 Ml reddish-brown mg sst -1 - 1 MD reddish-brown and greenish mst chips 73 0.02 0.4 0.8 0.1


RB-09-256 011 58.00 Sl greyish cgl -1 MD bleached appearance…moderate to strong kaolinite alteration of fsp's 71 0.00 0.8 0.0 5.9



RB-09-257 001 6.00 Su reddish cg sst 2 MD moderately strong reddish hematite as fg disseminations…weak kaolinite alteration of fsp's 69 0.00 1.3 0.0 6.1


RB-09-257 003 16.00 Mu reddish-brown fg sst 4 MD strongly oxidized 67 0.03 1.0 0.0 6.1


RB-09-257 005 26.00 Mu reddish-brown silty mst 4 MD very minor greenish reduction as wisps…broken and disaggregated 73 0.04 0.4 1.4 0.0

RB-09-257 006 31.00 Sst reddish-brown fg to mg sst 2 MD weak mottled hematite and stratified hematite 71 0.00 0.3 0.0 3.4

RB-09-257 007 36.00 Ml reddish-brown slt 4 MD strongly oxidized 76 0.03 0.9 0.0 10.6

RB-09-257 008 41.00 Ml reddish-brown to greenish silty mst -1 - 2 MD granular...interbedded sst 68 0.03 0.6 0.1 5.8

RB-09-257 009 46.00 Sl greenish cgl -1 MD moderate to strong pervasive greenish reduction 68 0.01 0.6 2.1 1.1


RB-09-258 001 6.00 Su reddish-brown cg sst 3 MD blotchy reddish-brown hematite disease 71 0.01 0.2 0.3 3.4

RB-09-258 002 11.00 Su reddish cg sst 4 MD locally strong reddish hematite 71 0.00 0.6 0.3 3.5

RB-09-258 003 16.00 Mu reddish-brown clayey mst 4 MD caliche-rich horizon (caliche fragments) 72 0.00 0.6 2.6 3.3


RB-09-258 005 26.00 Sst reddish-brown mg sst 2 MD stratified/pervasive hematite 72 0.01 0.6 0.0 5.8






RB-09-259 003 17.00 Sst tan-buff cg sst 0 MD moderate kaolinite alteration…fg diss organics 70 0.02 0.3 0.3 3.4

RB-09-259 004 22.00 Sst tan-buff to reddish-brown mg sst 0 - 4 MD stratified reddish-brown oxidation…fractured sub-parallel TCA 77 0.05 1.2 0.0 10.7

RB-09-259 005 27.00 Sst tan-buff cg sst 0 MD moderate kaolinite alteration…tr fg organics 80 0.01 0.4 1.0 1.2

RB-09-259 006 32.00 Sst tan-buff to reddish-brown cg sst 1 MD weak reddish-brown mottled hematite 73 0.00 0.7 0.3 3.6

RB-09-259 007 37.00 Sst reddish-brown mg sst 3 MD micaceous…weak to moderate pervasive reddish-brown hematite 70 0.01 1.0 0.0 1.5


RB-09-259 009 47.00 Ml greenish to reddish-brown clayey mst -1 - 2 MD both oxidized and reduced 70 0.01 0.2 0.0 5.8

RB-09-259 010 52.00 Ml reddish-brown slt 4 MD strongly oxidized 72 0.05 0.7 0.2 0.2

RB-09-259 011 57.00 Sl greenish cg sst -1 MD hosts teal green mst chip 71 0.01 0.9 0.0 3.7

Page 9 of 10


DDHNo.

SampleNo.

SampleDepth (m)

LITHOCode

SampleColour


OxidationScore

SampledBy

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-259 012 61.93 RB Fm charcoal grey shale -1 MD calcareous 71 0.00 1.0 0.8 3.6

RB-09-260 001 8.00 Su tan-buff cg sst 1 MD moderate kaolinite alteration…weak reddish-brown hematite alteration 69 0.00 0.4 0.0 5.8

RB-09-260 002 13.00 Mu brick red clayey mst 4 MD minor greenish alteration as spots 71 0.03 0.5 1.4 3.4

RB-09-260 003 18.00 Sst reddish clayey mst 4 MD strongly oxidized 74 0.05 0.5 0.2 5.7

RB-09-260 004 23.00 Sst reddish-brown mg sst 3 MD moderate pervasive/stratified hematite 75 0.00 0.9 0.0 8.3

RB-09-260 005 28.00 Ml reddish-brown clayey mst 4 MD minor greyish patches 70 0.03 0.5 1.9 0.0


RB-09-260 007 38.00 RB Fm teal green clayey mst -1 MD minor black-brown patches 70 0.04 0.5 0.7 5.7

RB-09-261 001 7.00 Su tan-buff cg to vcg sst 1 MD weak reddish-brown mottled hematite…minor beige clay alteration 70 0.00 0.9 0.0 5.9

RB-09-261 002 12.00 Su reddish-brown cg sst 1 - 4 MD strong reddish-brown hematite blotch…pink fsp's 78 0.03 1.1 0.2 3.7

RB-09-261 003 17.00 Mst reddish-brown mg sst 2 MD moderate reddish-brown pervasive/stratified hematite and minor blotchy greenish reduction 68 0.02 0.7 0.1 5.8

RB-09-261 004 22.00 Mst tan-buff to greenish mg sst -1 MD local greenish blotch…moderate kaolinite alteration of fsp's 70 0.00 0.8 1.0 1.3

RB-09-261 005 27.00 Mst reddish-brown fg sst 4 MD strongly oxidized 75 0.03 1.0 0.0 6.0

RB-09-261 006 32.00 Sst greenish to reddish-brown cg sst -1 - 2 MD moderate greenish reduction and reddish-brown oxidation 79 0.00 0.4 0.0 5.8

RB-09-261 007 37.00 Sst tan-buff mg sst -1 MDminor fg stratified organic detritus…bleached appearance…moderate to strong kaolinite


RB-09-261 008 42.00 Ml greenish clayey mst -1 MD reduced with moderate weak reddish-brown remnant oxidation 71 0.02 0.1 3.2 3.1

RB-09-261 009 47.00 Sl greenish mg sst -1 MD moderate greenish pervasive/stratified reduction…moderate kaolinite alteration 70 0.02 0.4 1.4 0.0

RB-09-262 001 8.00 OB/RB Fm reddish-brown clayey mst 3 MD puggy mst with fragments…possible overburden(?) 66 0.42 0.5 0.0 5.8

RB-09-262 002 13.00 RB Fm charcoal-grey to brownish slt to shale -1 MD fragments and cobbles 69 0.04 1.0 0.9 1.4

RB-09-262 003 18.00 RB Fm greenish slt -1 MD minor white mica 72 0.05 0.7 1.0 1.3

RB-09-263 001 8.00 OB/RB Fm greenish shale -1 MD very calcareous…abundant calcite veinlets (calcareous horizon) 72 42.60 0.8 0.0 3.6

RB-09-263 002 15.00 RB Fm charcoal grey slt -1 MD rounded rubble…vitreous fractures 80 0.02 1.0 0.0 8.4

Page 10 of 10

…A7

APPENDIX 7: 2009 DRILL CORE INTERVAL SAMPLING

Drill Core Interval Sampling; 2009 Drilling Campaign

DDHNo.

SampleFrom (m)

SampleTo (m)

SampleLength (m)

SampleNumber

LITHOCode

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-226 17.19 17.61 0.42 2920 Su Borehole anomaly with a peak/average of 150/90 CPS; 0.20m of core loss over interval 0.05 64 0.8 0.0 6.0RB-09-226 17.61 18.03 0.42 2921 Su Borehole anomaly with a peak/average of 150/70 CPS; 0.20m of core loss over interval 0.04 70 0.8 0.4 1.3RB-09-226 19.41 19.96 0.55 2922 Su Borehole anomaly with a peak/average of 95/60 CPS 0.04 65 0.4 1.4 3.4RB-09-226 19.96 20.51 0.55 2923 Su Borehole anomaly with a peak/average of 90/52 CPS 0.07 63 1.3 0.0 3.9RB-09-226 20.51 21.06 0.55 2924 Su Borehole anomaly with a peak/average of 142/77 CPS 0.04 57 1.0 0.7 5.9RB-09-226 21.06 21.61 0.55 2925 Su Borehole anomaly with a peak/average of 139/79 CPS 0.02 65 1.1 0.4 1.5

RB-09-227 11.88 12.23 0.35 2926 St Borehole anomaly with a peak/average of 142/72 CPS; 0.18m of core loss over interval 0.04 56 0.7 5.9 5.9RB-09-227 28.73 29.39 0.66 2927 St Borehole anomaly with a peak/average of 120/65 CPS 0.05 67 0.6 0.1 0.1RB-09-227 35.95 36.67 0.72 2928 Sm Borehole anomaly with a peak/average of 141/66 CPS; 0.06m of core loss over interval 0.04 68 0.90 8.40 8.40RB-09-227 42.75 43.21 0.46 2929 Sm Borehole anomaly with a peak/average of 94/59 CPS 0.03 65 0.8 1.3 1.3

RB-09-228 8.50 9.06 0.56 2930 Su Borehole anomaly with a peak/average of 109/66 CPS; 0.10m of core loss over interval 0.03 67 0.7 1.0 1.3RB-09-228 9.26 9.84 0.58 2931 Su Borehole anomaly with a peak/average of 93/57 CPS; 0.10m of core loss over interval 0.02 60 0.7 1.0 1.3RB-09-228 9.84 10.42 0.58 2932 Su Borehole anomaly with a peak/average of 90/60 CPS; 0.10m of core loss over interval 0.04 69 0.8 1.4 3.5RB-09-228 10.42 11.00 0.58 2933 Su Borehole anomaly with a peak/average of 104/67 CPS; 0.10m of core loss over interval 0.20 68 0.5 1.6 1.2RB-09-228 11.65 12.15 0.50 2934 Su Borehole anomaly with a peak/average of 84/56 CPS; 0.10m of core loss over interval 0.08 65 0.6 2.7 1.1RB-09-228 12.15 12.65 0.50 2935 Su Borehole anomaly with a peak/average of 103/67 CPS 0.08 66 0.8 0.0 1.4RB-09-228 12.65 13.15 0.50 2936 Su Borehole anomaly with a peak/average of 117/74 CPS 0.06 64 0.8 2.7 1.2RB-09-228 13.15 13.65 0.50 2937 Su Borehole anomaly with a peak/average of 123/93 CPS 0.07 68 0.6 0.0 5.8RB-09-228 13.65 14.15 0.50 2938 Su Borehole anomaly with a peak/average of 143/69 CPS 0.13 67 0.8 2.5 0.1RB-09-228 14.15 14.65 0.50 2939 Mu Borehole anomaly with a peak/average of 94/57 CPS 0.03 64 0.5 1.0 1.2RB-09-228 14.65 15.15 0.50 2940 Mu Borehole anomaly with a peak/average of 95/57 CPS 0.13 72 1.1 0.0 6.0RB-09-228 15.15 15.65 0.50 2941 Mu Borehole anomaly with a peak/average of 81/60 CPS 0.15 68 0.9 0.0 3.7RB-09-228 15.65 16.15 0.50 2942 Mu Borehole anomaly with a peak/average of 98/63 CPS 0.12 64 0.5 3.8 1.0

RB-09-229 6.74 7.35 0.61 2943 Su Borehole anomaly with a peak/average of 194/79 CPS 0.03 63 0.1 2.5 0.0RB-09-229 7.35 7.95 0.60 2944 Su Borehole anomaly with a peak/average of 232/109 CPS 0.02 65 0.3 0.0 0.0RB-09-229 8.47 9.01 0.54 2945 Su Borehole anomaly with a peak/average of 210/115 CPS 0.04 75 0.6 1.3 5.7RB-09-229 9.01 9.55 0.54 2946 Su Borehole anomaly with a peak/average of 462/140 CPS; 0.08m of core loss over interval 0.02 60 0.7 2.1 1.2RB-09-229 9.55 10.09 0.54 2947 Su Borehole anomaly with a peak/average of 788/430 CPS; 0.08m of core loss over interval 0.02 68 1.1 0.2 3.7RB-09-229 10.96 11.70 0.74 2948 Su Borehole anomaly with a peak/average of 120/63 CPS; 0.08m of core loss over interval 0.08 122 1.1 7.6 3.1RB-09-229 14.34 14.80 0.46 2949 Mu Borehole anomaly with a peak/average of 110/65 CPS; 0.18m of core loss over interval 0.13 64 0.8 0.4 1.3RB-09-229 14.80 15.26 0.46 2950 Mu Borehole anomaly with a peak/average of 219/121 CPS; 0.18m of core loss over interval 0.12 65 1.1 0.0 3.8RB-09-229 15.26 15.72 0.46 2951 Mu Borehole anomaly with a peak/average of 158/107 CPS; 0.10m of core loss over interval 0.17 66 0.3 0.0 1.2RB-09-229 15.72 16.18 0.46 2952 Mu Borehole anomaly with a peak/average of 115/69 CPS; 0.10m of core loss over interval 0.11 76 0.6 3.3 9.9RB-09-229 16.18 16.65 0.47 2953 Mu Borehole anomaly with a peak/average of 96/53 CPS; 0.10m of core loss over interval 0.10 74 0.6 0.0 8.0RB-09-229 39.53 40.03 0.50 2954 Mu Borehole anomaly with a peak/average of 119/68 CPS; 0.07m of core loss over interval 0.02 62 1.3 0.0 1.6RB-09-229 40.36 40.98 0.62 2955 Mu Borehole anomaly with a peak/average of 119/70 CPS; 0.07m of core loss over interval 0.01 65 1.1 0.8 3.7RB-09-229 42.85 43.32 0.47 2956 Mu Borehole anomaly with a peak/average of 128/72 CPS 0.03 69 0.4 1.4 0.0RB-09-229 46.53 47.02 0.49 2957 Sm Borehole anomaly with a peak/average of 106/64 CPS 0.03 79 1.0 1.2 5.8

RB-09-230 36.19 36.72 0.53 2958 Sm Borehole anomaly with a peak/average of 88/62 CPS 0.02 68 0.6 0.0 1.3RB-09-230 36.72 37.25 0.53 2959 Sm Borehole anomaly with a peak/average of 101/62 CPS 0.03 66 0.5 0.0 10.5RB-09-230 37.25 37.78 0.53 2960 Sm Borehole anomaly with a peak/average of 89/57 CPS 0.03 67 1.4 1.5 1.5

RB-09-231 10.88 11.32 0.44 2961 Su Borehole anomaly with a peak/average of 113/61 CPS; 0.10m of core loss over interval 0.02 63 0.6 1.0 1.2RB-09-231 11.32 11.75 0.43 2962 Su Borehole anomaly with a peak/average of 95/58 CPS; 0.10m of core loss over interval 0.02 70 0.0 0.0 3.3RB-09-231 13.78 14.34 0.56 2963 Su Borehole anomaly with a peak/average of 88/59 CPS; 0.10m of core loss from 11.00 - 14.00m, 0.70m of core loss from 14.00 - 17.00m 0.03 73 1.1 1.5 1.4RB-09-231 14.34 14.90 0.56 2964 Su Borehole anomaly with a peak/average of 115/66 CPS; 0.70m of core loss from 14.00 - 17.00m 0.03 66 1.1 0.0 8.3RB-09-231 14.90 15.47 0.57 2965 Su Borehole anomaly with a peak/average of 84/58 CPS; 0.70m of core loss from 14.00 - 17.00m 0.04 76 0.6 0.1 5.8

RB-09-232 38.82 39.36 0.54 2966 Mu Borehole anomaly with a peak/average of 102/57 CPS 0.18 68 0.6 0.8 0.2RB-09-232 39.36 39.90 0.54 2967 Mu Borehole anomaly with a peak/average of 161/90 CPS 0.20 73 0.8 0.0 6.0RB-09-232 39.90 40.44 0.54 2968 Mu Borehole anomaly with a peak/average of 151/104 CPS 0.22 58 0.7 0.0 1.4RB-09-232 40.44 40.98 0.54 2969 Mu Borehole anomaly with a peak/average of 152/86 CPS 0.16 67 1.3 0.0 3.9RB-09-232 40.98 41.52 0.54 2970 Mu Borehole anomaly with a peak/average of 124/73 CPS 0.16 71 0.7 0.0 8.1RB-09-232 41.52 42.04 0.52 2971 Mu Borehole anomaly with a peak/average of 127/77 CPS 0.11 67 0.2 1.5 3.3RB-09-232 42.04 42.52 0.48 2972 St Borehole anomaly with a peak/average of 202/120 CPS 0.02 74 0.6 1.1 7.9RB-09-232 42.52 43.00 0.48 2973 St Borehole anomaly with a peak/average of 151/101 CPS 0.03 72 0.8 1.0 10.3RB-09-232 43.00 43.48 0.48 2974 St Borehole anomaly with a peak/average of 148/97 CPS 0.04 70 0.7 1.6 1.2RB-09-232 43.48 43.96 0.48 2975 St Borehole anomaly with a peak/average of 199/130 CPS 0.04 65 0.8 0.0 6.0RB-09-232 43.96 44.44 0.48 2976 St Borehole anomaly with a peak/average of 103/72 CPS 0.02 74 0.4 1.6 1.1RB-09-232 44.44 44.89 0.45 2977 St Borehole anomaly with a peak/average of 114/78 CPS 0.04 72 0.0 2.3 7.6RB-09-232 46.93 47.52 0.59 2978 St Borehole anomaly with a peak/average of 126/65 CPS; 0.15m of core loss over interval 0.03 58 0.9 1.0 1.3RB-09-232 60.50 60.94 0.44 2979 St Borehole anomaly with a peak/average of 137/78 CPS; 1.20m of core loss over interval 0.02 62 0.5 0.2 0.2RB-09-232 64.62 65.18 0.56 2984 St Borehole anomaly with a peak/average of 151/63 CPS; 0.10m of core loss over interval 0.01 71 0.4 0.5 1.2RB-09-232 65.18 65.74 0.56 2985 St Borehole anomaly with a peak/average of 112/75 CPS; 0.10m of core loss over interval 0.01 68 0.7 0.0 1.4RB-09-232 65.74 66.30 0.56 2986 St Borehole anomaly with a peak/average of 105/70 CPS; 0.10m of core loss from 63.00 - 66.00m; 0.20m of core loss from 66.00 - 69.00m 0.01 68 0.7 0.0 3.7RB-09-232 66.30 66.86 0.56 2987 St Borehole anomaly with a peak/average of 125/80 CPS; 0.20m of core loss over interval 0.00 66 0.5 2.5 0.0RB-09-232 66.86 67.42 0.56 2988 St Borehole anomaly with a peak/average of 139/77 CPS; 0.20m of core loss over interval 0.02 71 0.5 1.6 1.1RB-09-232 68.05 68.82 0.77 2989 St Borehole anomaly with a peak/average of 100/61 CPS; 0.20m of core loss over interval 0.01 66 0.6 0.0 8.0RB-09-232 69.25 69.74 0.49 2990 Mm Borehole anomaly with a peak/average of 122/72 CPS; 0.20m of core loss over interval 0.06 68 1.3 0.0 3.8

Page 1 of 2

Drill Core Interval Sampling; 2009 Drilling Campaign

DDHNo.

SampleFrom (m)

SampleTo (m)

SampleLength (m)

SampleNumber

LITHOCode

SampleComments



SpectrometerK_%

SpectrometerU_ppm

SpectrometerTh_ppm

RB-09-232 70.77 71.24 0.47 2991 Sm Borehole anomaly with a peak/average of 98/62 CPS 0.01 64 0.8 2.5 0.1RB-09-232 71.24 71.71 0.47 2992 Sm Borehole anomaly with a peak/average of 92/66 CPS 0.03 74 0.8 0.0 0.3RB-09-232 71.71 72.18 0.47 2993 Sm Borehole anomaly with a peak/average of 102/60 CPS 0.05 72 0.8 1.8 5.7

RB-09-234 15.35 15.90 0.55 2994 Su Borehole anomaly with a peak/average of 108/68 CPS; 0.15m of core loss over interval 0.01 68 1.1 0.0 3.7RB-09-234 15.90 16.44 0.54 2995 Su Borehole anomaly with a peak/average of 108/58 CPS; 0.15m of core loss over interval 0.02 71 0.4 0.0 8.0

RB-09-241 16.85 17.40 0.55 2997 Mu Borehole anomaly with a peak/average of 96/58 CPS 0.06 71 0.2 2.2 1.0RB-09-241 17.40 17.95 0.55 2998 Mu Borehole anomaly with a peak/average of 133/86 CPS 0.06 69 1.1 1.9 0.3RB-09-241 17.95 18.50 0.55 2999 Mu Borehole anomaly with a peak/average of 130/80 CPS 0.03 67 0.6 0.6 7.9RB-09-241 18.50 19.06 0.56 3000 Mu Borehole anomaly with a peak/average of 159/84 CPS 0.03 68 0.4 2.5 0.0RB-09-241 50.52 50.66 0.14 2996 St Organic trash fragment with abundant pyrite and trace chalcopyrite 0.00 63 0.1 0.0 8.0

RB-09-242 9.91 10.39 0.48 3901 Su Borehole anomaly with a peak/average of 115/65 CPS 0.00 71 1.0 2.1 1.3RB-09-242 10.39 10.87 0.48 3902 Su Borehole anomaly with a peak/average of 94/66 CPS 0.01 65 0.9 0.0 8.2RB-09-242 10.87 11.35 0.48 3903 Su Borehole anomaly with a peak/average of 92/53 CPS 0.00 65 0.7 0.3 3.6RB-09-242 11.35 11.83 0.48 3904 Su Borehole anomaly with a peak/average of 97/62 CPS 0.00 74 0.6 1.3 0.1RB-09-242 11.83 12.30 0.47 3905 Su Borehole anomaly with a peak/average of 122/67 CPS 0.00 69 1.0 2.7 1.2RB-09-242 15.99 16.51 0.52 3906 Mu Borehole anomaly with a peak/average of 100/66 CPS 0.11 72 0.0 1.2 7.7RB-09-242 16.51 17.03 0.52 3907 Mu Borehole anomaly with a peak/average of 130/70 CPS 0.10 70 0.5 0.0 12.5RB-09-242 17.03 17.55 0.52 3908 Mu Borehole anomaly with a peak/average of 119/73 CPS 0.08 68 1.1 0.0 3.8RB-09-242 17.55 18.08 0.53 3909 Mu Borehole anomaly with a peak/average of 158/95 CPS; 0.05m of core loss over interval 0.14 73 0.8 1.0 1.3RB-09-242 18.08 18.60 0.52 3910 Mu Borehole anomaly with a peak/average of 157/68 CPS; 0.05m of core loss over interval 0.09 74 0.8 0.0 5.9

RB-09-243 6.25 6.71 0.46 3911 Su Borehole anomaly with a peak/average of 326/143 CPS; 0.20m of core loss over interval 0.05 74 1.1 0.2 3.7RB-09-243 9.46 9.94 0.48 3912 Mu Borehole anomaly with a peak/average of 108/64 CPS 0.12 74 0.6 1.0 1.2RB-09-243 9.94 10.42 0.48 3913 Mu Borehole anomaly with a peak/average of 148/70 CPS 0.04 79 0.7 1.1 8.0RB-09-243 10.42 10.90 0.48 3914 Mu Borehole anomaly with a peak/average of 269/109 CPS 0.07 77 1.1 0.0 8.3RB-09-243 10.90 11.40 0.50 3915 Mu Borehole anomaly with a peak/average of 348/166 CPS 0.07 84 0.3 4.2 0.0RB-09-243 14.88 15.40 0.52 3916 Mu Borehole anomaly with a peak/average of 106/60 CPS 0.09 74 0.4 2.6 3.3RB-09-243 15.40 15.92 0.52 3917 Mu Borehole anomaly with a peak/average of 124/72 CPS 0.16 79 0.9 0.0 10.5RB-09-243 15.92 16.44 0.52 3918 Mu Borehole anomaly with a peak/average of 133/86 CPS 0.15 75 1.1 0.0 6.0RB-09-243 16.44 16.96 0.52 3919 Mu Borehole anomaly with a peak/average of 113/70 CPS 0.11 85 0.6 2.0 3.4

RB-09-245 43.32 43.87 0.55 3920 Sm Borehole anomaly with a peak/average of 153/97 CPS 0.02 80 1.1 2.5 3.5RB-09-245 43.87 44.41 0.54 3921 Sm Borehole anomaly with a peak/average of 166/70 CPS 0.04 80 1.0 1.0 1.4RB-09-245 65.86 66.48 0.62 3922 Sm Borehole anomaly with a peak/average of 112/71 CPS; 0.14m of core loss over interval 0.03 78 0.7 0.3 3.6RB-09-245 66.48 67.11 0.63 3923 Sm Borehole anomaly with a peak/average of 115/68 CPS; 0.14m of core loss over interval 0.04 72 0.6 2.0 3.4RB-09-245 67.11 67.61 0.50 3924 Ml Borehole anomaly with a peak/average of 107/66 CPS; 0.14m of core loss over interval 0.07 76 1.1 0.8 3.7RB-09-245 67.61 68.11 0.50 3925 Ml Borehole anomaly with a peak/average of 87/61 CPS; 0.14m of core loss over interval 0.10 78 0.2 0.3 3.4RB-09-245 68.11 68.61 0.50 3926 Ml Borehole anomaly with a peak/average of 94/62 CPS 0.10 82 1.5 0.0 8.4RB-09-245 68.61 69.11 0.50 3927 Ml Borehole anomaly with a peak/average of 107/64 CPS 0.11 79 1.1 0.0 6.0RB-09-245 69.11 69.61 0.50 3928 Ml Borehole anomaly with a peak/average of 111/68 CPS 0.10 75 0.6 0.8 0.2RB-09-245 69.61 70.11 0.50 3929 Ml Borehole anomaly with a peak/average of 109/74 CPS 0.14 83 1.0 0.0 8.4RB-09-245 70.11 70.61 0.50 3930 Ml Borehole anomaly with a peak/average of 140/80 CPS 0.09 77 0.9 2.0 3.5RB-09-245 70.61 71.11 0.50 3931 Ml Borehole anomaly with a peak/average of 124/72 CPS 0.15 74 0.7 0.7 5.8

RB-09-246 7.74 8.29 0.55 2980 Su Borehole anomaly with a peak/average of 117/66 CPS 0.02 67 0.7 1.0 1.3RB-09-246 39.58 40.11 0.53 2981 HF Sst Borehole anomaly with a peak/average of 102/60 CPS 0.05 84 1.0 1.3 0.3RB-09-246 40.11 40.64 0.53 2982 HF Sst Borehole anomaly with a peak/average of 86/61 CPS 0.02 66 0.8 0.3 3.6RB-09-246 40.99 41.45 0.46 2983 HF Sst Borehole anomaly with a peak/average of 112/64 CPS 0.01 65 0.9 0.0 1.4RB-09-247 6.04 6.59 0.55 3932 Su Borehole anomaly with a peak/average of 104/60 CPS; 0.17m of core loss over interval 0.04 71 1.2 0.0 3.9RB-09-248 29.95 30.42 0.47 3933 Mu Borehole anomaly with a peak/average of 180/96 CPS; 0.15 85 0.0 1.3 5.4

RB-09-251 7.25 7.76 0.51 3934 Su Borehole anomaly with a peak/average of 193/82 CPS 0.01 68 0.8 0.7 5.8RB-09-251 7.76 8.27 0.51 3935 Su Borehole anomaly with a peak/average of 236/184 CPS; 1.60m of core loss over interval 0.03 56 0.3 3.9 0.9RB-09-251 8.27 8.78 0.51 3936 Su Borehole anomaly with a peak/average of 287/166 CPS; 1.60m of core loss over interval 0.01 73 1.3 0.0 6.3RB-09-251 52.68 53.42 0.74 3937 HF Sst Borehole anomaly with a peak/average of 140/77 CPS 0.13 67 0.8 2.1 1.2RB-09-252 8.13 8.84 0.71 3938 Su Borehole anomaly with a peak/average of 132/81CPS 0.01 69 0.8 0.4 1.4

RB-09-253 25.93 26.83 0.90 3939 HF Mst Borehole anomaly with a peak/average of 412/181 CPS 0.22 62 1.6 0.8 3.9RB-09-253 26.83 27.43 0.60 3940 Hf Mst Borehole anomaly with a peak/average of 336/133 CPS 0.14 67 0.3 3.2 3.2RB-09-255 41.23 41.81 0.58 3941 Sl Borehole anomaly with a peak/average of 117/64 CPS 0.01 56 0.9 0.0 6.1

RB-09-256 36.34 36.96 0.62 3942 Mu Borehole anomaly with a peak/average of 622/260 CPS 0.04 65 0.4 1.9 0.0RB-09-256 36.96 37.38 0.42 3943 Mu Borehole anomaly with a peak/average of 656/252 CPS 0.02 66 0.1 4.2 0.0RB-09-256 38.00 38.50 0.50 3944 Mu Borehole anomaly with a peak/average of 67/34 CPS; Anomalous Hm in St-like sst 0.06 129 1.8 4.7 3.6

RB-09-258 5.40 5.90 0.50 3945 Su Borehole anomaly with a peak/average of 124/78 CPS 0.05 63 0.6 0.1 5.8RB-09-258 5.90 6.40 0.50 3946 Su Borehole anomaly with a peak/average of 90/57 CPS; 1.67m of core loss over interval 0.03 68 0.0 1.9 5.4RB-09-258 6.40 6.91 0.51 3947 Su Borehole anomaly with a peak/average of 101/59 CPS; 1.67m of core loss over interval 0.03 83 0.3 0.2 5.7

RB-09-259 33.21 33.82 0.61 3949 HF Sst Borehole anomaly with a peak/average of 99/61CPS 0.06 74 0.0 1.8 7.6RB-09-259 40.43 40.92 0.49 3950 HF Sst Borehole anomaly with a peak/average of 104/68 CPS 0.03 64 0.3 2.2 1.0RB-09-261 6.57 7.10 0.53 3948 Su Borehole anomaly with a peak/average of 128/71 CPS 0.02 68 0.4 1.3 5.6

Page 2 of 2

…A8

APPENDIX 8: 2009 LABORATORY ASSAY CERTIFICATES

SRC Geoanalytical Laboratories125 - 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8

Tel: (306) 933-8118 Fax: (306) 933-5656 Email: [email protected]

ICP1 Total Digestion

Altius Resources Inc.Attention: Andrea Devereaux

Samples: 126PO #/Project: Rocky Brook

Report No: G-09-1879

Date of Report: January 14, 2010

Column Header Details

Silver in ppm (Ag) Aluminum in wt % (Al2O3) Barium in ppm (Ba) Berylium in ppm (Be) Calcium in wt % (CaO)

Cadmium in ppm (Cd) Cerium in ppm (Ce) Cobalt in ppm (Co) Chromium in ppm (Cr) Copper in ppm (Cu)

Dysprnnosium in ppm (Dy) Erbium in ppm (Er) Europium in ppm (Eu) Iron in wt % (Fe2O3) Gallium in ppm (Ga)

Gadolinium in ppm (Gd) Hafnium in ppm (Hf) Holmium in ppm (Ho) Potassium in wt % (K2O) Lanthanum in ppm (La)

Lithium in ppm (Li) Magnesium in wt % (MgO) Manganese in wt % (MnO) Molybdenum in ppm (Mo) Sodium in wt % (Na2O)

Niobium in ppm (Nb) Neodymium in ppm (Nd) Nickel in ppm (Ni) Phosphorus in wt % (P2O5) Lead in ppm (Pb)

Praseodymium in ppm (Pr) Scandium in ppm (Sc) Samarium in ppm (Sm) Tin in ppm (Sn) Strontium in ppm (Sr)

Tantalum in ppm (Ta) Terbium in ppm (Tb) Thorium in ppm (Th) Titanium in wt % (TiO2) Uranium in ppm (U, ICP)

1Page of 14









Vanadium in ppm (V) Tungsten in ppm (W) Yttrium in ppm (Y) Ytterbium in ppm (Yb) Zinc in ppm (Zn)

Zirconium in ppm (Zr)

2Page of 14








HfGdGaFe2O3EuErDyCuCrCoCeCdCaOBeBaAl2O3AgSampleppmppmppmwt %ppmppmppmppmppmppmppmppmwt %ppmppmwt %ppmNumber

0.61.110.53<0.2<0.20.34466<113<0.20.01<0.2190.52<0.2ASR1093.21.661.340.41.11.24145320.41.940.44365.780.8RB-09-251-0014.68.6267.542.35.15.94564191301.21.052.961017.213.7RB-09-251-0024.89.8257.142.54.45.9663201431.02.752.7143016.8<0.2RB-09-251-0033.612.9309.603.46.68.12161181951.20.763.051218.8<0.2RB-09-251-004

4.68.8289.492.54.85.5557181501.10.712.949717.2<0.2RB-09-251-0055.316.5256.854.76.18.31362153071.10.572.547716.4<0.2RB-09-251-0064.16.0297.511.84.44.876720841.20.513.849118.8<0.2RB-09-251-0074.35.0247.981.62.93.248820861.00.423.155316.3<0.2RB-09-251-0081.11.260.770.40.60.81173230.50.400.62827.70<0.2RB-09-251-009

3.21.650.560.51.21.212142380.50.620.42747.12<0.2RB-09-251-0104.010.8227.733.06.37.61985111361.10.462.448915.7<0.2RB-09-251-0113.03.1132.671.01.92.0111512550.60.310.84539.98<0.2RB-09-251-0126.33.382.260.83.12.624205600.30.180.710705.72<0.2RB-09-251-0130.64.611.771.01.15.96412532.049.10.51563.40<0.2RB-09-251-014

1.11.140.830.40.71.326179180.41.710.33225.450.4RB-09-252-0013.78.1278.982.44.85.63364161371.13.873.241616.7<0.2RB-09-252-0024.66.8309.032.04.85.176318881.20.862.855517.8<0.2RB-09-252-0034.04.0100.531.11.82.543205680.70.580.729509.29<0.2RB-09-252-0042.11.851.560.61.32.86116230.74.880.49726.91<0.2RB-09-252-005

6.22.430.830.41.31.74422147<0.20.020.2192.43<0.2ASR2092.71.831.330.51.51.536133430.40.860.44964.88<0.2RB-09-252-0063.18.0289.482.64.45.11369251301.10.492.751917.9<0.2RB-09-252-0078.13.8196.321.23.23.1436811570.80.352.335313.8<0.2RB-09-252-0083.05.3226.591.53.64.11810920481.26.212.824717.1<0.2RB-09-252-009

5.34.193.421.13.24.0193228650.78.670.8366010.2<0.2RB-09-252-0101.83.851.861.02.15.219127470.88.300.56747.92<0.2RB-09-253-0012.41.992.420.61.31.6201515370.40.790.52867.90<0.2RB-09-253-002

19.17.181.591.84.44.4362891490.60.750.856610.1<0.2RB-09-253-0033.87.2288.082.14.85.21470201051.30.663.540218.6<0.2RB-09-253-004

2.25.6309.331.83.84.2912826831.20.464.138520.6<0.2RB-09-253-0053.65.9289.381.84.34.5137620801.00.623.545017.3<0.2RB-09-253-0065.86.6183.121.93.23.74873111220.91.261.839313.3<0.2RB-09-253-0074.22.061.020.51.41.33104420.40.320.45056.23<0.2RB-09-253-0081.74.3215.591.22.83.21912216511.44.672.548316.0<0.2RB-09-253-009

4.26.4225.111.83.94.33646181041.01.481.858514.5<0.2RB-09-254-0015.08.9266.972.45.26.2567181151.20.592.643617.2<0.2RB-09-254-0023.49.63210.42.85.76.4678221381.30.453.447319.5<0.2RB-09-254-0031.93.080.950.81.41.74335680.40.320.63977.43<0.2RB-09-254-0041.74.2225.751.22.83.21912217511.34.682.549716.1<0.2RB-09-253-009 R

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0.71.210.54<0.20.20.34483<114<0.20.03<0.2180.50<0.2ASR1094.65.1192.421.43.03.2126717950.80.431.650612.9<0.2RB-09-254-0055.66.9185.581.55.76.686814580.80.562.239613.1<0.2RB-09-254-0061.91.430.300.40.81.15181250.20.580.22723.94<0.2RB-09-254-0071.64.0195.021.12.24.2538523433.017.82.580714.1<0.2RB-09-254-008

1.84.0185.411.12.72.94712917460.98.142.183413.6<0.2RB-09-254-0094.913.8299.933.48.610.2858161941.10.723.472616.4<0.2RB-09-255-0016.75.5236.671.64.24.2106115891.01.521.686115.6<0.2RB-09-255-0026.23.161.010.82.92.213224620.50.640.45398.00<0.2RB-09-255-0032.72.740.860.81.42.43263320.32.250.33655.38<0.2RB-09-255-004

1.41.650.580.50.91.02143340.30.790.43055.07<0.2RB-09-255-0054.75.7226.941.73.84.257713861.00.463.145815.0<0.2RB-09-255-0065.86.7155.261.84.24.85668890.70.531.643910.6<0.2RB-09-255-0073.01.950.720.51.71.741103360.41.660.43696.17<0.2RB-09-255-0081.75.2205.961.53.04.0358618631.011.42.296314.9<0.2RB-09-255-009

3.016.03812.54.011.513.5878222141.40.513.649321.4<0.2RB-09-256-0012.05.270.821.42.33.329134940.62.500.740008.74<0.2RB-09-256-0022.21.760.460.51.01.64082300.51.980.312007.45<0.2RB-09-256-0032.57.23811.42.35.45.6575221071.30.423.358322.30.2RB-09-256-0046.26.7214.631.95.55.8175014960.90.372.059214.9<0.2RB-09-256-005

6.12.430.860.41.21.64431149<0.20.020.3202.48<0.2ASR2091.41.981.080.61.01.42144310.50.520.64717.93<0.2RB-09-256-0061.62.6192.500.91.51.71179416510.90.391.737813.61.1RB-09-256-0075.85.0216.131.53.63.847714860.90.502.746114.5<0.2RB-09-256-0083.02.461.510.71.51.94356440.41.620.613006.80<0.2RB-09-256-009

3.29.33310.52.65.96.77470181161.40.603.778419.3<0.2RB-09-256-0102.61.440.680.41.01.25153250.32.250.33554.72<0.2RB-09-256-0111.75.0276.951.53.33.5399820711.35.272.8142018.50.3RB-09-256-0121.63.1145.011.02.42.5258213440.86.631.580911.3<0.2RB-09-256-0131.41.230.640.40.71.5272180.33.930.33245.07<0.2RB-09-257-001

5.19.7258.102.75.46.3859191591.01.252.655816.2<0.2RB-09-257-0023.79.2279.012.85.05.61348141601.10.532.467316.8<0.2RB-09-257-0033.28.1318.732.54.85.31466201421.20.702.848518.8<0.2RB-09-257-0045.04.5256.951.54.03.9236717701.10.472.555316.3<0.2RB-09-257-0051.42.891.480.91.41.86306440.60.431.02979.87<0.2RB-09-257-006

4.56.9288.062.14.75.067520981.20.493.045518.1<0.2RB-09-257-0073.23.4134.481.22.12.3124924670.40.451.63019.28<0.2RB-09-257-0082.23.2112.661.11.82.018228700.50.180.83807.75<0.2RB-09-257-0091.74.1215.411.32.93.13411733551.15.402.274116.70.3RB-09-257-0104.16.7277.722.04.64.967419951.00.572.944717.7<0.2RB-09-257-007 R

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0.81.210.560.20.20.45498115<0.20.01<0.2190.51<0.2ASR1093.52.960.710.71.52.559268550.53.180.65536.98<0.2RB-09-258-0011.81.851.110.61.02.55105290.45.470.44456.530.2RB-09-258-0021.49.922.402.04.89.9<1228522.036.10.41305.61<0.2RB-09-258-0033.08.7288.912.64.26.41064191251.23.302.755717.3<0.2RB-09-258-004

3.42.2101.220.71.11.627184490.70.580.654510.2<0.2RB-09-258-0056.75.8257.101.83.54.365313991.10.491.868116.2<0.2RB-09-258-0063.78.9308.892.65.36.8581171111.20.693.535318.5<0.2RB-09-258-0075.44.4275.651.42.33.0109322751.00.402.743516.5<0.2RB-09-258-0085.26.9267.651.94.05.676018881.01.462.487016.40.3RB-09-259-001

3.89.9379.393.05.77.6580221671.40.463.261921.5<0.2RB-09-259-0022.72.150.730.61.21.923153480.52.720.47277.00<0.2RB-09-259-0035.63.31212.01.31.41.845183670.40.360.84447.550.3RB-09-259-0042.21.750.540.60.81.516101270.41.960.44845.90<0.2RB-09-259-0051.31.660.280.60.61.1152101290.60.700.45437.08<0.2RB-09-259-006

2.22.6131.650.91.01.623010620.70.401.038511.20.3RB-09-259-0075.47.3237.792.03.85.1377815961.10.483.248315.1<0.2RB-09-259-0086.06.3184.321.83.24.37285131020.80.482.042613.61.4RB-09-259-0093.211.63411.83.26.48.814771191731.40.393.572020.5<0.2RB-09-259-0102.92.2112.230.71.11.61022111480.40.120.74186.56<0.2RB-09-259-011

6.32.530.850.41.01.75444<147<0.20.020.3182.50<0.2ASR2091.17.6134.401.62.74.9566913781.023.80.9120010.4<0.2RB-09-259-0121.81.770.260.60.61.32182360.51.700.416607.36<0.2RB-09-260-0014.07.4288.082.13.65.2674161051.30.503.247818.8<0.2RB-09-260-0024.511.5348.683.35.47.61179331781.30.333.862820.2<0.2RB-09-260-003

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3.92.670.370.71.01.712172560.70.540.55949.18<0.2RB-09-261-0073.87.5235.542.03.04.531784131151.11.402.447916.4<0.2RB-09-261-0082.31.781.810.60.81.21811510350.70.650.54689.14<0.2RB-09-261-0093.24.4154.361.12.13.42512621710.94.150.932213.6<0.2RB-09-262-0013.67.6225.492.13.04.632084131161.21.452.447716.6<0.2RB-09-261-008 R

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0.81.210.54<0.20.20.35487<114<0.20.02<0.2200.52<0.2ASR1091.93.7205.871.22.12.4579218541.03.681.734213.50.3RB-09-262-0022.74.8277.381.52.83.4349919591.23.142.637118.0<0.2RB-09-262-0031.02.01816.41.11.11.563866110.910.1<0.211814.40.7RB-09-263-0011.84.8124.701.42.43.824688550.612.21.43968.78<0.2RB-09-263-002

1.75.3134.861.52.74.122727580.813.31.440710.2<0.2RB-09-263-002 R

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SnSmScPrPbP2O5NiNdNbNa2OMoMnOMgOLiLaK2OHoSampleppmppmppmppmppmwt %ppmppmppmwt %ppmwt %wt %ppmppmwt %ppmNumber

<11.0<1120.013124<1<0.0130.0040.031950.041<0.4ASR109<12.013220.028141191.23<10.0600.2256152.190.4RB-09-251-001

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1012.72021170.162428250.60<10.0401.80511023.602.3RB-09-251-004

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11.0<1120.014124<1<0.0130.0040.030960.044<0.4ASR10915.2139100.057293490.27<10.0171.1439442.441.0RB-09-254-00563.7134120.060332280.24<10.0161.3640271.851.9RB-09-254-006

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15.1154140.1341102030.76<10.0738.2179243.130.8RB-09-254-0091112.21819230.157247541.01<10.0361.5440903.632.9RB-09-255-00155.2148180.1143534161.38<10.0351.9847453.771.4RB-09-255-002

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<11.2<1130.016145<10.0130.0040.0301060.042<0.4ASR109<13.735100.034920111.67<10.1240.38510262.500.7RB-09-258-001<12.92370.03551151.59<10.2922.214162.340.4RB-09-258-002<114.661220.04264051.9510.5643.309480.6932.0RB-09-258-003

89.61912170.142375560.87<10.1372.4054653.191.8RB-09-258-004

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58.31810150.142374760.31<10.0382.2131513.211.4RB-09-261-008 R

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<11.2<1130.012135<1<0.0130.0040.029960.044<0.4ASR10934.1125210.1667622111.27190.0488.0098282.870.6RB-09-262-00265.0165130.1858327101.79<10.0447.1886324.571.0RB-09-262-003

111.461<1160.09675111.10<10.1797.82810.476<0.4RB-09-263-001<17.310780.130422751.0010.1427.1956332.110.8RB-09-263-002

<17.812790.134442941.10<10.1488.5060352.201.0RB-09-263-002 R

10Page of 14








ZrZnYbYWVU, ICPTiO2ThTbTaSrSampleppmppmppmppmppmppmppmwt %ppmppmppmppmNumber

4010.32<14<20.0311<0.3<138ASR10912380.87<15340.8637<0.3<170RB-09-251-001188774.3412013141.0513<0.3<1160RB-09-251-002189833.334<195<20.98417<0.3<1238RB-09-251-003157685.356<1110<21.03150.6<1210RB-09-251-004

185574.138<112021.0813<0.3<1176RB-09-251-005212434.450<190<21.13121.0<1201RB-09-251-006169603.834<112431.2213<0.3<1182RB-09-251-007177792.422<111130.92313<0.3<1167RB-09-251-00844150.64<129<20.1533<0.3<183RB-09-251-009

127110.97<130<20.7025<0.3<197RB-09-251-010158445.261<197<20.864110.6<1383RB-09-251-011121451.413<142<20.8677<0.3<1126RB-09-251-012258222.116<18231.9714<0.31146RB-09-251-013154491.022<127<20.12641.52477RB-09-251-014

38140.76<12120.0862<0.3<163RB-09-252-001150773.836<1124<20.97414<0.3<1218RB-09-252-002190704.237<114521.0913<0.3<1239RB-09-252-003157271.414<134<20.5247<0.3<1167RB-09-252-00476241.09<143<20.3964<0.3<1131RB-09-252-005

25721.312<11530.22427<0.3<1165ASR209101110.97<131<21.2612<0.3178RB-09-252-006135873.734<111021.0111<0.3<1198RB-09-252-007320413.023<19321.1712<0.3<1355RB-09-252-008124613.229<112020.79011<0.3<1960RB-09-252-009

215592.120<1113<21.2211<0.3<1657RB-09-252-01070271.717<135<20.2603<0.3<1147RB-09-253-00194541.09<158<20.6125<0.3<192RB-09-253-002

762183.127<18132.0826<0.31132RB-09-253-003153524.336<118331.1112<0.3<1169RB-09-253-004

97973.432<113020.81614<0.3<1152RB-09-253-005151693.934<111931.0214<0.3<1228RB-09-253-006228302.722<18920.92812<0.3<1261RB-09-253-007161191.18<132<20.98612<0.3<168RB-09-253-008661052.320<1198<20.6397<0.3<11360RB-09-253-009

162533.128<197<21.0011<0.3<1233RB-09-254-001206464.444<111021.1113<0.3<1228RB-09-254-002149804.846<112631.0811<0.3<1238RB-09-254-00372171.210<157<20.2607<0.3<1184RB-09-254-004681042.321<120320.6367<0.3<11350RB-09-253-009 R

11Page of 14









3710.32<14<20.0301<0.3<142ASR109181322.620<190<20.87811<0.3<1237RB-09-254-005223335.153<193<20.893120.3<1369RB-09-254-0067550.76<115<20.3024<0.3<165RB-09-254-007641761.819<1102<20.5049<0.3<1633RB-09-254-008

65962.119<199<20.57910<0.3<1753RB-09-254-009195717.077<110421.04161.0<1192RB-09-255-001264523.530<1116<21.1013<0.3<1257RB-09-255-002237101.613<187<22.2214<0.3187RB-09-255-00310261.110<129<20.4404<0.3<165RB-09-255-004

5270.76<123<20.2953<0.3<1124RB-09-255-005193483.530<19120.96914<0.3<1226RB-09-255-006222243.636<18820.87213<0.3<1275RB-09-255-00711490.98<130<21.158<0.3<185RB-09-255-00863682.424<1130<20.62711<0.3<1686RB-09-255-009

122889.6112<112331.12191.3<1221RB-09-256-00179101.618<138<20.4945<0.3<1209RB-09-256-0027950.87<157<20.3164<0.3<1113RB-09-256-003

100704.642<116731.1416<0.3<1256RB-09-256-004248384.547<184<21.2210<0.3<1208RB-09-256-005

25621.312<11530.22927<0.31164ASR2095480.98<123<20.2273<0.3<191RB-09-256-00668661.911<1511150.5256<0.3<1124RB-09-256-007

223443.428<19020.97514<0.3<1246RB-09-256-008119141.311<134<20.4794<0.3<189RB-09-256-009

129745.149<113221.0413<0.3<1279RB-09-256-01094110.86<122<20.5593<0.3<181RB-09-256-01159952.422<1193<20.7698<0.3<1727RB-09-256-01252751.715<1136<20.5105<0.3<1798RB-09-256-0134440.66<130<20.1263<0.3<172RB-09-257-001

208754.342<1108<21.0113<0.3<1222RB-09-257-002143513.838<195<21.0213<0.3<1215RB-09-257-003122574.036<1120<21.0412<0.3<1268RB-09-257-004197453.428<19321.1211<0.3<1199RB-09-257-00559211.111<154<20.3916<0.3<190RB-09-257-006

173664.036<111721.0814<0.3<1297RB-09-257-007129452.016<166<20.5457<0.3<1265RB-09-257-00885411.513<142<20.5876<0.31156RB-09-257-00961812.220<118230.6108<0.3<11420RB-09-257-010

168653.834<111521.0613<0.3<1313RB-09-257-007 R

12Page of 14









4220.32<16<20.0291<0.3<144ASR109131101.411<142111.0713<0.3<195RB-09-258-0016160.98<147<20.5016<0.3<192RB-09-258-00242275.162<151<20.27661.9<1182RB-09-258-003

108734.239<1122<20.95113<0.3<1193RB-09-258-004

125141.210<150<20.7497<0.3<1117RB-09-258-005249443.630<1122<21.3212<0.3<1221RB-09-258-006141505.551<1119<21.1313<0.3<1234RB-09-258-007204822.621<1107<20.93814<0.3<1219RB-09-258-008193674.238<1122<21.0815<0.3<1188RB-09-259-001

148835.953<1137<21.1819<0.3<1230RB-09-259-00210191.08<146<20.97512<0.3<1107RB-09-259-003202131.714<193<21.7613<0.3<191RB-09-259-0048250.86<120<20.6064<0.3<170RB-09-259-0054840.76<116<20.1661<0.3<197RB-09-259-006

82281.09<157<20.4419<0.3<1130RB-09-259-007198514.036<18741.0014<0.3<1240RB-09-259-008219323.629<19521.0114<0.3<1247RB-09-259-009124836.668<1138<21.05140.5<1319RB-09-259-010105371.412<196<20.3554<0.3<1138RB-09-259-011

25221.312<11630.23427<0.3<1170ASR20937922.632<1264<20.403100.8<11110RB-09-259-0126460.75<138<20.3575<0.3<1142RB-09-260-001

155514.035<111721.1213<0.3<1201RB-09-260-002171905.255<112541.35120.3<1260RB-09-260-003

56140.98<137<20.3945<0.3<1125RB-09-260-004237363.428<199<21.0614<0.3<1173RB-09-260-005201666.576<1158<21.10130.9<1173RB-09-260-00663502.116<121020.8144<0.3<1322RB-09-260-0074161.010<181<20.2313<0.3<169RB-09-261-001

257101.914<116322.6033<0.3195RB-09-261-002202171.412<161<21.0311<0.3<1220RB-09-261-003199121.916<181<21.216<0.3<1138RB-09-261-004170603.228<1112<21.079<0.3<1198RB-09-261-005152301.512<16221.647<0.3<1143RB-09-261-006

15161.110<134<20.6786<0.3<1125RB-09-261-007141463.327<1133<20.87612<0.3<1343RB-09-261-00891130.97<182<20.5795<0.3<191RB-09-261-009

129462.120<184<20.5855<0.3<1252RB-09-262-001136453.427<1131<20.87012<0.3<1346RB-09-261-008 R

13Page of 14









4010.32<14<20.0301<0.3<141ASR109591012.016<124620.6136<0.3<1470RB-09-262-002

105632.623<1110<20.7319<0.3<1458RB-09-262-0039772.110<1633<20.6101<0.3<1148RB-09-263-001

56372.221<184<20.42570.3<1627RB-09-263-002

54372.424<178<20.42290.3<1637RB-09-263-002 R

Total Digestion: A 0.250 g pulp is gently heated in a mixture of HF/HNO3/HClO4 until dry and the residue dissolved in dilute HNO3. The standards are ASR109 and ASR209.

14Page of 14



ICP1 Partial Digestion






Silver in ppm (Ag) Arsenic in ppm (As) Bismuth in ppm (Bi) Cobalt in ppm (Co) Copper in ppm (Cu)

Germanium in ppm (Ge) Mercury in ppm (Hg) Molybdenum in ppm (Mo) Nickel in ppm (Ni) Lead in ppm (Pb)

Antimony in ppm (Sb) Selenium in ppm (Se) Tellurium in ppm (Te) Uranium (Fluorimetry) in ppm (U, Fl.) Vanadium in ppm (V)

Zinc in ppm (Zn)

ZnVU, Fl.TeSeSbPbNiMoHgGeCuCoBiAsAgSampleppmppmppmppmppmppmppmppmppmppmppmppmppmppmppmppmNumber

1.01.90.180<0.20.5<0.21.2013.12.5<0.2<0.24.70.70.70.7<0.1ASR1090.421.71.99<0.20.4<0.22.7013.30.2<0.2<0.22.05.20.20.90.6RB-09-251-001

32.019.32.54<0.23.9<0.26.3923.40.20.2<0.234.311.90.80.80.7RB-09-251-00220.68.20.760<0.23.0<0.25.3124.5<0.10.2<0.21.811.60.81.1<0.1RB-09-251-00314.616.40.870<0.22.1<0.26.0922.90.2<0.2<0.210.99.91.11.4<0.1RB-09-251-004

15.127.30.960<0.22.4<0.29.1918.10.2<0.20.40.68.61.31.0<0.1RB-09-251-00512.318.71.04<0.22.3<0.27.2314.4<0.1<0.2<0.211.68.20.9<0.2<0.1RB-09-251-00621.926.51.07<0.22.5<0.27.8219.2<0.1<0.20.32.011.80.90.5<0.1RB-09-251-00757.326.91.09<0.24.4<0.27.1343.50.2<0.20.40.617.30.50.8<0.1RB-09-251-00812.56.00.260<0.20.4<0.20.884.90.2<0.2<0.21.53.10.20.3<0.1RB-09-251-009

6.68.20.310<0.20.2<0.21.332.00.2<0.2<0.21.82.10.20.5<0.1RB-09-251-01012.111.40.980<0.21.3<0.24.6415.5<0.1<0.2<0.218.65.20.70.4<0.1RB-09-251-01142.822.80.320<0.22.8<0.22.6011.1<0.1<0.20.310.112.40.70.3<0.1RB-09-251-01215.930.91.25<0.21.5<0.29.667.30.1<0.20.219.83.80.51.60.1RB-09-251-01393.12.10.330<0.2<0.2<0.20.704.30.3<0.2<0.21.80.50.53.1<0.1RB-09-251-014

9.611.20.940<0.21.2<0.23.9910.60.4<0.2<0.223.09.80.43.70.4RB-09-252-00123.616.30.9500.52.5<0.25.5422.40.10.2<0.220.510.21.12.0<0.1RB-09-252-00217.427.10.880<0.21.7<0.27.2218.0<0.1<0.20.30.59.11.20.7<0.1RB-09-252-00312.83.20.710<0.2<0.2<0.21.343.1<0.1<0.2<0.232.83.8<0.20.7<0.1RB-09-252-00412.022.40.100.4<0.2<0.21.743.00.2<0.2<0.22.55.20.81.6<0.1RB-09-252-005

1Page of 4









1.14.81.19<0.20.50.22.7011.92.0<0.2<0.24.10.70.71.7<0.1ASR2095.56.10.620<0.2<0.2<0.21.101.00.1<0.2<0.229.61.4<0.20.5<0.1RB-09-252-006

61.329.60.950<0.21.3<0.29.3034.30.1<0.20.58.821.21.30.4<0.1RB-09-252-00717.419.00.650<0.22.3<0.24.6115.7<0.1<0.20.431.97.30.90.6<0.1RB-09-252-00816.624.61.16<0.23.3<0.26.1959.0<0.10.3<0.216.214.21.22.00.1RB-09-252-009

40.363.90.9100.23.6<0.24.4634.4<0.10.2<0.21717.51.24.9<0.1RB-09-252-0108.819.20.1101.00.5<0.22.104.10.2<0.2<0.217.86.21.33.1<0.1RB-09-253-001

53.529.00.630<0.22.4<0.22.056.1<0.1<0.20.211.115.00.60.4<0.1RB-09-253-0025.010.50.780<0.20.3<0.24.655.40.4<0.2<0.230.66.40.62.6<0.1RB-09-253-003

15.541.11.070.53.1<0.25.7220.2<0.1<0.20.36.410.41.0<0.2<0.1RB-09-253-004

54.119.60.960<0.23.6<0.25.6879.00.10.30.43.919.11.31.3<0.1RB-09-253-00523.116.40.940<0.21.5<0.27.2127.4<0.1<0.20.66.711.91.21.0<0.1RB-09-253-0066.26.61.26<0.21.3<0.23.2014.0<0.1<0.2<0.244.15.30.50.7<0.1RB-09-253-007

16.718.60.3500.31.0<0.21.323.00.3<0.2<0.20.94.10.30.8<0.1RB-09-253-00880.820.80.940<0.22.7<0.213.770.5<0.10.4<0.216.612.71.512.8<0.1RB-09-253-009

27.622.20.660<0.22.5<0.25.5222.8<0.1<0.2<0.234.814.50.81.6<0.1RB-09-254-00114.220.40.780<0.22.3<0.25.5316.7<0.1<0.20.20.49.60.90.6<0.1RB-09-254-00239.424.70.190<0.21.6<0.28.0823.0<0.10.20.52.113.91.4<0.2<0.1RB-09-254-00312.69.50.620<0.20.9<0.20.938.4<0.1<0.2<0.23.35.1<0.2<0.2<0.1RB-09-254-00481.523.11.03<0.24.4<0.213.671.7<0.10.4<0.217.313.01.613.4<0.1RB-09-253-009 R

0.81.70.1700.40.2<0.21.1913.22.4<0.2<0.24.50.70.60.6<0.1ASR10913.26.10.840<0.22.0<0.23.3920.5<0.1<0.2<0.27.812.81.00.7<0.1RB-09-254-0057.212.00.700<0.22.2<0.23.7616.5<0.1<0.20.25.27.60.61.0<0.1RB-09-254-0061.86.00.260<0.20.3<0.20.871.30.2<0.2<0.23.81.4<0.20.5<0.1RB-09-254-00713712.00.470<0.22.8<0.251.360.8<0.10.5<0.253.518.41.66.3<0.1RB-09-254-008

67.422.10.840<0.28.1<0.29.0090.4<0.10.60.444.914.92.112.8<0.1RB-09-254-00911.722.01.040.90.6<0.29.6710.60.3<0.20.40.95.81.51.3<0.1RB-09-255-00128.125.10.7200.22.2<0.26.2925.00.1<0.20.34.410.01.01.7<0.1RB-09-255-0022.429.50.4000.4<0.2<0.20.971.80.1<0.2<0.26.02.7<0.2<0.2<0.1RB-09-255-0030.719.70.330<0.2<0.2<0.21.051.90.2<0.2<0.230.33.30.41.1<0.1RB-09-255-004

2.75.60.250<0.20.5<0.20.842.5<0.1<0.2<0.22.43.8<0.20.6<0.1RB-09-255-00513.312.80.980<0.21.9<0.26.3419.1<0.1<0.20.20.66.51.01.3<0.1RB-09-255-0062.310.80.660<0.20.9<0.23.018.2<0.1<0.2<0.21.22.90.60.4<0.1RB-09-255-0072.714.90.3400.3<0.2<0.21.152.00.2<0.2<0.239.82.2<0.21.7<0.1RB-09-255-0087.83.10.230<0.20.6<0.22.0715.0<0.1<0.2<0.27.53.60.33.3<0.1RB-09-255-009

34.924.31.740.81.0<0.211.326.40.5<0.20.52.613.21.80.8<0.1RB-09-256-0010.67.10.440<0.20.9<0.21.092.3<0.1<0.2<0.223.82.50.20.8<0.1RB-09-256-0020.928.30.1400.50.4<0.20.770.70.2<0.2<0.238.51.70.20.5<0.1RB-09-256-003

27.346.00.8900.72.1<0.211.418.60.3<0.21.00.613.01.51.2<0.1RB-09-256-00415.716.00.620<0.21.7<0.23.2415.5<0.1<0.20.211.29.30.6<0.2<0.1RB-09-256-005

2Page of 4









0.95.01.19<0.20.2<0.22.5612.12.1<0.2<0.24.30.80.71.6<0.1ASR2093.58.40.060<0.2<0.2<0.21.722.40.1<0.2<0.22.23.00.20.4<0.1RB-09-256-006

63.91497.232.02.90.62.9320.50.2<0.20.711516.01.2<0.20.8RB-09-256-00710.011.60.870<0.21.9<0.25.7119.3<0.1<0.20.20.46.60.81.1<0.1RB-09-256-0086.710.60.380<0.21.0<0.21.805.10.2<0.2<0.23.05.10.40.9<0.1RB-09-256-009

40.126.90.8900.33.3<0.27.6725.5<0.10.30.667.913.61.51.2<0.1RB-09-256-0105.611.90.300<0.2<0.2<0.21.123.70.2<0.2<0.24.22.60.21.3<0.1RB-09-256-011

75.319.01.52<0.23.7<0.29.2161.5<0.10.4<0.234.316.61.67.30.1RB-09-256-01255.234.70.770<0.25.8<0.218.552.0<0.10.50.326.910.71.79.4<0.1RB-09-256-0130.816.60.6000.4<0.2<0.20.842.40.1<0.2<0.21.72.00.31.0<0.1RB-09-257-001

35.816.80.890<0.22.3<0.26.3225.9<0.10.2<0.23.412.21.20.5<0.1RB-09-257-00220.916.40.7200.41.3<0.26.2914.50.2<0.2<0.210.28.11.00.4<0.1RB-09-257-00312.215.00.610<0.21.4<0.25.2116.1<0.1<0.2<0.24.18.30.70.3<0.1RB-09-257-00418.919.10.860<0.21.9<0.26.8517.00.1<0.20.421.610.50.91.1<0.1RB-09-257-00516.215.40.540<0.20.6<0.21.7110.60.1<0.2<0.25.55.30.20.5<0.1RB-09-257-006

30.723.80.6800.32.0<0.28.9527.1<0.1<0.20.51.312.51.21.5<0.1RB-09-257-00733.613.60.670<0.21.9<0.23.4920.2<0.1<0.20.311.821.30.80.6<0.1RB-09-257-00838.318.80.570<0.21.8<0.22.869.90.1<0.20.215.07.40.7<0.2<0.1RB-09-257-00954.824.42.56<0.26.1<0.224.494.70.10.4<0.228.827.91.630.6<0.1RB-09-257-01030.923.30.7400.21.9<0.28.9827.3<0.1<0.20.61.412.81.11.6<0.1RB-09-257-007 R

0.81.60.2000.20.2<0.21.2313.22.6<0.2<0.24.50.80.60.6<0.1ASR1090.79.26.390.3<0.2<0.23.037.20.2<0.2<0.257.27.40.21.1<0.1RB-09-258-0010.620.81.060.3<0.2<0.21.533.2<0.1<0.2<0.23.05.40.62.3<0.1RB-09-258-0020.86.20.420<0.2<0.2<0.20.392.5<0.1<0.2<0.20.21.50.40.9<0.1RB-09-258-003

23.726.00.7800.52.4<0.27.3323.70.10.2<0.25.511.61.21.8<0.1RB-09-258-004

7.619.20.450<0.20.4<0.21.262.80.1<0.2<0.227.24.60.20.3<0.1RB-09-258-00517.338.31.010.91.1<0.26.9614.4<0.1<0.20.70.78.61.11.2<0.1RB-09-258-00612.525.31.370.32.3<0.27.8918.1<0.1<0.20.4<0.19.01.20.5<0.1RB-09-258-00762.426.61.02<0.23.3<0.24.3743.20.20.20.37.918.41.10.8<0.1RB-09-258-00822.327.60.8400.32.0<0.27.8220.30.3<0.20.21.410.31.11.60.2RB-09-259-001

28.943.61.281.11.1<0.213.420.60.2<0.20.8<0.111.91.70.4<0.1RB-09-259-0020.817.90.4800.3<0.2<0.20.671.10.2<0.2<0.216.81.8<0.21.3<0.1RB-09-259-0030.914.91.080.70.5<0.23.451.10.4<0.20.523.51.20.90.4<0.1RB-09-259-0040.76.60.200<0.2<0.2<0.20.491.00.2<0.2<0.217.21.2<0.20.4<0.1RB-09-259-0051.03.61.05<0.2<0.2<0.20.660.80.2<0.2<0.21201.1<0.20.8<0.1RB-09-259-006

24.021.61.4<0.21.2<0.21.4013.90.2<0.2<0.20.89.40.2<0.2<0.1RB-09-259-00711.212.51.98<0.22.8<0.25.8822.0<0.1<0.20.323.37.21.00.2<0.1RB-09-259-0088.314.60.920<0.22.2<0.23.6616.3<0.1<0.2<0.269.07.50.50.80.4RB-09-259-009

39.431.51.460.32.8<0.29.3024.60.3<0.20.512312.51.60.9<0.1RB-09-259-01033.739.30.9800.51.30.33.098.60.2<0.20.496.411.00.72.70.1RB-09-259-011

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0.94.51.200.20.2<0.22.6912.32.1<0.2<0.24.10.80.62.0<0.1ASR20915.215.71.060.20.5<0.222.117.6<0.1<0.2<0.212.02.80.514.8<0.1RB-09-259-0121.15.70.160<0.2<0.2<0.20.641.70.1<0.2<0.20.51.4<0.21.0<0.1RB-09-260-0019.424.41.45<0.21.3<0.27.3712.60.2<0.20.4<0.16.31.10.8<0.1RB-09-260-002

33.828.91.82<0.22.0<0.26.3622.30.2<0.20.32.918.41.6<0.2<0.1RB-09-260-003

6.08.70.520<0.20.7<0.21.004.9<0.1<0.2<0.22.33.90.30.6<0.1RB-09-260-00412.721.90.870<0.23.2<0.26.2919.0<0.1<0.2<0.21.47.70.70.4<0.1RB-09-260-00525.337.21.20.81.7<0.29.1922.00.3<0.20.60.510.61.70.8<0.1RB-09-260-00616.118.82.89<0.22.7<0.28.35102<0.10.20.250148.61.12.3<0.1RB-09-260-0071.240.50.5200.70.4<0.21.934.00.3<0.2<0.21.61.40.3<0.2<0.1RB-09-261-001

1.171.90.5901.3<0.2<0.23.071.10.3<0.2<0.2<0.12.2<0.20.30.2RB-09-261-0026.120.30.9600.20.3<0.21.505.40.2<0.2<0.20.44.10.40.6<0.1RB-09-261-0031.225.40.4300.2<0.2<0.22.172.50.2<0.2<0.218.13.80.31.0<0.1RB-09-261-004

31.431.20.8500.52.0<0.27.1522.80.3<0.20.60.314.81.40.9<0.1RB-09-261-00517.012.60.920<0.21.5<0.22.166.60.1<0.2<0.21.210.60.30.4<0.1RB-09-261-006

1.35.31.23<0.2<0.2<0.20.791.00.1<0.2<0.29.41.8<0.20.6<0.1RB-09-261-0078.112.30.670<0.22.8<0.23.4217.1<0.1<0.2<0.23166.00.6<0.2<0.1RB-09-261-0087.755.00.4900.71.2<0.21.957.80.2<0.20.413310.90.40.9<0.1RB-09-261-009

22.329.60.480<0.21.8<0.23.8448.40.5<0.2<0.222.313.10.33.00.1RB-09-262-0018.111.50.70<0.22.2<0.23.3417.6<0.10.2<0.23206.20.50.2<0.1RB-09-261-008 R

1.01.80.170<0.2<0.2<0.21.1213.12.6<0.2<0.24.60.70.70.7<0.1ASR10995.753.41.980.25.4<0.214.462.94.80.40.955.516.52.620.50.2RB-09-262-00234.710.80.760<0.24.8<0.27.7968.7<0.10.60.732.115.22.26.2<0.1RB-09-262-00318.61240.0700.42.2<0.26.141.40.5<0.21.263.634.61.23.8<0.1RB-09-263-0013.813.40.9100.20.7<0.22.4720.20.4<0.2<0.212.93.51.26.7<0.1RB-09-263-002

3.811.50.820<0.20.8<0.22.4018.00.3<0.2<0.210.92.90.94.2<0.1RB-09-263-002 R

Partial Digestion: A 2.00 g pulp is digested with 2.25 ml of 8:1 HNO3:HCl for 1 hour at 95 C. The standards are ASR109 and ASR209.

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0.81.210.52<0.20.30.35497<113<0.20.02<0.2180.52<0.2ASR1091.12.3100.880.81.01.66174390.70.740.87299.34<0.2RB-09-239-0012.02.8131.380.91.51.87255480.80.281.577411.2<0.2RB-09-239-0022.811.4258.763.16.89.3674151051.17.043.027316.7<0.2RB-09-239-0031.31.760.460.51.01.25481310.51.390.73806.69<0.2RB-09-239-004

1.72.280.440.71.11.37479430.60.730.94147.89<0.2RB-09-239-0051.92.170.410.61.11.36254440.40.480.83986.63<0.2RB-09-239-0064.14.0201.151.12.52.41615810900.90.202.544912.9<0.2RB-09-239-0071.51.470.430.50.81.01093270.60.860.86847.86<0.2RB-09-239-0082.52.6100.440.81.61.74144570.80.461.451410.8<0.2RB-09-239-009

1.52.090.460.71.01.413146280.60.921.27669.50<0.2RB-09-239-0102.22.780.430.71.72.121114390.60.991.16879.40<0.2RB-09-239-0111.92.480.540.71.21.617185470.61.470.96067.59<0.2RB-09-239-0123.09.4463.352.65.86.41131854995<0.20.4010.036025.10.3RB-09-239-0131.01.660.420.51.01.39308280.51.320.64107.34<0.2RB-09-239-014

1.41.680.610.60.91.2166168280.61.120.75937.740.3RB-09-239-0150.91.5101.070.60.91.42104370.71.211.389310.3<0.2RB-09-240-0013.36.0328.072.03.94.0888171011.30.763.931920.10.2RB-09-240-0021.86.2166.261.73.77.075213560.913.72.216213.6<0.2RB-09-240-0031.12.030.310.61.11.715261240.54.190.59715.88<0.2RB-09-240-004

6.42.630.870.51.41.75478148<0.20.030.3202.48<0.2ASR2092.32.3100.510.71.21.4154310530.60.101.24498.470.3RB-09-240-0051.31.240.320.40.60.8493160.30.870.54255.14<0.2RB-09-240-0061.72.6100.520.81.41.87264410.70.821.25039.83<0.2RB-09-240-0071.11.470.280.50.70.96183240.60.560.76077.87<0.2RB-09-240-008

2.42.360.300.71.61.83784250.51.440.79217.19<0.2RB-09-240-0094.85.8285.461.83.43.7277417941.20.535.151318.30.2RB-09-241-0013.26.0237.381.83.75.8117115791.26.764.028116.0<0.2RB-09-241-0027.76.0192.941.63.33.8693891151.11.452.552714.60.2RB-09-241-0035.87.5143.382.23.23.9194871360.61.281.543010.3<0.2RB-09-241-004

1.21.550.250.50.81.35302200.43.010.53285.76<0.2RB-09-241-0051.11.140.300.40.60.84133200.30.750.44014.73<0.2RB-09-241-0061.52.270.620.61.21.516356340.41.340.84736.16<0.2RB-09-241-0077.36.6130.871.64.14.1128881090.81.561.839911.7<0.2RB-09-241-0081.21.840.310.61.11.337144300.40.930.85636.13<0.2RB-09-241-009

1.42.8130.520.91.61.923185510.91.671.553112.1<0.2RB-09-241-0101.81.990.290.71.21.341113410.80.481.276810.1<0.2RB-09-241-0112.83.1112.700.81.51.81173690.70.141.346110.3<0.2RB-09-242-0010.91.560.500.50.61.0<161250.51.050.67227.08<0.2RB-09-242-0021.01.950.300.61.11.338134300.40.900.75576.02<0.2RB-09-241-009 R

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0.71.210.52<0.20.20.35481<114<0.20.02<0.2180.51<0.2ASR1093.56.3266.501.83.85.0257918901.33.044.237718.7<0.2RB-09-242-0032.53.3211.721.01.72.27307711.21.512.868716.6<0.2RB-09-242-0042.76.6287.021.83.54.389920941.32.074.333619.7<0.2RB-09-242-0053.34.5265.241.33.03.01523973750.90.465.629519.00.4RB-09-242-006

1.01.240.470.40.61.09124180.41.070.44795.20<0.2RB-09-242-0071.20.840.280.30.40.6463140.30.690.45195.01<0.2RB-09-242-0084.34.440.510.72.02.54183790.30.090.54505.34<0.2RB-09-243-0013.36.7336.401.94.04.55110119921.40.427.638121.0<0.2RB-09-243-0025.96.5265.691.83.44.14069131171.10.454.239217.7<0.2RB-09-243-003

6.13.9183.621.12.33.3164211731.02.262.445914.9<0.2RB-09-243-0042.95.72610.31.83.53.83324721891.00.444.836518.1<0.2RB-09-243-0051.51.450.360.40.71.06225260.51.100.55206.08<0.2RB-09-243-0061.61.350.320.40.70.98173240.40.500.65405.63<0.2RB-09-243-0071.00.840.520.30.30.5965150.30.400.45405.06<0.2RB-09-243-008

1.41.771.060.51.01.3482230.60.581.06617.99<0.2RB-09-243-0092.72.272.170.61.51.64105410.61.261.17498.36<0.2RB-09-243-0102.22.572.280.71.62.07174470.41.171.15517.31<0.2RB-09-243-0113.85.0182.501.32.12.73557881.00.203.461915.4<0.2RB-09-243-0121.92.080.420.60.91.271286460.50.220.85347.72<0.2RB-09-244-001

6.22.530.870.41.21.75460151<0.20.020.3202.59<0.2ASR2091.61.740.370.51.11.3277243340.41.920.64925.280.2RB-09-244-0021.51.550.750.40.81.019152250.40.570.75165.86<0.2RB-09-244-0031.82.2121.300.71.11.47304490.80.311.456510.6<0.2RB-09-244-0041.42.1124.190.81.21.412168510.70.421.750910.8<0.2RB-09-244-005

3.14.282.681.12.54.318356480.712.01.03309.04<0.2RB-09-245-0013.64.2152.961.22.73.2587714581.03.231.640613.6<0.2RB-09-245-0023.66.2215.491.73.34.0119218861.01.342.643616.0<0.2RB-09-245-0033.24.9185.471.42.83.81810117601.07.882.039214.8<0.2RB-09-245-0042.67.3267.732.13.84.514103161261.32.933.322219.7<0.2RB-09-245-005

3.94.6258.021.43.03.31315020691.41.342.541918.0<0.2RB-09-245-0063.15.0306.721.73.33.62611220911.40.643.737921.8<0.2RB-09-245-0078.24.3101.290.74.04.3172387620.50.970.94387.82<0.2RB-09-245-0081.11.250.790.40.60.83172250.40.640.64145.18<0.2RB-09-245-0092.52.970.700.71.41.75402910.50.531.05917.35<0.2RB-09-245-010

7.64.6130.921.02.32.769041070.70.121.455110.7<0.2RB-09-245-0111.21.160.640.40.50.7461270.50.230.68437.72<0.2RB-09-245-0122.86.6319.372.04.14.6810623961.30.598.237821.1<0.2RB-09-245-0131.21.560.470.50.91.7558140.53.450.77007.64<0.2RB-09-245-0146.94.0130.900.92.02.459641040.60.131.454610.5<0.2RB-09-245-011 R

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0.61.210.53<0.20.20.34483<114<0.20.01<0.2180.52<0.2ASR1091.51.651.680.51.01.45132220.51.580.610906.85<0.2RB-09-245-0151.42.241.190.61.12.74146230.45.340.43255.26<0.2RB-09-246-0011.00.830.250.30.40.7<1191150.41.310.33445.75<0.2RB-09-246-0023.78.9278.762.55.06.01058191531.10.652.656717.61.2RB-09-246-003

3.411.2267.563.05.77.4460141571.20.622.557917.3<0.2RB-09-246-0042.32.662.010.81.83.43812260.75.260.35636.99<0.2RB-09-246-0053.49.4196.292.54.96.3337121140.90.511.880313.7<0.2RB-09-246-0063.03.681.260.81.41.927264830.40.450.74468.26<0.2RB-09-246-0074.67.8257.362.24.75.51575161161.00.533.037216.2<0.2RB-09-246-008

3.87.5247.062.14.35.268915971.21.282.524616.9<0.2RB-09-246-0096.05.8205.271.63.33.810515823980.90.901.998015.2<0.2RB-09-246-0101.43.2215.081.02.32.43911641461.23.251.846317.40.4RB-09-246-0111.01.240.960.40.71.15122200.41.690.23266.420.7RB-09-247-0011.91.450.540.50.81.0161290.41.070.34686.44<0.2RB-09-247-002

6.47.2278.072.04.44.9457201121.00.542.460817.3<0.2RB-09-247-0039.16.7196.701.84.44.8641111151.00.521.570614.3<0.2RB-09-247-0044.211.72910.53.06.27.71768201611.20.893.646717.7<0.2RB-09-248-0011.82.270.450.71.21.7682490.61.270.56019.28<0.2RB-09-248-0022.42.770.530.81.42.39295550.72.350.44968.13<0.2RB-09-248-003

6.22.430.840.41.31.75396150<0.20.020.2202.47<0.2ASR2097.012.8299.283.56.88.1657181961.20.652.164418.3<0.2RB-09-248-0042.12.160.680.71.31.93672340.52.130.45036.97<0.2RB-09-248-0053.96.8264.951.94.04.66114726981.20.454.445618.9<0.2RB-09-248-0061.92.341.490.61.34.19133220.57.600.53575.29<0.2RB-09-248-007

5.36.8186.032.13.34.067391140.90.722.144013.4<0.2RB-09-248-0082.01.540.810.40.81.0318337<0.20.270.318203.86<0.2RB-09-248-0091.64.2246.931.32.62.9449420591.24.292.386916.50.2RB-09-248-0101.34.2165.451.23.03.3358221510.99.461.697413.0<0.2RB-09-248-0111.24.4206.391.32.93.1339014601.14.552.173414.90.2RB-09-248-012

1.03.9114.801.02.63.0326812510.510.61.06069.77<0.2RB-09-248-0135.510.6299.892.75.56.51058171451.21.692.762718.4<0.2RB-09-249-0012.82.381.670.71.41.6611715480.61.060.412008.180.2RB-09-249-0022.42.880.330.81.71.97162750.60.960.54878.65<0.2RB-09-249-0033.23.2141.641.02.02.316327660.70.191.244010.4<0.2RB-09-249-004

1.62.6111.650.81.31.82339550.70.581.025510.6<0.2RB-09-249-0058.43.6123.421.12.52.6145418850.60.360.97209.97<0.2RB-09-249-0063.45.62910.21.63.94.3138723601.10.753.364818.1<0.2RB-09-249-0073.96.3237.001.83.74.3227610981.10.582.4122015.8<0.2RB-09-249-0088.43.7123.401.12.52.6135517850.50.360.96919.95<0.2RB-09-249-006 R

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0.71.2<10.53<0.20.20.36473<115<0.20.02<0.2200.52<0.2ASR1090.52.732.020.50.45.337467100.446.80.72124.78<0.2RB-09-249-0096.09.7279.152.64.16.21460181491.11.043.256017.0<0.2RB-09-250-0012.31.670.660.50.61.213142320.61.430.45387.77<0.2RB-09-250-0028.24.682.811.22.64.2262111840.53.360.46357.660.2RB-09-250-003

5.17.4298.102.04.15.6665151031.30.452.655418.6<0.2RB-09-250-0045.75.0175.121.62.23.21433151140.70.271.484211.9<0.2RB-09-250-0053.73.1132.311.01.32.092210700.70.300.853211.5<0.2RB-09-250-0063.85.6213.281.72.53.73257435951.00.353.858315.41.7RB-09-250-0075.810.7247.522.84.06.41775141670.90.602.848315.7<0.2RB-09-250-008

5.85.9144.631.43.95.6196411760.70.291.744610.7<0.2RB-09-250-0097.44.3163.021.12.63.4126811690.90.282.162313.8<0.2RB-09-250-0105.33.821.280.71.72.61915376<0.21.600.445603.16<0.2RB-09-250-0112.35.5235.061.52.74.0439525671.27.552.6115015.70.6RB-09-250-0121.03.693.180.81.42.537483300.727.50.85926.90<0.2RB-09-250-013

1.23.283.120.71.32.337462290.525.40.75906.87<0.2RB-09-250-013 R

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<11.2<1130.013124<10.0130.0040.029940.043<0.4ASR109<12.524160.036514<11.18<10.0520.61613204.12<0.4RB-09-239-001

23.045180.050111811.27<10.0100.46119294.350.5RB-09-239-002510.61811160.217344740.20<10.3264.5667583.172.2RB-09-239-003

<12.12390.02171121.01<10.0300.23017162.66<0.4RB-09-239-004

<12.634130.037121620.67<10.0180.31917203.02<0.4RB-09-239-005<12.535100.034101720.73<10.0100.23917262.48<0.4RB-09-239-006

14.289150.074353291.43<10.0060.60651493.200.9RB-09-239-007<11.712140.029610<11.53<10.0160.16918163.56<0.4RB-09-239-008<13.025170.04961972.20<10.0130.41429323.900.6RB-09-239-009

<12.123180.040711<11.52<10.0300.51911164.09<0.4RB-09-239-010<13.024170.03661521.77<10.0200.60917224.260.5RB-09-239-011<13.034160.03471720.97<10.0460.74812253.53<0.4RB-09-239-012

88.63110110.1251404520.14<10.0091.46153454.291.9RB-09-239-013<12.032110.02771011.13<10.0340.64911142.88<0.4RB-09-239-014

<12.013200.029611<10.78<10.0370.6498164.02<0.4RB-09-239-015<12.124180.038414<11.64<10.0740.84214194.89<0.4RB-09-240-001116.1209190.099443820.22<10.0432.3577544.461.3RB-09-240-002<18.211790.090302630.1810.6468.5341373.051.1RB-09-240-003<13.03270.01531020.88<10.1030.16216132.26<0.4RB-09-240-004

22.61470.04611155<0.0120.0050.0407220.2110.5ASR20912.644140.032181730.48<10.0030.19519272.970.4RB-09-240-005

<11.411100.01656<10.69<10.0160.3411492.60<0.4RB-09-240-006<12.934150.03781531.57<10.0220.77631223.840.4RB-09-240-007<11.712150.02469<11.39<10.0110.48721133.92<0.4RB-09-240-008

<12.522120.02741031.47<10.0230.4739143.310.4RB-09-240-00995.7158140.092353531.43<10.0522.1194513.871.2RB-09-241-00146.6147120.089312960.65<10.4115.1162443.731.1RB-09-241-00237.0811170.118134192.16<10.0521.2441653.671.2RB-09-241-00339.2814120.072175470.68<10.0641.2522773.141.1RB-09-241-004

<12.42280.0186820.90<10.0570.15110112.32<0.4RB-09-241-005<11.412110.01667<10.56<10.0150.14011112.55<0.4RB-09-241-006<12.633120.023131330.43<10.0260.25512162.61<0.4RB-09-241-007

17.6911130.0841841161.88<10.0441.3038573.091.3RB-09-241-008<12.113140.02651151.05<10.0230.38312163.20<0.4RB-09-241-009

<13.445160.05071822.30<10.0290.78824284.010.5RB-09-241-010<12.124150.03541432.00<10.0130.40124224.090.4RB-09-241-011

23.536160.05272441.43<10.0140.41329403.500.5RB-09-242-001<12.0<13150.024110<10.81<10.0170.1629163.86<0.4RB-09-242-002<12.113130.02551141.02<10.0220.37112153.21<0.4RB-09-241-009 R

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<11.511100.017137<10.63<10.0300.6271092.89<0.4RB-09-242-007<11.011110.01455<10.63<10.0120.3021072.98<0.4RB-09-242-008<15.02770.031631120.20<10.0220.1183374.120.9RB-09-243-001

96.1188140.076553880.34<10.0332.08152434.431.3RB-09-243-00276.71411140.084324560.91<10.0381.6177603.791.2RB-09-243-003

34.3106140.067192571.58<10.1842.0054363.880.8RB-09-243-004115.0207150.0972123440.12<10.0402.0466433.971.3RB-09-243-005<11.722110.02011910.44<10.0180.17112123.02<0.4RB-09-243-006<11.412100.0225910.57<10.0120.3209122.89<0.4RB-09-243-007<10.9<11120.01675<10.66<10.0060.1341273.01<0.4RB-09-243-008

<11.812170.03741011.41<10.0120.22324114.34<0.4RB-09-243-009<12.323170.047714111.3910.0320.27616204.310.5RB-09-243-010<12.634140.04681671.22<10.0260.19312223.290.5RB-09-243-011

25.198150.063403251.33<10.0050.55746444.290.8RB-09-243-012<12.234160.03491630.72<10.0050.25212243.23<0.4RB-09-244-001

22.51470.05013166<0.0130.0040.0407220.2170.5ASR209<12.123140.02251260.6040.0400.5327162.80<0.4RB-09-244-002<11.51290.03261020.81<10.0110.1169122.86<0.4RB-09-244-003<12.244130.043131721.00<10.0060.24017243.530.4RB-09-244-004

41.844180.065101742.22<10.0100.28219273.750.4RB-09-244-005

<16.57660.085142341.6210.3023.5814292.490.8RB-09-245-001<14.615690.140382461.57<10.0932.5039313.560.8RB-09-245-002

55.9158150.283513650.63<10.0583.6070453.921.2RB-09-245-00315.9146150.144462640.88<10.1723.4047313.790.9RB-09-245-00467.81811160.150514640.10<10.0712.9971604.491.3RB-09-245-005

104.1185170.104792670.37<10.0682.0377343.221.0RB-09-245-00684.9208120.1108435100.1310.0462.17124473.821.1RB-09-245-007

<13.926140.0351122160.9310.0420.3779284.511.3RB-09-245-008<11.412100.02412910.53<10.0100.13311122.42<0.4RB-09-245-009<13.828100.046929151.27<10.0100.13511473.320.6RB-09-245-010

<14.8310120.061233761.30<10.0020.35731523.351.0RB-09-245-011<11.112150.02639<11.26<10.0050.11412144.23<0.4RB-09-245-012125.9228130.134753910.20<10.0202.1282515.491.4RB-09-245-013<12.111160.02336<11.4010.1342.32984.23<0.4RB-09-245-014

14.339120.061243361.30<10.0030.36231473.370.8RB-09-245-011 R

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99.01714180.149365920.88<10.0301.8452734.021.7RB-09-246-003

710.61715170.165266630.92<10.0211.2740773.642.0RB-09-246-004<13.210280.03631041.72<10.3203.054112.830.5RB-09-246-005

57.81110170.221204670.87<10.0220.84238553.251.8RB-09-246-006<14.428120.04553051.34<10.0220.43611433.000.6RB-09-246-007

76.91710160.143354640.32<10.0241.6246563.411.7RB-09-246-008

67.0199130.138414260.15<10.0231.7650492.881.5RB-09-246-00966.0148120.073773681.46<10.0532.2462472.681.2RB-09-246-01043.4154490.1101731962.3920.0624.6868242.880.7RB-09-246-011

<11.622260.0306840.97<10.0540.293782.24<0.4RB-09-247-001<11.81270.02721031.48<10.0270.0874142.18<0.4RB-09-247-002

106.71710210.160334571.53<10.0281.3746543.641.5RB-09-247-00346.3129160.1211742101.60<10.0370.77629523.511.6RB-09-247-004

1010.71916150.237396950.35<10.0421.8840794.492.3RB-09-248-001<12.62490.04221622.95<10.0570.2279222.740.4RB-09-248-002<13.16490.03621712.13<10.1120.4139242.360.4RB-09-248-003

22.51470.048121650.0120.0040.0387210.2050.6ASR209912.71819230.225318141.59<10.0311.0853873.102.4RB-09-248-004

<12.43380.02931331.34<10.0940.2426162.580.4RB-09-248-00556.2208120.1131143820.80<10.0382.4283483.401.4RB-09-248-006

<13.72380.65651011.08<10.5523.435121.90<0.4RB-09-248-007

47.11410100.092284580.19<10.0201.4230532.481.2RB-09-248-008<11.61340.02431271.03<10.0140.3027171.18<0.4RB-09-248-009

44.6155520.137822650.88<10.0918.2385313.570.8RB-09-248-010<15.8135280.151982460.7550.11612.978282.910.7RB-09-248-011

34.9146170.161642740.7010.07110.685323.090.8RB-09-248-012

<15.7105130.087692241.2710.09512.667291.470.7RB-09-248-013910.61915230.279336351.53<10.0351.5955723.531.9RB-09-249-001

<12.53480.03241792.15<10.0420.45012232.360.5RB-09-249-002<12.94470.04831751.09<10.0220.21512242.690.7RB-09-249-003

13.16680.046112341.07<10.0100.64329312.600.7RB-09-249-004

<12.94580.045132062.03<10.0350.88421271.930.5RB-09-249-00523.47590.0441924100.55<10.0241.0226332.281.0RB-09-249-006

134.2204170.159562790.28<10.0212.1946313.241.2RB-09-249-00786.016990.1183939100.37<10.0202.5747493.631.3RB-09-249-00813.47690.0431924110.55<10.0231.0025322.291.0RB-09-249-006 R

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<11.2<1130.014125<1<0.0130.0040.030960.046<0.4ASR109<11.73650.119341230.1610.7831.5817231.40<0.4RB-09-249-009119.91713180.176406140.74<10.0341.7048684.131.9RB-09-250-001<12.12270.04021242.26<10.0500.1656152.43<0.4RB-09-250-002<15.496100.044731221.38<10.2542.3213382.761.3RB-09-250-003

86.4207180.1143341160.86<10.0261.1672453.161.8RB-09-250-00445.097130.0722036141.06<10.0360.86437442.971.2RB-09-250-00513.14480.070112192.08<10.0220.69417272.720.9RB-09-250-00645.8148210.096533791.50<10.0271.3972452.541.1RB-09-250-007910.81613180.1793465110.24<10.0251.3745713.311.9RB-09-250-008

44.0115120.0612225100.20<10.0200.87132312.081.7RB-09-250-00933.514490.0552523110.66<10.0191.2148292.701.2RB-09-250-010

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4010.32<14<20.0271<0.3<139ASR1094260.98<160<20.1494<0.3<1120RB-09-239-00179161.312<158<20.2968<0.3<1142RB-09-239-002

118625.159<1101<20.792120.8<1114RB-09-239-0035960.87<121<20.2874<0.3<1101RB-09-239-004

6450.98<132<20.2904<0.3<1156RB-09-239-0057140.98<128<20.2676<0.3<1138RB-09-239-006

161131.915<18120.86411<0.3<1220RB-09-239-0075540.65<116<20.1763<0.3<1139RB-09-239-0089141.110<130<20.53310<0.3<1175RB-09-239-009

5740.88<124<20.1914<0.3<1210RB-09-239-0108241.412<122<20.2457<0.3<1175RB-09-239-0117040.98<126<20.2698<0.3<1169RB-09-239-012

123334.643<118231.03141.2<1373RB-09-239-0134140.87<125<20.2203<0.3<1109RB-09-239-014

5640.87<123<20.1104<0.3<1156RB-09-239-0153580.76<124<20.1143<0.3<1193RB-09-240-001

140803.326<112230.93715<0.3<1110RB-09-240-00268472.631<185<20.52210<0.3<1104RB-09-240-0034250.87<123<20.2153<0.3<189RB-09-240-004

27021.413<11620.22627<0.3<1169ASR2098861.08<13920.3918<0.3<1125RB-09-240-0054630.54<113<20.1012<0.3<179RB-09-240-0066041.010<133<20.3595<0.3<1151RB-09-240-0074130.65<117<20.1283<0.3<1129RB-09-240-008

9041.312<120<20.3456<0.3<1124RB-09-240-009189792.825<111320.87414<0.3<187RB-09-241-001129642.929<1113<20.67813<0.3<174RB-09-241-002302302.724<17620.74222<0.3<1137RB-09-241-003215272.322<172<20.76121<0.3<1100RB-09-241-004

4440.76<120<20.2133<0.3<184RB-09-241-0054020.54<111<20.1203<0.3<180RB-09-241-0065641.08<129<20.3768<0.3<196RB-09-241-007

28192.826<16721.2420<0.31232RB-09-241-0084440.77<122<20.4576<0.31119RB-09-241-009

5761.212<138<20.3385<0.3<1204RB-09-241-0106940.88<126<20.4336<0.3<1163RB-09-241-011

10961.211<13930.39415<0.3<199RB-09-242-0013330.55<117<20.0784<0.3<1106RB-09-242-0024230.77<121<20.4545<0.3<1119RB-09-241-009 R

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3540.65<114<20.0692<0.3<186RB-09-242-0074020.43<110<20.0542<0.3<177RB-09-242-008

17051.615129<21.0728<0.3<174RB-09-243-001135903.531<115540.97415<0.3<155RB-09-243-002223673.028<19770.86219<0.3<1105RB-09-243-003

242502.118<17620.72813<0.3<1124RB-09-243-004131683.328<115630.89111<0.3<1140RB-09-243-0055440.76<121<20.1763<0.3<194RB-09-243-0065640.65<121<20.2024<0.3<195RB-09-243-0073720.33<110<20.0782<0.3<178RB-09-243-008

5530.89<11420.2094<0.3<1122RB-09-243-00910051.110<12820.82211<0.3<1156RB-09-243-0108561.312<13440.6638<0.3<1175RB-09-243-011

154141.818<17130.72615<0.3<1124RB-09-243-0127350.87<127<20.3467<0.3<1147RB-09-244-001

26321.312<11630.23827<0.3<1167ASR2096250.87<121<20.5936<0.3<1113RB-09-244-0025850.76<118<20.2015<0.3<196RB-09-244-0037261.08<140<20.4067<0.3<1142RB-09-244-0045471.010<14020.4995<0.3<1193RB-09-244-005

127282.221<156<20.5347<0.3<173RB-09-245-001144552.321<1102<20.7329<0.3<174RB-09-245-002148792.827<110730.81411<0.3<1106RB-09-245-003125712.422<196<20.71110<0.3<1123RB-09-245-004108703.028<114820.79614<0.3<1133RB-09-245-005

160532.723<113930.90712<0.3<197RB-09-245-006131782.925<113330.92816<0.3<1101RB-09-245-007358174.231<128150.55614<0.3<189RB-09-245-0084240.65<11920.1493<0.3<1110RB-09-245-00995111.010<12450.71412<0.3<1180RB-09-245-010

299111.917<14650.73617<0.3<1184RB-09-245-0114630.44<114<20.2304<0.3<1144RB-09-245-012

122503.835<113870.90315<0.3<1215RB-09-245-01340110.67<113<20.0692<0.3<1125RB-09-245-014

290121.815<14650.72216<0.3<1180RB-09-245-011 R

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149794.440<1103<20.98814<0.3<1200RB-09-246-003

130554.651<186<20.940110.5<1212RB-09-246-00484231.512<142<20.5203<0.3<1117RB-09-246-005

131393.544<18730.986110.4<1261RB-09-246-006117151.010<137<20.51820<0.3<1109RB-09-246-007186554.240<111631.0113<0.3<1209RB-09-246-008

157443.936<112530.90013<0.3<1321RB-09-246-009242762.924111030.97114<0.3<1323RB-09-246-01061872.115<126630.6347<0.3<1640RB-09-246-0114050.85<115220.1342<0.3<168RB-09-247-0016840.75<140<20.3923<0.3<188RB-09-247-002

258723.734<111431.1115<0.3<1206RB-09-247-003380383.634<110321.4015<0.3<1207RB-09-247-004170785.156<112621.05140.6<1129RB-09-248-0017261.09<176<20.3213<0.3<1119RB-09-248-00283131.212<146<20.2324<0.3<1110RB-09-248-003

26121.312<11520.22527<0.3<1163ASR209281545.353<116721.27130.6<1254RB-09-248-0047981.09<136<20.4703<0.3<1104RB-09-248-005

160943.431<114450.99113<0.3<1188RB-09-248-00662321.012<127<20.2823<0.3<1104RB-09-248-007

212332.927<193<20.87011<0.3<1582RB-09-248-00875130.75<130<20.6908<0.3<153RB-09-248-009601132.018<116720.6736<0.3<11250RB-09-248-01049922.220<121550.5296<0.3<11500RB-09-248-01146762.119<1144<20.5987<0.3<1994RB-09-248-012

35542.019<117320.3595<0.3<11270RB-09-248-013221744.643<110521.1217<0.3<1222RB-09-249-001110111.18<194<20.84810<0.3<1115RB-09-249-0029671.212<133<20.6304<0.3<1128RB-09-249-003

127241.817<149<20.5536<0.3<1157RB-09-249-004

62251.110<187<20.4147<0.3<1110RB-09-249-005338432.218<16421.0410<0.3<1133RB-09-249-006147683.732<114130.90713<0.3<1365RB-09-249-007155553.430<111120.81411<0.3<1338RB-09-249-008335422.318<16321.0710<0.3<1130RB-09-249-006 R

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311152.520<1124<21.9020<0.32144RB-09-250-003

193554.540<1120<21.2511<0.3<1244RB-09-250-004218382.421<172<21.5011<0.3<1227RB-09-250-005144381.413<146<21.026<0.3<1139RB-09-250-006140732.623<1100100.8489<0.3<1265RB-09-250-007216494.141<1110<21.06130.4<1303RB-09-250-008

219254.247<166<20.88810<0.3<1180RB-09-250-009275303.025<176<21.0512<0.3<1186RB-09-250-010199151.514<15022.6030<0.33176RB-09-250-01182802.825<1141<20.74910<0.3<1958RB-09-250-01234581.817<166<20.30260.6<11040RB-09-250-013

36571.616<165<20.30050.6<11020RB-09-250-013 R


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Zinc in ppm (Zn)

1Page of 5









0.81.70.170<0.2<0.2<0.21.2013.22.5<0.2<0.24.70.60.60.8<0.1ASR1090.710.40.860<0.20.6<0.21.123.90.4<0.2<0.25.03.30.31.1<0.1RB-09-239-0018.85.80.740<0.21.2<0.21.747.80.1<0.2<0.26.33.30.40.70.1RB-09-239-002

15.720.80.6500.41.2<0.25.2121.40.30.7<0.22.38.91.62.4<0.1RB-09-239-0030.51.70.690<0.20.3<0.20.685.60.3<0.2<0.23.91.5<0.21.1<0.1RB-09-239-004

0.21.50.760<0.20.3<0.21.678.00.6<0.2<0.27.68.30.23.1<0.1RB-09-239-0050.63.00.560<0.20.4<0.21.477.90.4<0.2<0.23.73.3<0.21.6<0.1RB-09-239-0063.65.60.880<0.20.7<0.23.3023.50.3<0.2<0.210.28.20.42.40.2RB-09-239-0071.31.60.220<0.20.8<0.21.494.70.3<0.2<0.210.33.1<0.22.4<0.1RB-09-239-0080.73.00.650<0.20.4<0.21.224.20.2<0.2<0.23.23.4<0.21.8<0.1RB-09-239-009

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14192.017<126<20.2356<0.3<153RB-09-226-002273164.133<15130.28410<0.3<153RB-09-226-003159742.523<19230.78613<0.3<1114RB-09-226-004

105872.826<112720.75612<0.3<1129RB-09-226-005129542.219<110830.75512<0.3<1112RB-09-226-006147512.724<19620.80411<0.3<1124RB-09-226-0075250.87<125<20.2773<0.3<1145RB-09-227-0013130.55<113<20.0802<0.3<1104RB-09-227-002

12141.813<114<20.1466<0.3<190RB-09-227-003113101.616<159<20.5508<0.3<1241RB-09-227-00415791.615<17030.84212<0.3<1315RB-09-227-00510081.413<142<20.5859<0.3<1228RB-09-227-00619491.715<15320.79516<0.3<1148RB-09-227-007

4140.55<121<20.1172<0.3<1144RB-09-227-0084660.87<131<20.2454<0.3<1150RB-09-227-009

26793.830<13330.26411<0.3<147RB-09-228-0016040.77<125<20.2088<0.3<1140RB-09-228-00292723.436<1111300.73213<0.3<1111RB-09-228-003

24731.413<11620.23025<0.31166ASR209116703.744<111740.82812<0.3<1127RB-09-228-00485221.114<142<20.5238<0.3<1204RB-09-228-0053030.54<112<20.0702<0.3<186RB-09-228-0064940.76<127<20.2273<0.3<185RB-09-228-007

16181.513<147<20.87810<0.3<1131RB-09-228-0085751.010<135<20.4189<0.3<1186RB-09-228-0096840.88<125<20.2276<0.3<1165RB-09-228-0104250.65<12440.2004<0.3<1134RB-09-229-0012840.76<11280.0482<0.3<1124RB-09-229-002

170762.321<18720.82514<0.3<170RB-09-229-003146563.027<19420.84213<0.3<1126RB-09-229-004141623.024113960.93813<0.3<1169RB-09-229-0053240.66<114<20.0872<0.3<185RB-09-229-0063430.44<113<20.1602<0.3<174RB-09-229-007

15872.421<13931.7826<0.3192RB-09-229-0084130.44<113<20.1082<0.3<1127RB-09-229-0095560.910<12720.2566<0.3<1122RB-09-229-01058140.88<134<20.3484<0.3<1131RB-09-230-0013430.44<113<20.1642<0.3<174RB-09-229-007 R

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133744.239<113150.99814<0.3<1267RB-09-230-0063930.55<115<20.1073<0.3<1139RB-09-230-007

183662.925<18930.91815<0.3<1130RB-09-230-0085040.65<127<20.1915<0.3<1108RB-09-230-0095750.76<129<20.4396<0.3<1102RB-09-230-010

18862.923<128<20.1507<0.3<1167RB-09-230-011203673.937<19541.0413<0.3<1243RB-09-230-0128770.86<142<20.4884<0.3<1112RB-09-230-0134070.87<122<20.1953<0.3<197RB-09-230-0143540.54<117<20.1143<0.3<163RB-09-230-015

117141.511<110920.5797<0.3<187RB-09-230-0168840.76<116<20.4013<0.3<175RB-09-230-017

148101.412<151<20.8477<0.3<1123RB-09-230-01865492.218<117640.7268<0.3<1357RB-09-230-019

161242.119<19820.61113<0.3<1212RB-09-231-001

26121.412<11630.22627<0.3<1165ASR2097491.415<159<20.39010<0.31105RB-09-231-002

168543.124<112050.95615<0.3<1144RB-09-231-003145623.128<110430.86616<0.3<1142RB-09-231-00454121.011<13240.2058<0.3<190RB-09-231-005

3540.65<118<20.0752<0.3<1122RB-09-231-00611391.212<127<20.94013<0.3<182RB-09-231-0074440.64<119<20.2023<0.3<186RB-09-231-0085340.75<119<20.1564<0.3<189RB-09-231-009

117182.016<176<20.4887<0.3<166RB-09-232-001

192342.623<169<20.6409<0.3<184RB-09-232-002155642.723<187<20.7389<0.3<182RB-09-232-003125703.025<1106<20.73011<0.3<1110RB-09-232-004110563.030<1100<20.70411<0.3<1147RB-09-232-005112653.426<114240.86316<0.3<1122RB-09-232-006

119713.226<114220.86313<0.3<1118RB-09-232-0075371.010<141160.3594<0.3<1209RB-09-232-0085961.09<13770.2716<0.3<1194RB-09-232-0095250.75<124<20.4103<0.3<1112RB-09-232-010

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150524.138<113680.95214<0.3<1144RB-09-232-013203533.840<110880.91616<0.3<1193RB-09-232-014

70101.312<140<20.3566<0.3<1239RB-09-232-0154460.55<116<20.1143<0.3<152RB-09-233-001

160702.620<1112110.84411<0.3<148RB-09-233-002224113.224<129<20.29910<0.3<1234RB-09-233-00395232.528<138<20.39360.9<194RB-09-233-004

123812.825<111820.76411<0.3<196RB-09-233-005150432.319<178<20.6158<0.3<197RB-09-233-006113753.028<112120.72111<0.3<1118RB-09-233-007154502.922<112530.86912<0.3<1103RB-09-233-0084140.43<115<20.1724<0.3<171RB-09-234-001

4660.76<117<20.1994<0.3<157RB-09-234-0023540.43<110<20.0662<0.3<165RB-09-234-003

128762.824<113020.78111<0.3<173RB-09-234-004131152.022<147<20.716110.4<1110RB-09-234-005305104.637<14420.36112<0.3<157RB-09-234-006

27221.512<11630.23127<0.3<1168ASR209150592.620<19020.73310<0.3<174RB-09-234-0074070.54<11820.1383<0.3<163RB-09-234-008

178312.218<16040.6429<0.3<197RB-09-235-0013950.54<114<20.1162<0.3<171RB-09-235-002

153151.413<13830.96818<0.3159RB-09-235-003117742.723<112520.78910<0.3<156RB-09-235-004146252.018<159<20.55210<0.3<1120RB-09-235-005269124.839<149<20.29411<0.3<168RB-09-235-006135762.825<110420.76610<0.3<1100RB-09-235-007

4290.54<11830.0792<0.3<176RB-09-236-001196542.621<19820.79812<0.3<159RB-09-236-002160673.531<113420.87515<0.3<177RB-09-236-003114111.815<144<20.4589<0.3<164RB-09-236-004130872.923<112430.80511<0.3<188RB-09-236-005

158342.116<167<20.6248<0.3<193RB-09-236-006117783.128<112320.75612<0.3<1126RB-09-236-0073790.88<120<20.1572<0.3<184RB-09-237-0014840.87<116<20.0843<0.3<1149RB-09-237-002

119783.129<112320.76712<0.3<1129RB-09-236-007 R

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104673.534<194<20.65510<0.3<198RB-09-238-001121582.825<1106<20.74011<0.3<1102RB-09-238-0026840.76<11720.2084<0.3<1104RB-09-238-003

6540.65<11620.2064<0.3<199RB-09-238-003 R


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Zinc in ppm (Zn)


0.91.60.18<0.2<0.2<0.21.2513.12.6<0.2<0.24.70.70.70.9<0.1ASR1094.04.00.51<0.20.3<0.23.528.90.2<0.2<0.22.21.50.21.30.2RB-09-226-0012.57.20.21<0.21.2<0.21.543.90.2<0.2<0.20.91.50.52.3<0.1RB-09-226-0025.813.50.99<0.20.5<0.22.095.20.2<0.2<0.22.83.40.54.8<0.1RB-09-226-003

57.928.21.05<0.22.4<0.23.7026.60.4<0.20.719.413.81.41.0<0.1RB-09-226-004

49.126.81.33<0.22.0<0.26.3041.00.20.20.55.813.61.94.3<0.1RB-09-226-00518.817.41.27<0.21.0<0.25.4726.20.3<0.20.63.17.41.62.4<0.1RB-09-226-00628.120.20.78<0.21.2<0.23.9151.00.2<0.20.520.610.11.41.9<0.1RB-09-226-0070.52.01.38<0.2<0.2<0.20.955.70.2<0.2<0.24.91.8<0.20.9<0.1RB-09-227-0010.72.30.30<0.2<0.2<0.21.124.40.3<0.2<0.23.42.80.22.8<0.1RB-09-227-002

0.61.90.31<0.2<0.2<0.22.578.70.7<0.2<0.221.58.10.211.60.2RB-09-227-0030.56.70.70<0.2<0.2<0.21.5315.90.4<0.2<0.217.47.70.42.9<0.1RB-09-227-0042.13.92.16<0.2<0.2<0.22.238.10.1<0.2<0.211.16.50.30.9<0.1RB-09-227-0050.84.80.68<0.20.5<0.21.846.30.4<0.20.41.93.10.80.6<0.1RB-09-227-0060.79.61.10<0.2<0.2<0.21.898.40.3<0.20.40.84.20.70.5<0.1RB-09-227-007

0.53.50.48<0.20.3<0.20.712.20.2<0.2<0.22.61.2<0.21.0<0.1RB-09-227-0080.57.10.61<0.20.2<0.21.136.90.3<0.20.22.93.30.51.6<0.1RB-09-227-0090.67.70.61<0.2<0.2<0.21.343.40.1<0.2<0.29.52.60.31.1<0.1RB-09-228-0011.17.01.00<0.2<0.2<0.21.153.10.2<0.2<0.24.72.30.52.2<0.1RB-09-228-002

26.114.213.3<0.21.0<0.24.9527.00.20.2<0.225.911.22.47.9<0.1RB-09-228-003

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1.24.51.19<0.20.4<0.22.5411.62.1<0.2<0.24.10.70.72.0<0.1ASR20928.626.71.900.20.9<0.25.5123.00.2<0.2<0.22.49.61.92.8<0.1RB-09-228-0049.211.10.48<0.20.2<0.21.938.70.2<0.2<0.28.23.80.91.5<0.1RB-09-228-0050.63.10.14<0.2<0.2<0.21.576.50.3<0.2<0.22.42.60.42.9<0.1RB-09-228-0060.74.40.23<0.2<0.2<0.23.0019.30.7<0.2<0.211.813.70.33.80.2RB-09-228-007

0.54.00.69<0.2<0.2<0.22.0712.70.2<0.2<0.25.13.80.31.0<0.1RB-09-228-008<0.12.60.50<0.2<0.2<0.21.395.30.3<0.2<0.27.14.50.22.00.2RB-09-228-009<0.11.90.34<0.20.3<0.24.147.20.5<0.2<0.211.69.20.313.10.4RB-09-228-010

1.86.62.36<0.2<0.2<0.21.064.00.1<0.2<0.221.54.00.31.0<0.1RB-09-229-0011.63.56.85<0.21.6<0.21.410.90.2<0.2<0.230.71.0<0.20.6<0.1RB-09-229-002

51.717.10.79<0.21.2<0.23.4829.60.4<0.20.422.814.21.31.8<0.1RB-09-229-00330.27.71.22<0.21.6<0.23.1325.70.2<0.2<0.230.110.81.21.0<0.1RB-09-229-00438.923.40.97<0.20.2<0.23.5240.70.3<0.20.563.415.22.28.3<0.1RB-09-229-0050.63.80.29<0.2<0.2<0.21.786.90.4<0.2<0.297.24.50.44.00.1RB-09-229-0060.91.80.21<0.2<0.2<0.21.024.80.3<0.2<0.210.13.4<0.22.0<0.1RB-09-229-007

0.85.21.28<0.2<0.2<0.24.1413.110.7<0.20.641810.93.613.00.6RB-09-229-0080.71.51.00<0.20.2<0.20.541.80.3<0.2<0.26.31.0<0.20.9<0.1RB-09-229-0090.65.21.94<0.20.2<0.21.453.40.2<0.2<0.20.71.20.40.3<0.1RB-09-229-0100.64.60.20<0.20.3<0.21.6633.25.0<0.2<0.23.127.61.04.0<0.1RB-09-230-0010.51.80.20<0.2<0.2<0.20.964.90.4<0.2<0.210.83.5<0.22.7<0.1RB-09-229-007 R

0.61.60.19<0.2<0.2<0.21.1813.32.6<0.2<0.24.70.70.70.8<0.1ASR10911.79.81.09<0.20.5<0.23.7919.40.2<0.20.32.48.11.21.8<0.1RB-09-230-0020.611.31.34<0.2<0.2<0.23.177.40.3<0.20.43.03.00.91.2<0.1RB-09-230-0030.611.60.86<0.2<0.2<0.21.842.70.4<0.20.32.11.70.60.7<0.1RB-09-230-0040.79.30.63<0.2<0.2<0.21.676.60.2<0.2<0.21.44.60.50.4<0.1RB-09-230-005

27.111.61.47<0.21.3<0.23.5983.20.2<0.20.67.618.41.31.1<0.1RB-09-230-0060.72.00.27<0.2<0.2<0.20.561.3<0.1<0.2<0.22.30.6<0.20.4<0.1RB-09-230-007

12.010.41.39<0.20.4<0.25.1414.20.3<0.20.41.56.81.4<0.2<0.1RB-09-230-0080.45.80.52<0.2<0.2<0.20.923.60.3<0.2<0.21.11.5<0.21.8<0.1RB-09-230-0090.45.40.58<0.2<0.2<0.20.903.80.2<0.2<0.21.21.20.31.0<0.1RB-09-230-010

0.38.00.57<0.20.3<0.21.184.00.2<0.2<0.21.51.10.41.8<0.1RB-09-230-01114.316.51.15<0.20.8<0.26.4913.10.3<0.20.71.68.21.51.5<0.1RB-09-230-0121.117.51.16<0.2<0.2<0.22.391.50.1<0.2<0.21.82.20.50.6<0.1RB-09-230-0130.39.10.58<0.2<0.2<0.21.336.50.2<0.2<0.21.66.30.41.1<0.1RB-09-230-0140.35.40.31<0.2<0.2<0.20.842.90.2<0.2<0.20.91.7<0.20.7<0.1RB-09-230-015

2.429.91.350.20.5<0.23.2211.30.2<0.20.40.84.00.90.5<0.1RB-09-230-0160.75.70.34<0.2<0.2<0.20.861.20.2<0.2<0.20.52.30.30.3<0.1RB-09-230-0170.515.60.74<0.20.5<0.22.141.70.2<0.20.20.81.20.50.5<0.1RB-09-230-018

20.313.82.29<0.23.4<0.25.411221.50.30.476.359.02.07.0<0.1RB-09-230-01911.434.31.16<0.2<0.2<0.25.0511.20.4<0.20.50.86.71.02.5<0.1RB-09-231-001

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0.94.61.21<0.20.4<0.22.6111.42.1<0.2<0.24.20.70.62.0<0.1ASR2090.825.41.090.2<0.2<0.22.383.1<0.1<0.2<0.21.04.50.61.9<0.1RB-09-231-002

14.310.71.33<0.20.2<0.22.4016.6<0.1<0.2<0.21.66.01.00.9<0.1RB-09-231-00323.38.30.94<0.21.2<0.22.5024.10.1<0.2<0.20.89.61.01.0<0.1RB-09-231-0040.911.72.44<0.2<0.2<0.23.583.30.4<0.2<0.24.92.71.12.0<0.1RB-09-231-005

0.86.70.64<0.20.2<0.21.232.50.4<0.2<0.26.01.20.41.8<0.1RB-09-231-0060.76.40.73<0.2<0.2<0.21.933.90.3<0.2<0.22.02.90.40.5<0.1RB-09-231-0070.55.80.40<0.2<0.2<0.21.013.70.3<0.2<0.21.51.40.41.2<0.1RB-09-231-0080.65.10.49<0.20.4<0.20.782.80.1<0.2<0.22.20.80.20.8<0.1RB-09-231-0092.834.60.34<0.2<0.2<0.21.583.80.2<0.2<0.210.83.50.61.9<0.1RB-09-232-001

9.521.20.560.3<0.2<0.22.3813.20.3<0.2<0.211.56.20.92.4<0.1RB-09-232-00238.823.51.11<0.21.6<0.25.2427.00.3<0.20.24.011.21.32.8<0.1RB-09-232-00332.422.01.15<0.21.4<0.25.2932.50.3<0.2<0.26.611.61.44.7<0.1RB-09-232-0049.817.91.63<0.21.1<0.24.7529.50.30.2<0.23.18.91.75.2<0.1RB-09-232-005

21.222.91.93<0.2<0.2<0.27.1141.90.4<0.20.71.910.21.72.0<0.1RB-09-232-006

32.918.20.77<0.21.4<0.24.271380.3<0.20.439.216.81.41.0<0.1RB-09-232-0070.66.011.2<0.20.2<0.21.4610.20.3<0.2<0.21396.20.24.40.1RB-09-232-0080.99.36.61<0.2<0.2<0.23.7811.20.5<0.20.44.63.40.91.7<0.1RB-09-232-0090.23.11.00<0.2<0.2<0.20.693.40.2<0.2<0.21.61.10.20.6<0.1RB-09-232-010

33.119.00.78<0.21.9<0.24.351400.3<0.20.740.117.31.81.3<0.1RB-09-232-007 R

0.91.70.20<0.2<0.2<0.21.0613.22.5<0.2<0.24.60.70.70.7<0.1ASR1090.44.10.86<0.2<0.2<0.20.954.30.2<0.2<0.21.81.70.30.5<0.1RB-09-232-0110.56.80.88<0.2<0.2<0.21.193.10.2<0.2<0.22.82.70.51.0<0.1RB-09-232-012

14.313.84.210.30.8<0.25.0140.50.3<0.20.4<0.18.41.41.9<0.1RB-09-232-01321.615.34.16<0.21.2<0.23.7654.90.3<0.20.40.812.61.22.0<0.1RB-09-232-014

0.87.30.93<0.20.3<0.21.756.60.2<0.2<0.23.43.90.40.9<0.1RB-09-232-0153.24.80.85<0.20.60.21.246.90.2<0.2<0.210.23.30.30.9<0.1RB-09-233-001

46.616.57.14<0.21.8<0.23.0844.60.2<0.20.224.114.21.12.4<0.1RB-09-233-0020.74.90.43<0.20.3<0.20.741.9<0.1<0.2<0.212.21.10.44.4<0.1RB-09-233-0030.610.00.390.70.6<0.21.299.8<0.10.2<0.23.54.71.34.7<0.1RB-09-233-004

47.725.71.72<0.22.2<0.26.7240.10.4<0.20.640.913.51.63.1<0.1RB-09-233-00521.821.90.57<0.20.6<0.23.5624.90.2<0.20.28.27.50.92.9<0.1RB-09-233-00635.427.41.15<0.21.1<0.24.7634.2<0.1<0.2<0.25.312.31.44.4<0.1RB-09-233-00713.130.91.270.30.6<0.27.2529.30.3<0.20.51.87.91.83.1<0.1RB-09-233-0080.64.80.75<0.2<0.2<0.21.324.00.2<0.2<0.25.42.90.30.70.3RB-09-234-001

2.12.50.71<0.20.4<0.20.914.5<0.1<0.2<0.21.91.3<0.20.4<0.1RB-09-234-0022.73.20.46<0.20.3<0.21.044.8<0.1<0.2<0.22.32.60.20.6<0.1RB-09-234-003

49.116.60.86<0.21.9<0.23.4443.30.20.20.227.713.81.42.0<0.1RB-09-234-0040.612.10.680.6<0.2<0.21.374.2<0.1<0.2<0.25.12.20.91.1<0.1RB-09-234-0051.39.30.50<0.2<0.2<0.20.932.1<0.1<0.2<0.24.70.80.30.6<0.1RB-09-234-006

3Page of 4








Revision 1


1.14.51.22<0.20.3<0.22.6611.82.1<0.2<0.24.00.70.61.5<0.1ASR20938.126.30.87<0.21.0<0.26.5129.50.3<0.20.44.910.91.32.7<0.1RB-09-234-0073.52.81.06<0.20.50.31.684.20.1<0.2<0.23.62.20.20.30.3RB-09-234-008

16.111.72.34<0.20.6<0.23.2313.50.3<0.2<0.210.15.90.93.5<0.1RB-09-235-0012.34.60.63<0.2<0.2<0.21.436.60.1<0.2<0.21.63.60.30.60.2RB-09-235-002

2.18.91.12<0.20.2<0.22.188.90.2<0.2<0.24.95.10.50.9<0.1RB-09-235-00348.422.80.81<0.21.1<0.25.4239.20.3<0.2<0.25.013.51.41.70.6RB-09-235-00413.412.60.50<0.20.8<0.21.6713.30.2<0.2<0.25.74.70.51.0<0.1RB-09-235-0050.57.10.51<0.2<0.2<0.20.722.80.1<0.2<0.21.61.00.31.6<0.1RB-09-235-006

43.424.50.84<0.22.1<0.27.4835.20.3<0.20.449.611.71.43.9<0.1RB-09-235-007

6.85.82.18<0.2<0.2<0.22.436.20.1<0.2<0.283.01.3<0.21.90.4RB-09-236-00135.020.30.58<0.22.2<0.22.8729.20.3<0.20.312.810.51.22.0<0.1RB-09-236-00235.210.90.83<0.21.8<0.23.3129.40.1<0.2<0.222.010.51.01.5<0.1RB-09-236-0030.717.90.820.30.4<0.21.252.50.2<0.2<0.23.62.10.61.6<0.1RB-09-236-004

52.722.71.84<0.21.9<0.26.1243.80.1<0.20.532.215.51.31.9<0.1RB-09-236-005

16.420.20.69<0.20.8<0.23.7813.70.2<0.2<0.22.45.70.92.5<0.1RB-09-236-00634.421.41.16<0.21.8<0.25.3835.0<0.1<0.2<0.25.412.21.33.4<0.1RB-09-236-0070.64.21.220.5<0.2<0.23.9310.44.5<0.2<0.240.13.91.915.90.1RB-09-237-0010.61.20.41<0.2<0.2<0.21.615.60.3<0.2<0.27.23.80.34.0<0.1RB-09-237-002

35.122.31.01<0.21.2<0.25.3236.00.20.2<0.25.612.51.33.6<0.1RB-09-236-007 R

0.81.80.17<0.2<0.20.21.1113.52.6<0.2<0.24.60.70.71.0<0.1ASR1090.82.40.24<0.2<0.2<0.21.496.50.4<0.2<0.26.65.00.35.0<0.1RB-09-237-003

22.721.90.560.70.5<0.24.6140.50.30.2<0.216.79.41.94.7<0.1RB-09-238-00126.817.40.690.31.6<0.23.9253.80.2<0.2<0.221.611.21.31.6<0.1RB-09-238-0020.72.51.04<0.2<0.2<0.22.9213.51.4<0.2<0.222.24.80.34.40.4RB-09-238-003

0.82.31.09<0.2<0.2<0.22.8712.71.4<0.2<0.221.64.50.54.10.4RB-09-238-003 R


4Page of 4












Zinc in ppm (Zn)

1Page of 5









0.81.70.160.4<0.2<0.20.9713.02.4<0.2<0.24.60.70.70.8<0.1ASR1099.221.10.540.80.6<0.24.014.4<0.1<0.2<0.23.03.10.54.9<0.1R2920

11.322.70.790.51.1<0.20.936.50.1<0.2<0.22.53.70.72.3<0.1R292116.116.42.450.41.4<0.20.9811.10.1<0.2<0.220.34.80.71.8<0.1R292212.315.82.330.70.4<0.20.496.0<0.1<0.2<0.213.03.11.01.9<0.1R2923

7.66.21.66<0.2<0.2<0.20.442.00.1<0.2<0.25.61.60.51.8<0.1R29246.56.21.750.4<0.2<0.20.601.6<0.1<0.2<0.216.31.30.41.4<0.1R29254.31.40.92<0.2<0.2<0.22.115.60.2<0.2<0.210.73.90.215.4<0.1R29265.44.51.150.3<0.2<0.22.215.50.2<0.2<0.221.65.40.32.0<0.1R29272.63.81.120.50.5<0.20.873.20.2<0.2<0.24.43.20.40.3<0.1R2928

4.13.80.400.3<0.2<0.21.021.5<0.1<0.2<0.27.71.90.31.1<0.1R29294.56.80.320.5<0.2<0.20.221.50.1<0.2<0.210.71.30.41.7<0.1R29304.89.30.950.50.4<0.21.945.00.3<0.2<0.28.74.10.810.60.4R2931

22.513.63.070.81.1<0.21.1315.5<0.1<0.2<0.230.27.41.02.90.1R293258.427.41.281.73.5<0.21.3532.0<0.1<0.20.229.014.51.91.00.2R2933

46.523.82.052.13.0<0.220.143.50.30.20.413233.12.91451.1R293432.216.74.990.82.6<0.210.628.1<0.1<0.2<0.225.918.91.523.30.6R293510.414.51.210.60.4<0.23.257.7<0.1<0.2<0.219.84.60.71.3<0.1R293631.813.10.840.72.3<0.24.6329.2<0.10.2<0.222.313.31.42.40.3R293748.813.53.611.13.1<0.25.7453.4<0.10.3<0.280.022.81.93.50.5R2938

1.34.61.190.5<0.2<0.22.6711.41.9<0.2<0.24.50.80.71.8<0.1ASR20910.08.01.150.3<0.2<0.20.826.1<0.1<0.2<0.226.33.40.42.0<0.1R293942.811.96.991.42.4<0.22.8132.8<0.10.3<0.240.812.41.82.9<0.1R294042.314.71.931.42.2<0.21.5033.5<0.10.2<0.223.010.51.41.1<0.1R294142.721.91.851.82.9<0.22.2833.1<0.10.3<0.232.411.12.14.0<0.1R2942

10.43.22.800.20.4<0.20.602.6<0.1<0.2<0.213.42.80.20.6<0.1R294314.92.52.590.2<0.2<0.20.822.8<0.1<0.2<0.218.03.10.31.70.2R294419.68.813.40.31.2<0.23.0816.8<0.1<0.2<0.287.28.60.63.50.2R29455.35.62.370.3<0.2<0.20.501.50.2<0.2<0.213.72.10.41.6<0.1R29465.04.211.6<0.2<0.20.30.611.4<0.1<0.2<0.226.61.10.51.7<0.1R2947

48.916.41120.72.6<0.26.4334.4<0.1<0.2<0.22309.20.93.1<0.1R294852.117.91.601.92.5<0.21.0225.6<0.10.3<0.225.713.41.72.10.1R294945.115.81.141.32.6<0.20.6924.1<0.10.30.222.811.81.60.8<0.1R295039.917.21.221.33.3<0.20.9222.7<0.1<0.2<0.224.411.92.01.3<0.1R295127.715.81.811.31.9<0.20.8815.60.1<0.2<0.227.68.71.21.8<0.1R2952

11.715.31.131.10.6<0.20.185.8<0.1<0.2<0.216.64.50.81.2<0.1R29534.22.42.280.3<0.2<0.21.123.20.3<0.2<0.263.93.7<0.23.40.2R29543.63.61.150.6<0.2<0.22.524.61.1<0.2<0.239.37.20.410.60.4R29553.14.02.120.80.8<0.21.032.7<0.1<0.20.27.21.60.51.0<0.1R2956

27.215.81.731.42.4<0.20.8315.5<0.1<0.2<0.226.38.71.21.5<0.1R2952 R

2Page of 5









0.81.70.200.3<0.2<0.20.9613.42.6<0.2<0.24.60.70.70.7<0.1ASR1092.95.41.730.90.4<0.23.401.90.3<0.20.215.22.00.80.4<0.1R29574.62.90.220.3<0.2<0.20.391.9<0.1<0.2<0.24.41.40.20.8<0.1R29587.98.60.690.60.6<0.21.0912.8<0.1<0.2<0.24.85.30.40.5<0.1R29595.86.10.270.4<0.2<0.21.571.6<0.1<0.2<0.23.94.30.41.8<0.1R2960

6.06.70.420.4<0.2<0.20.384.4<0.1<0.2<0.21.73.80.30.4<0.1R29615.25.20.370.3<0.2<0.20.352.00.1<0.2<0.21.23.2<0.20.5<0.1R29627.125.51.211.1<0.2<0.22.843.50.1<0.2<0.23.15.40.62.0<0.1R29638.311.80.500.5<0.2<0.22.004.1<0.1<0.2<0.21.66.20.51.9<0.1R2964

10.416.42.540.7<0.2<0.23.364.4<0.1<0.2<0.22.99.40.82.9<0.1R2965

25.820.40.283.3<0.2<0.20.2737.0<0.10.4<0.225.29.22.35.00.2R296634.124.70.922.41.0<0.22.3190.8<0.10.3<0.289.411.32.36.3<0.1R296735.319.10.511.81.8<0.22.71115<0.1<0.20.344.113.51.81.8<0.1R296835.518.90.831.32.2<0.22.4782.5<0.1<0.2<0.239.512.41.40.8<0.1R296936.218.60.581.42.4<0.24.74113<0.10.20.371.829.31.92.1<0.1R2970

37.517.71.351.32.9<0.23.5593.20.20.20.310130.02.06.90.5R29715.65.610.31.00.5<0.25.4721.00.8<0.2<0.217313.20.956.50.7R29725.44.84.470.7<0.2<0.23.469.90.5<0.2<0.21608.90.521.20.6R29735.74.32.440.4<0.2<0.22.186.80.2<0.2<0.21074.10.23.40.1R29746.47.81.960.5<0.2<0.22.939.00.3<0.2<0.21098.10.56.50.2R2975

1.34.71.220.30.5<0.22.5811.11.9<0.2<0.24.60.70.71.9<0.1ASR2095.35.113.10.30.5<0.22.3212.70.2<0.2<0.21099.40.32.20.2R29765.65.012.10.3<0.2<0.22.4013.60.2<0.2<0.22188.20.33.00.2R29774.83.22.620.5<0.2<0.20.674.4<0.1<0.2<0.23.52.00.31.7<0.1R29784.83.60.540.4<0.2<0.20.184.50.1<0.2<0.23.82.90.31.1<0.1R2979

6.49.51.200.80.2<0.20.878.6<0.1<0.2<0.212.55.10.62.7<0.1R298013.516.01.970.70.4<0.20.282.8<0.1<0.2<0.257.43.60.40.6<0.1R298111.47.34.180.60.3<0.20.553.7<0.1<0.2<0.21952.80.40.8<0.1R298219.113.67.400.50.7<0.20.229.0<0.1<0.2<0.216.55.70.40.9<0.1R29834.34.80.580.4<0.2<0.20.652.10.2<0.2<0.23.32.60.31.2<0.1R2984

4.45.40.690.5<0.2<0.20.902.20.1<0.2<0.23.52.20.41.0<0.1R29853.68.11.330.7<0.2<0.21.702.90.2<0.2<0.22.61.80.40.9<0.1R29864.37.20.980.7<0.2<0.21.143.00.2<0.2<0.22.52.50.51.4<0.1R29874.24.50.860.5<0.2<0.20.812.8<0.1<0.2<0.22.82.20.30.9<0.1R29884.44.81.110.6<0.2<0.21.356.0<0.1<0.2<0.21.42.30.51.2<0.1R2989

19.610.34.401.01.8<0.21.9141.7<0.1<0.2<0.20.37.91.01.6<0.1R29905.77.01.080.7<0.2<0.21.272.7<0.1<0.2<0.23.43.10.40.4<0.1R29916.26.71.340.60.5<0.21.583.2<0.1<0.2<0.23.13.40.40.5<0.1R29925.911.02.861.0<0.2<0.21.962.9<0.1<0.2<0.23.03.10.60.4<0.1R2993

20.011.14.331.21.7<0.21.9742.2<0.1<0.2<0.20.38.21.21.8<0.1R2990 R

3Page of 5









0.71.90.17<0.2<0.2<0.21.1813.92.7<0.2<0.24.60.70.80.8<0.1ASR1093.16.31.16<0.20.3<0.21.9914.20.1<0.2<0.210.03.70.51.00.2R29943.310.01.12<0.20.2<0.22.178.10.2<0.2<0.216.04.90.42.10.2R29950.616.80.480.7<0.2<0.230.760.58.1<0.210.563674.82.946.52.7R2996

17.112.20.60<0.2<0.2<0.21.9710.40.2<0.2<0.228.35.60.62.8<0.1R2997

22.110.40.72<0.21.2<0.21.7112.50.1<0.2<0.24.66.00.41.4<0.1R29984.57.90.57<0.2<0.2<0.21.274.30.2<0.2<0.25.72.40.50.8<0.1R29993.811.60.87<0.2<0.2<0.21.474.8<0.1<0.2<0.214.03.00.61.4<0.1R30000.79.40.92<0.2<0.2<0.21.221.80.2<0.2<0.29.51.80.31.0<0.1R39010.56.50.67<0.2<0.2<0.20.892.00.2<0.2<0.210.21.70.20.9<0.1R3902

0.86.00.85<0.2<0.2<0.20.661.60.1<0.2<0.210.21.6<0.20.9<0.1R39031.15.20.74<0.2<0.2<0.20.841.80.1<0.2<0.28.61.70.21.3<0.1R39040.97.00.90<0.20.2<0.20.841.70.1<0.2<0.27.31.5<0.21.0<0.1R3905

56.220.21.22<0.21.9<0.24.4035.00.3<0.20.623.614.61.61.1<0.1R390654.023.51.22<0.21.5<0.24.0528.80.4<0.20.423.711.81.60.9<0.1R3907

48.016.10.93<0.20.9<0.23.2322.80.3<0.20.327.610.61.10.7<0.1R390851.116.70.91<0.21.5<0.23.9929.20.2<0.20.423.412.51.31.2<0.1R390946.817.10.97<0.21.1<0.23.5923.70.2<0.20.315.112.41.11.1<0.1R39100.78.30.29<0.2<0.2<0.20.902.40.2<0.2<0.217.93.00.51.0<0.1R3911

37.415.60.77<0.21.0<0.24.7133.00.2<0.20.417.316.61.70.6<0.1R3912

1.04.71.19<0.2<0.2<0.22.5212.02.0<0.2<0.24.10.70.81.9<0.1ASR20923.210.21.22<0.20.9<0.22.3920.10.2<0.2<0.234.46.60.80.9<0.1R39135.013.90.56<0.20.4<0.21.184.20.2<0.2<0.247.73.80.61.8<0.1R3914

12.216.11.13<0.20.8<0.22.309.90.3<0.20.262.89.71.01.0<0.1R391544.821.21.24<0.21.3<0.24.3025.80.4<0.20.621.711.31.61.6<0.1R3916

51.320.71.22<0.21.7<0.24.1727.20.4<0.20.621.313.41.31.4<0.1R391750.720.21.07<0.21.2<0.24.2528.80.4<0.20.620.014.01.62.0<0.1R391840.217.01.29<0.22.1<0.23.6424.20.3<0.20.525.613.11.61.0<0.1R39190.84.54.69<0.2<0.2<0.21.474.30.2<0.2<0.212.01.70.31.1<0.1R39200.94.14.54<0.2<0.2<0.20.883.00.2<0.2<0.210.11.60.31.5<0.1R3921

1.222.81.61<0.2<0.2<0.22.326.10.8<0.20.43.94.41.11.6<0.1R39220.58.42.070.4<0.2<0.22.154.10.3<0.2<0.24.14.50.61.4<0.1R3923

15.410.85.29<0.20.8<0.24.1454.80.3<0.20.51.110.81.43.2<0.1R392412.910.45.62<0.21.0<0.23.7146.20.4<0.20.70.912.81.94.2<0.1R392513.318.24.710.2<0.2<0.24.7834.40.5<0.21.2<0.111.12.30.9<0.1R3926

17.413.33.26<0.21.0<0.23.9034.90.4<0.20.70.410.81.70.9<0.1R392723.219.13.43<0.20.8<0.25.8837.70.4<0.20.65.714.31.93.5<0.1R392830.816.62.07<0.20.8<0.24.8841.30.2<0.2<0.22.615.11.41.8<0.1R392931.013.43.32<0.21.6<0.24.1937.70.2<0.2<0.21.013.51.81.60.4R393023.221.83.25<0.20.7<0.25.9737.40.4<0.20.65.514.71.94.1<0.1R3928 R

4Page of 5









0.81.70.18<0.2<0.20.21.1913.52.5<0.2<0.24.50.70.60.7<0.1ASR10932.213.62.42<0.21.6<0.24.2539.50.2<0.2<0.20.813.31.3<0.2<0.1R39310.731.40.640.3<0.2<0.21.033.30.2<0.2<0.25.61.90.30.9<0.1R3932

51.432.70.96<0.21.9<0.24.9762.60.3<0.20.54.817.21.51.7<0.1R39330.844.02.760.50.8<0.22.944.00.3<0.2<0.25.64.70.31.00.1R3934

0.226.43.850.30.3<0.21.762.90.2<0.2<0.27.43.1<0.20.60.1R39350.526.17.43<0.20.40.21.372.30.1<0.2<0.28.22.8<0.2<0.2<0.1R3936

36.212.80.37<0.20.6<0.21.642.50.3<0.20.37.96.10.71.0<0.1R39370.599.85.621.41.51.011.97.00.2<0.20.347.312.7<0.23.20.7R3938

50.026.80.76<0.21.3<0.25.4480.40.3<0.20.713.119.71.60.7<0.1R3939

62.926.04.01<0.22.0<0.22.9557.20.2<0.20.450.120.40.92.0<0.1R39409.612.40.25<0.20.9<0.22.627.60.7<0.20.313.62.50.95.6<0.1R3941

30.816.90.75<0.20.6<0.21.6017.40.2<0.20.23.710.90.41.0<0.1R394220.512.80.93<0.20.7<0.21.1615.00.2<0.2<0.215.68.00.30.70.2R394355.830891.53.88.71.322.644.40.4<0.21.2107026.20.410.80.8R3944

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85.5148140.101403710.57<10.0462.2583473.861.1R390665.5148150.092383720.85<10.0542.2187503.911.2R3907

55.9129140.087293911.16<10.0571.9170553.811.1R390875.4148160.087393611.03<10.0502.0784494.041.1R390956.21210150.088294021.41<10.0541.9175553.961.2R3910

<12.22270.0422921.21<10.0951.2016122.140.4R391166.5139170.099404030.51<10.0371.7690514.441.4R3912

22.41370.04712155<0.0120.0040.0397220.2220.6ASR20923.976140.049242541.01<10.0300.98371333.810.8R3913

<14.036150.05052242.02<10.1001.3427353.600.7R391425.6510150.073113671.99<10.0371.1641553.460.9R391585.9149140.083333950.81<10.0411.7677533.701.3R3916

85.4138140.082333560.83<10.0451.9679493.651.1R391786.0149140.119353950.80<10.0451.9887543.751.2R391866.91211150.089314451.06<10.0501.7582623.611.2R391913.334100.04281861.34<10.0380.6309243.090.8R3920

<11.91290.02851020.86<10.0190.3597142.63<0.4R3921

22.724190.056111531.9610.0500.66214233.450.4R3922<13.225160.05071831.70<10.0550.82410293.420.5R3923

97.02010220.146844430.63<10.0221.6195584.421.6R3924105.8207150.134743620.30<10.0281.9875474.421.3R3925117.91810200.240564630.64<10.0211.4685584.221.6R3926

97.71910170.214564520.48<10.0141.6486534.421.6R392788.91611170.246574920.79<10.0511.9289584.241.6R392877.31710200.160574430.63<10.0522.24107574.381.4R392996.8179160.152534120.56<10.0312.06103554.601.4R393098.91511180.242535030.78<10.0511.9187594.151.6R3928 R

9Page of 14









<11.2<1120.013145<1<0.0130.0040.0291070.044<0.4ASR10977.52011130.171634550.33<10.0282.29100625.421.6R3931

<12.52390.02241290.83<10.0980.1376162.300.5R393294.7167180.111793240.99<10.0482.1667403.161.2R3933

<11.912110.02451021.36<10.1271.474122.44<0.4R3934

<11.81380.02631461.19<10.0130.4624192.13<0.4R393511.412100.03131031.54<10.0080.4994142.71<0.4R3936

<11.62360.03231391.07<10.0300.59912181.230.5R3937<11.012250.02899111.03<10.0050.2307131.77<0.4R3938116.2238180.1381164070.20<10.0382.6388503.711.4R3939

55.3158120.093693441.78<10.0361.7164482.901.1R3940<12.02270.02591230.56<10.0550.87816161.60<0.4R3941

12.854100.048221851.88<10.0420.92228252.240.4R394212.74590.043171862.03<10.0340.63319262.090.5R394322.795510.0444920292.20<10.0291.0848262.480.9R3944

<11.622110.02211821.10<10.0620.5478112.05<0.4R3945<13.235120.040919121.79<10.1010.5849252.560.8R3946<12.836120.036622301.82<10.0911.416282.230.7R3947<11.912100.0246860.98<10.1570.7105112.37<0.4R3948<11.833120.022413111.22<10.0280.4889182.180.7R3949

12.41480.04813165<0.0130.0040.0407220.2090.5ASR209<11.82270.03211921.13<10.0430.2107121.75<0.4R3950<11.72270.03212821.12<10.0400.2067101.74<0.4R3950 R

10Page of 14









4610.32<1420.0282<0.3<140ASR109128142.118<16820.3967<0.3<177R2920175152.622<17820.3878<0.3<181R2921233202.020<17250.80730<0.3<1155R292255171.417<14650.3886<0.3<1177R2923

58101.010<13320.2975<0.3<1194R29245771.010<13420.3286<0.3<1149R29255340.86<114<20.0853<0.3<1114R2926

21181.816<15320.85814<0.3<1214R29274830.77<121<20.2124<0.3<1155R2928

4640.54<114<20.1323<0.3<1108R29294840.78<121<20.0923<0.3<1116R29309161.010<133<20.3528<0.3<1134R2931

109291.717<16150.46611<0.3<1154R2932191793.333<112140.94215<0.3<179R2933

138683.634<114260.90214<0.3<1121R2934111462.723<1118100.71213<0.3<1130R293591131.312<18720.3997<0.3<1147R2936

117482.423<110530.63411<0.3<1111R2937156773.430<115080.98315<0.3<1100R2938

25821.412<11620.225240.4<1161ASR209144121.313<15230.40814<0.3<1164R2939113813.841<1132140.84515<0.3<1164R2940113853.434<114350.83214<0.3<1121R2941101853.333<113140.75513<0.3<1126R2942

35130.55<11940.1383<0.3<1123R294341170.55<11640.1275<0.3<1131R294462291.010<155160.2635<0.3<1185R29453060.55<11840.0692<0.3<1125R29463160.66<113190.0472<0.3<1126R2947

134682.829<11171250.68011<0.3<1173R2948201802.927<1105110.85216<0.3<180R2949201632.622<19320.86015<0.3<182R2950308582.826<110440.91925<0.3<192R2951823394.23918371.11611.1<1141R2952

649193.332<16450.993490.8<1163R29535870.87<116<20.1423<0.3<1110R29546440.76<12120.3394<0.3<1123R29558551.010<12630.29811<0.3<1170R2956

812384.03717971.08510.9<1138R2952 R

11Page of 14









3810.32<14<20.0271<0.3<142ASR1096240.89<12320.4045<0.3<1158R29575350.77<120<20.3095<0.3<1163R2958

144152.018<154<20.72212<0.3<1282R29594680.66<119<20.1183<0.3<1145R2960

6270.89<138<20.2365<0.3<1140R29614360.78<136<20.1594<0.3<1136R2962

143102.226<16640.54015<0.31152R2963120121.413<145<20.47314<0.3<1190R2964100141.61515340.44714<0.3<1179R2965

54563.139<187<20.45580.6<1137R296690682.829<112630.71911<0.3<1200R2967

106703.231<114230.85212<0.3<1125R2968128653.331<113630.88813<0.3<1126R2969129613.232<112840.87914<0.3<1124R2970

132563.230<113860.92214<0.3<1143R29715780.99<128160.2254<0.3<1101R2972

12361.816<128110.3217<0.3<1103R297328893.528<12550.32716<0.3<178R2974223113.127<13660.60611<0.3194R2975

24921.211<11530.22525<0.31167ASR209133102.118<156210.4107<0.3<1160R2976122102.016<156190.4197<0.3<1172R29777971.111<12440.3037<0.3<1124R29784870.76<126<20.2633<0.3<1159R2979

4280.89<12620.2294<0.3176R298063141.010<13740.3357<0.3<1114R298152130.98<13650.2505<0.3<1114R298257230.98<14890.2975<0.3<1137R29835640.77<119<20.1724<0.3<1172R2984

5150.87<121<20.2325<0.3<1169R29855140.87<124<20.2516<0.3<1148R2986

10451.111<13530.61410<0.3<1125R29875650.88<125<20.3196<0.3<1225R2988

10471.415<13420.70413<0.3<1205R2989

123564.044<114590.93515<0.3<1172R29906470.911<130<20.4085<0.3<1128R2991

16381.515<13420.67113<0.3<1133R2992393102.526<16062.2834<0.33128R2993122564.045<114790.93414<0.3<1172R2990 R

12Page of 14









4110.32<14<20.0311<0.3<142ASR10970131.19<14520.6225<0.3<160R29947491.09<13130.3264<0.3<155R299512241.518<15870.03011.0<1<1R2996

167301.717<153<20.62812<0.3<1184R2997

134331.413<153<20.62510<0.3<1141R2998119151.211<138<20.4949<0.3<1144R2999223172.020<148<20.72518<0.31144R30003440.66<121<20.0973<0.3<1110R39013140.77<122<20.0883<0.3<1119R3902

3840.77<120<20.0743<0.3<1123R39033040.77<121<20.0893<0.3<1142R39043240.54<123<20.1173<0.3<1118R3905

146802.624<110340.80414<0.3<167R3906189812.623<111240.85217<0.3<175R3907

222682.423<18830.79218<0.3<191R3908206782.423<19230.84817<0.3<185R3909214672.424<18130.79018<0.3<1100R39106861.211<123<20.2073<0.3<170R391198603.133<110920.69715<0.3<177R3912

23821.313<11530.22424<0.3<1165ASR209112341.817<16330.4769<0.3<1100R3913140121.314<139<20.39813<0.3<1125R3914277192.020<15830.59120<0.3<1120R3915178672.828<110040.80815<0.3<199R3916

175712.322<19030.81316<0.3<194R3917171722.828<19220.83116<0.3<195R3918276602.725<17830.81423<0.3<1104R3919156102.219<12770.3339<0.3<196R39208341.09<11750.1864<0.3<1104R3921

5561.010<15520.2845<0.3<1209R392210361.111<12720.3819<0.3<1198R3923152433.735<1134100.96115<0.3<1380R3924121453.432<113290.86513<0.3<1210R3925134413.841<112370.90414<0.3<1305R3926

116463.736<112250.90114<0.3<1273R3927141503.336<111350.89716<0.3<1140R3928128603.232<112050.87817<0.3<1131R3929121623.131<111850.88316<0.3<1128R3930150503.336<111350.88317<0.3<1138R3928 R

13Page of 14









3710.32<14<20.0282<0.3<143ASR109115763.636<113450.92718<0.3<1138R39315570.87<185<20.7758<0.3175R3932

188813.026<114930.92113<0.3<1153R39336840.86<18140.2022<0.3<176R3934

8930.76<15440.6087<0.3<171R39358330.86<195100.3204<0.3<190R3936

164401.07<135<20.9867<0.3186R39375031.05<123180.5104<0.3<168R3938

1131033.534<115240.89613<0.3<1151R3939

189812.624<111280.92913<0.3<1137R3940101181.311<126<20.3454<0.3<176R394177411.09<159<20.4787<0.3<1105R394276281.08<155<20.45410<0.3<1106R394390643.324<17471130.67110<0.3<1124R3944

5670.76<136100.1883<0.3<165R394515081.713<1175110.94011<0.3<194R394612732.511<1682111.0812<0.3<184R394762180.97<1121<20.4184<0.3<168R3948

171111.310<14271.337<0.3184R3949

25821.312<11630.23827<0.3<1165ASR20940160.75<14820.2174<0.3<187R395043150.65<14720.2203<0.3<185R3950 R


14Page of 14

…A9

APPENDIX 9: 2009 PORTABLE INFRARED MINERAL ANALYSER (PIMA) RESULTS

Systematic Drill Core Sampling PIMA Results; 2009 Drilling Campaign

DDHNumber

SampleNumber

SpectralQuality

SpectralComments

Dominant Secondary Minor Trace TSA_A_Mineral1 TSA_A_Mineral2

RB-09-226 RB-09-226-001 fair -- kaolinite -- -- -- kaolinite null

RB-09-226 RB-09-226-002 fair -- illite (phengite) kaolinite -- -- phengite kaolinite

RB-09-226 RB-09-226-003 fair -- illite (phengite) -- -- kaolinite phengite null

RB-09-226 RB-09-226-004 good -- kaolinite montmorillonite -- -- kaolinite montmorillonite

RB-09-226 RB-09-226-005 fair -- illite (phengite) montmorillonite -- kaolinite montmorillonite phengite

RB-09-226 RB-09-226-006 fair -- montmorillonite illite -- kaolinite montmorillonite epidote

RB-09-226 RB-09-226-007 good -- montmorillonite kaolinite illite -- montmorillonite kaolinite

RB-09-227 RB-09-227-001 good -- kaolinite -- -- illite kaolinite null

RB-09-227 RB-09-227-002 fair -- kaolinite -- illite CO3 kaolinite dolomite

RB-09-227 RB-09-227-003 fair -- kaolinite -- -- illite kaolinite null

RB-09-227 RB-09-227-004 fair -- illite kaolinite -- -- illite kaolinite

RB-09-227 RB-09-227-005 fair -- kaolinite -- illite -- kaolinite null

RB-09-227 RB-09-227-006 good -- illite (muscovite) -- montmorillonite kaolinite muscovite montmorillonite

RB-09-227 RB-09-227-007 good -- illite (muscovite) kaolinite -- montmorillonite muscovite kaolinite

RB-09-227 RB-09-227-008 fair -- kaolinite illite -- montmorillonite kaolinite illite

RB-09-227 RB-09-227-009 good -- kaolinite illite -- montmorillonite kaolinite illite

RB-09-228 RB-09-228-001 good -- illite(phengite) kaolinite -- montmorillonite phengite kaolinite

RB-09-228 RB-09-228-002 good -- kaolinite -- illite -- kaolinite null

RB-09-228 RB-09-228-003 good -- montmorillonite kaolinite -- illite montmorillonite kaolinite

RB-09-228 RB-09-228-004 fair -- illite kaolinite montmorillonite -- illite null

RB-09-228 RB-09-228-005 good -- kaolinite montmorillonite illite -- kaolinite null






RB-09-229 RB-09-229-001 fair -- kaolinite illite (muscovite) montmorillonite -- kaolinite muscovite




RB-09-229 RB-09-229-005 good -- kaolinite illite(muscovite) -- montmorillonite kaolinite muscovite

RB-09-229 RB-09-229-006 good -- kaolinite -- -- -- kaolinite null

RB-09-229 RB-09-229-007 poor -- kaolinite -- illite -- halloysite null


RB-09-229 RB-09-229-009 poor -- illite (muscovite) kaolinite -- montmorillonite muscovite null


RB-09-230 RB-09-230-001 good -- kaolinite illite (muscovite) montmorillonite -- kaolinite muscovite


RB-09-230 RB-09-230-003 good -- kaolinite illite montmorillonite -- kaolinite Illite



RB-09-230 RB-09-230-006 good -- montmorillonite kaolinite illite -- illite kaolinite

RB-09-230 RB-09-230-007 good -- kaolinite illite (muscovite) -- -- kaolinite muscovite

Page 1 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-230 RB-09-230-008 good -- kaolinite montmorillonite -- illite kaolinite montmorillonite

RB-09-230 RB-09-230-009 good -- kaolinite illite -- montmorillonite kaolinite Illite

RB-09-230 RB-09-230-010 poor -- kaolinite -- illite -- kaolinite null

RB-09-230 RB-09-230-011 fair -- kaolinite (dickite) -- illite -- dickite null


RB-09-230 RB-09-230-013 poor -- illite CO3-calcite kaolinite -- calcite null

RB-09-230 RB-09-230-014 fair -- kaolinite illite -- -- kaolinite null

RB-09-230 RB-09-230-015 fair -- illite -- montmorillonite kaolinite illite null

RB-09-230 RB-09-230-016 good -- kaolinite montmorillonite illite -- kaolinite montmorillonite

RB-09-230 RB-09-230-017 poor -- illite montmorillonite -- -- illite null

RB-09-230 RB-09-230-017a fair lab replicate kaolinite illite -- -- halloysite null

RB-09-230 RB-09-230-018 fair -- kaolinite illite (phengite) -- -- kaolinite phengite

RB-09-230 RB-09-230-019 fair -- illite montmorillonite -- CO3 opal null

RB-09-231 RB-09-231-001 fair -- kaolinite -- -- montmorillonite kaolinite null








RB-09-231 RB-09-231-009 fair -- kaolinite illite (muscovite) -- -- kaolinite muscovite

RB-09-232 RB-09-232-001 fair -- illite (phengite) kaolinite -- montmorillonite phengite kaolinite

RB-09-232 RB-09-232-002 fair -- illite (muscovite) kaolinite CO3-calcite chlorite muscovite calcite

RB-09-232 RB-09-232-003 fair -- kaolinite illite CO3-ankerite -- halloysite ankerite

RB-09-232 RB-09-232-004 fair -- illite (muscovite) -- montmorillonite kaolinite muscovite null

RB-09-232 RB-09-232-005 good -- montmorillonite -- illite kaolinite montmorillonite null

RB-09-232 RB-09-232-006 poor -- montmorillonite -- kaolinite illite halloysite null

RB-09-232 RB-09-232-007 good -- montmorillonite -- kaolinite illite montmorillonite halloysite



RB-09-232 RB-09-232-010 fair -- illite (muscovite) kaolinite -- montmorillonite muscovite dickite



RB-09-232 RB-09-232-013 fair -- illite (phengite) -- kaolinite montmorillonite phengite halloysite

RB-09-232 RB-09-232-014 fair -- kaolinite illite montmorillonite -- kaolinite montmorillonite

RB-09-232 RB-09-232-015 good -- kaolinite illite montmorillonite -- kaolinite illite


RB-09-233 RB-09-233-002 fair -- illite (phengite) kaolinite montmorillonite -- phengite halloysite

RB-09-233 RB-09-233-003 fair -- illite kaolinite montmorillonite SO4-gypsum montmorillonite gypsum

RB-09-233 RB-09-233-004 very poor -- illite kaolinite -- montmorillonite zoisite null

RB-09-233 RB-09-233-005 poor -- illite (muscovite) -- kaolinite montmorillonite muscovite null

RB-09-233 RB-09-233-005a very poor lab replicate illite kaolinite montmorillonite -- aspectal null

Page 2 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-233 RB-09-233-006 noise no SWIR minerals -- -- -- -- aspectal null

RB-09-233 RB-09-233-006a noise lab replicate; no SWIR minerals -- -- -- -- aspectal null


RB-09-233 RB-09-233-008 fair -- kaolinite montmorillonite -- -- montmorillonite ankerite

RB-09-234 RB-09-234-001 good -- kaolinite -- -- -- kaolinite ankerite

RB-09-234 RB-09-234-002 good -- kaolinite -- illite montmorillonite kaolinite illite

RB-09-234 RB-09-234-003 fair -- kaolinite -- illite kaolinite null

RB-09-234 RB-09-234-004 poor -- illite -- kaolinite montmorillonite illite null

RB-09-234 RB-09-234-005 fair -- SO4-gypsum kaolinite -- illite gypsum kaolinite



RB-09-234 RB-09-234-007a poor lab replicate illite kaolinite montmorillonite -- aspectal null


RB-09-234 RB-09-234-008a noise lab replicate; no SWIR minerals -- -- -- -- aspectal null




RB-09-235 RB-09-235-004 poor -- illite (phengite) montmorillonite kaolinite -- phengite kaolinite

RB-09-235 RB-09-235-005 fair -- CO3-dolomite -- -- -- ankerite null

RB-09-235 RB-09-235-006 poor -- illite (phengite) -- kaolinite montmorillonite phengite null

RB-09-235 RB-09-235-006a fair lab replicate illite SO4-gypsum kaolinite -- illite gypsum

RB-09-235 RB-09-235-007 fair -- illite (muscovite) -- montmorillonite kaolinite opal muscovite


RB-09-236 RB-09-236-002 fair -- montmorillonite kaolinite illite -- illite null

RB-09-236 RB-09-236-003 fair -- montmorillonite illite kaolinite -- illite opal


RB-09-236 RB-09-236-005 fair -- montmorillonite illite (phengite) -- kaolinite montmorillonite phengite

RB-09-236 RB-09-236-006 noise no SWIR minerals -- -- -- -- aspectral null

RB-09-236 RB-09-236-006a noise lab replicate; no SWIR minerals -- -- -- -- aspectral null

RB-09-236 RB-09-236-007 fair -- illite (muscovite) montmorillonite -- kaolinite muscovite opal

RB-09-237 RB-09-237-001 fair -- kaolinite CO3-calcite illite -- kaolinite calcite


RB-09-237 RB-09-237-003 poor -- kaolinite montmorillonite illite -- aspectral null

RB-09-238 RB-09-238-001 poor -- montmorillonite kaolinite illite -- montmorillonite null

RB-09-238 RB-09-238-001a very poor lab replicate montmorillonite kaolinite illite -- tourmaline null

RB-09-238 RB-09-238-002 fair -- illite (muscovite) kaolinite -- montmorillonite muscovite kaolinite


RB-09-239 RB-09-239-001 good -- kaolinite -- illite montmorillonite kaolinite null

RB-09-239 RB-09-239-002 good -- kaolinite montmorillonite illite -- kaolinite Illite

RB-09-239 RB-09-239-003 poor -- kaolinite illite montmorillonite -- halloysite null

RB-09-239 RB-09-239-004 fair -- kaolinite illite -- -- kaolinite muscovite



Page 3 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-239 RB-09-239-007 fair -- kaolinite illite -- -- halloysite null





RB-09-239 RB-09-239-012 fair -- illite kaolinite -- montmorillonite illite kaolinite

RB-09-239 RB-09-239-013 fair -- kaolinite illite -- montmorillonite kaolinite Illite

RB-09-239 RB-09-239-014 fair -- kaolinite SO4-gypsum illite -- kaolinite gypsum

RB-09-239 RB-09-239-015 fair -- illite (muscovite) -- -- kaolinite muscovite null

RB-09-240 RB-09-240-001 good -- kaolinite illite -- montmorillonite kaolinite Illite

RB-09-240 RB-09-240-002 fair -- kaolinite montmorillonite illite -- montmorillonite halloysite

RB-09-240 RB-09-240-003 good -- montmorillonite kaolinite illite -- montmorillonite null

RB-09-240 RB-09-240-004 fair -- kaolinite illite -- -- halloysite calcite


RB-09-240 RB-09-240-006 poor -- kaolinite -- illite -- kaolinite null




RB-09-241 RB-09-241-001 fair -- kaolinite montmorillonite illite -- halloysite null

RB-09-241 RB-09-241-002 poor -- kaolinite montmorillonite illite (muscovite) -- muscovite null

RB-09-241 RB-09-241-002a poor lab replicate kaolinite montmorillonite illite (muscovite) -- muscovite null




RB-09-241 RB-09-241-006 fair -- kaolinite illite -- -- halloysite null



RB-09-241 RB-09-241-009 poor -- illite (muscovite) -- -- kaolinite muscovite null

RB-09-241 RB-09-241-009a fair lab replicate illite (muscovite) -- kaolinite -- muscovite kaolinite




RB-09-242 RB-09-242-002 good -- kaolinite -- illite -- kaolinite calcite

RB-09-242 RB-09-242-003 good -- kaolinite montmorillonite illite -- halloysite null


RB-09-242 RB-09-242-005 fair -- montmorillonite kaolinite illite -- montmorillonite kaolinite

RB-09-242 RB-09-242-006 good -- montmorillonite kaolinite illite -- montmorillonite halloysite


RB-09-242 RB-09-242-008 very poor -- kaolinite illite -- -- aspectral null

RB-09-242 RB-09-242-008a fair lab replicate kaolinite illite -- -- kaolinite null

RB-09-243 RB-09-243-001 fair -- illite (muscovite) -- -- kaolinite muscovite null

RB-09-243 RB-09-243-002 good -- kaolinite montmorillonite illite -- halloysite null

RB-09-243 RB-09-243-003 fair -- kaolinite illite -- montmorillonite halloysite null

Page 4 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-243 RB-09-243-004 fair -- kaolinite illite -- montmorillonite kaolinite null

RB-09-243 RB-09-243-005 fair -- montmorillonite kaolinite -- illite montmorillonite null

RB-09-243 RB-09-243-006 good -- kaolinite illite (muscovite) -- -- kaolinite muscovite


RB-09-243 RB-09-243-008 poor -- kaolinite illite -- -- aspectral null

RB-09-243 RB-09-243-008a poor lab replicate kaolinite illite -- -- muscovite null

RB-09-243 RB-09-243-009 poor -- illite kaolinite -- -- nacrite null

RB-09-243 RB-09-243-009a very poor lab replicate illite kaolinite -- -- opal null

RB-09-243 RB-09-243-010 poor -- illite kaolinite -- -- aspectral null

RB-09-243 RB-09-243-010a poor lab replicate illite kaolinite -- -- halloysite null

RB-09-243 RB-09-243-011 poor -- illite kaolinite -- -- halloysite null






RB-09-244 RB-09-244-005 noise no SWIR minerals -- -- -- aspectral null

RB-09-244 RB-09-244-005a very poor lab replicate montmorillonite -- kaolinite illite montmorillonite null

RB-09-245 RB-09-245-001 very poor -- montmorillonite -- illite kaolinite montmorillonite null

RB-09-245 RB-09-245-001a poor lab replicate CO3-ankerite -- illite -- ankerite null

RB-09-245 RB-09-245-002 good -- illite (phengite) -- montmorillonite kaolinite phengite illite

RB-09-245 RB-09-245-003 fair -- montmorillonite illite kaolinite -- montmorillonite null

RB-09-245 RB-09-245-004 poor -- illite (phengite) -- kaolinite -- phengite halloysite

RB-09-245 RB-09-245-004a poor lab replicate illite -- kaolinite -- dickite null

RB-09-245 RB-09-245-005 fair -- montmorillonite kaolinite illite -- montmorillonite null

RB-09-245 RB-09-245-006 poor -- illite (muscovite) -- kaolinite CO3-dolomite muscovite dolomite

RB-09-245 RB-09-245-006a very poor lab replicate; no SWIR minerals -- -- -- -- aspectral null


RB-09-245 RB-09-245-008 fair -- kaolinite -- illite -- dickite null


RB-09-245 RB-09-245-010 good -- kaolinite -- illite -- kaolinite illite


RB-09-245 RB-09-245-012 poor -- kaolinite -- -- illite kaolinite null

RB-09-245 RB-09-245-013 fair -- montmorillonite illite (muscovite) -- kaolinite montmorillonite muscovite

RB-09-245 RB-09-245-014 fair -- illite CO3-dolomite -- kaolinite illite dolomite

RB-09-245 RB-09-245-015 fair -- illite -- kaolinite montmorillonite illite null

RB-09-246 RB-09-246-001 fair -- montmorillonite kaolinite CO3-dolomite -- montmorillonite dolomite


RB-09-246 RB-09-246-003 fair -- illite kaolinite montmorillonite -- opal illite

RB-09-246 RB-09-246-004 fair -- illite montmorillonite kaolinite -- montmorillonite brucite

RB-09-246 RB-09-246-005 fair -- kaolinite CO3-dolomite illite -- dolomite kaolinite

RB-09-246 RB-09-246-006 poor -- kaolinite illite montmorillonite -- kaolinite null

RB-09-246 RB-09-246-006a very poor lab replicate illite kaolinite -- montmorillonite null null

Page 5 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments



RB-09-246 RB-09-246-008 poor -- illite (phengite) -- montmorillonite kaolinite phengite null

RB-09-246 RB-09-246-008a very poor lab replicate illite (phengite) -- kaolinite montmorillonite aspectral null

RB-09-246 RB-09-246-009 fair -- montmorillonite illite kaolinite -- montmorillonite null


RB-09-246 RB-09-246-011 fair -- montmorillonite illite -- -- montmorillonite null

RB-09-247 RB-09-247-001 good -- kaolinite CO3-calcite -- illite kaolinite calcite

RB-09-247 RB-09-247-002 fair -- kaolinite -- illite CO3 kaolinite null

RB-09-247 RB-09-247-003 poor -- illite kaolinite montmorillonite -- opal null

RB-09-247 RB-09-247-003a very poor lab replicate kaolinite illite -- tourmaline null


RB-09-248 RB-09-248-001 fair -- montmorillonite illite -- kaolinite montmorillonite null

RB-09-248 RB-09-248-002 fair -- montmorillonite illite kaolinite CO3-ankerite montmorillonite ankerite

RB-09-248 RB-09-248-003 fair -- illite montmorillonite -- kaolinite illite null

RB-09-248 RB-09-248-004 very poor -- -- -- kaolinite illite aspectral null




RB-09-248 RB-09-248-007 good -- kaolinite illite montmorillonite -- kaolinite montmorillonite

RB-09-248 RB-09-248-008 poor -- kaolinite montmorillonite illite -- montmorillonite null


RB-09-248 RB-09-248-009 fair -- illite (phengite) -- -- kaolinite phengite null

RB-09-248 RB-09-248-010 fair -- montmorillonite illite -- -- opal null

RB-09-248 RB-09-248-011 fair -- montmorillonite illite -- -- montmorillonite brucite

RB-09-248 RB-09-248-012 fair -- montmorillonite illite -- kaolinite montmorillonite brucite

RB-09-248 RB-09-248-013 fair -- illite montmorillonite -- CO3-ankerite montmorillonite ankerite

RB-09-249 RB-09-249-001 very poor -- kaolinite illite -- montmorillonite halloysite null

RB-09-249 RB-09-249-001a very poor lab replicate kaolinite illite -- montmorillonite montmorillonite null






RB-09-249 RB-09-249-007 poor -- montmorillonite -- kaolinite -- montmorillonite null

RB-09-249 RB-09-249-007a poor lab replicate montmorillonite -- kaolinite -- montmorillonite null

RB-09-249 RB-09-249-008 fair -- montmorillonite -- illite -- montmorillonite null

RB-09-249 RB-09-249-009 good -- montmorillonite CO3-calcite illite -- montmorillonite calcite

RB-09-250 RB-09-250-001 very poor -- montmorillonite -- kaolinite illite montmorillonite null




RB-09-250 RB-09-250-004 very poor -- illite kaolinite -- -- aspectral null

RB-09-250 RB-09-250-005 poor -- kaolinite illite -- -- kaolinite null

Page 6 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-250 RB-09-250-005a poor lab replicate kaolinite illite -- -- halloysite null

RB-09-250 RB-09-250-006 fair -- kaolinite (dickite) illite -- -- dickite null

RB-09-250 RB-09-250-007 poor -- kaolinite illite -- CO3 kaolinite null

RB-09-250 RB-09-250-007a poor lab replicate kaolinite illite -- CO3 white_marker null

RB-09-250 RB-09-250-008 fair -- illite montmorillonite -- kaolinite illite null


RB-09-250 RB-09-250-011 good -- Fe_chlorite -- CO3-calcite -- Fe_chlorite calcite

RB-09-250 RB-09-250-012 fair -- montmorillonite illite -- CO3 montmorillonite brucite

RB-09-250 RB-09-250-013 good -- montmorillonite illite CO3 chlorite montmorillonite brucite

RB-09-251 RB-09-251-001 very poor -- illite CO3-ankerite -- -- ankerite null

RB-09-251 RB-09-251-001a fair lab replicate kaolinite illite -- -- kaolinite null

RB-09-251 RB-09-251-002 fair -- montmorillonite illite kaolinite CO3-ankerite montmorillonite ankerite

RB-09-251 RB-09-251-003 good -- montmorillonite illite -- -- montmorillonite null

RB-09-251 RB-09-251-004 poor -- montmorillonite -- illite kaolinite montmorillonite null

RB-09-251 RB-09-251-005 poor -- montmorillonite -- kaolinite illite opal kaolinite

RB-09-251 RB-09-251-005a fair lab replicate montmorillonite -- kaolinite illite aspectral null

RB-09-251 RB-09-251-006 poor -- kaolinite montmorillonite -- illite halloysite null

RB-09-251 RB-09-251-007 fair -- montmorillonite kaolinite -- illite montmorillonite kaolinite

RB-09-251 RB-09-251-008 poor -- kaolinite -- montmorillonite illite halloysite null




RB-09-251 RB-09-251-012 good -- Fe_chlorite -- illite (phengite) montmorillonite Fe_chlorite phengite

RB-09-251 RB-09-251-013 good -- illite (phengite) -- chlorite CO3 phengite epidote

RB-09-251 RB-09-251-014 fair -- illite -- CO3-ankerite montmorillonite ankerite null

RB-09-252 RB-09-252-001 fair -- CO3-dolomite -- kaolinite -- dolomite kaolinite

RB-09-252 RB-09-252-002 fair -- montmorillonite -- illite kaolinite montmorillonite brucite

RB-09-252 RB-09-252-003 poor -- -- kaolinite illite -- halloysite null

RB-09-252 RB-09-252-005 fair -- kaolinite illite -- -- kaolinite dickite

RB-09-252 RB-09-252-006 very poor -- illite -- kaolinite -- aspectal null

RB-09-252 RB-09-252-006a fair lab replicate kaolinite illite CO3-dolomite -- kaolinite dolomite

RB-09-252 RB-09-252-007 very poor -- kaolinite illite -- -- tourmaline null

RB-09-252 RB-09-252-007a very poor lab replicate kaolinite illite -- -- halloysite null

RB-09-252 RB-09-252-008 poor -- montmorillonite kaolinite -- illite montmorillonite null

RB-09-252 RB-09-252-008a poor lab replicate montmorillonite kaolinite -- illite kaolinite null

RB-09-252 RB-09-252-009 fair -- montmorillonite -- kaolinite illite montmorillonite null

RB-09-252 RB-09-252-010 good -- Int_chlorite -- montmorillonite illite Int_chlorite montmorillonite

RB-09-253 RB-09-253-001 good -- montmorillonite -- illite -- montmorillonite epidote

RB-09-253 RB-09-253-002 fair -- Fe_chlorite -- kaolinite illite Fe_chlorite dickite


RB-09-253 RB-09-253-004 fair -- kaolinite montmorillonite -- illite halloysite null

RB-09-253 RB-09-253-005 fair -- montmorillonite kaolinite -- illite montmorillonite null

RB-09-253 RB-09-253-006 poor -- montmorillonite illite kaolinite -- opal null

Page 7 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments



RB-09-253 RB-09-253-008 fair -- Fe_chlorite illite (phengite) -- kaolinite Fe_chlorite phengite



RB-09-254 RB-09-254-002 fair -- kaolinite montmorillonite -- illite kaolinite null


RB-09-254 RB-09-254-003a very poor lab replicate -- -- kaolinite illite nacrite null

RB-09-254 RB-09-254-004 good -- montmorillonite kaolinite -- illite montmorillonite dickite


RB-09-254 RB-09-254-006 fair -- montmorillonite kaolinite -- illite montmorillonite halloysite

RB-09-254 RB-09-254-007 fair -- kaolinite illite CO3-siderite -- siderite kaolinite


RB-09-254 RB-09-254-009 good -- montmorillonite -- illite -- montmorillonite brucite

RB-09-255 RB-09-255-001 fair -- montmorillonite -- kaolinite illite montmorillonite null

RB-09-255 RB-09-255-002 noise no SWIR minerals -- -- -- kaolinite dark null




RB-09-255 RB-09-255-005 good -- kaolinite (dickite) illite -- montmorillonite kaolinite dickite

RB-09-255 RB-09-255-006 poor -- montmorillonite -- kaolinite -- montmorillonite null

RB-09-255 RB-09-255-007 poor -- montmorillonite illite -- CO3-siderite montmorillonite siderite

RB-09-255 RB-09-255-008 good -- montmorillonite kaolinite CO3-dolomite -- kaolinite dolomite

RB-09-255 RB-09-255-009 fair -- montmorillonite illite -- CO3 montmorillonite epidote

RB-09-256 RB-09-256-001 poor -- montmorillonite kaolinite illite CO3-siderite montmorillonite siderite

RB-09-256 RB-09-256-002 good -- illite montmorillonite -- -- opal illite

RB-09-256 RB-09-256-003 fair -- kaolinite illite -- CO3-ankerite kaolinite ankerite


RB-09-256 RB-09-256-004a very poor lab replicate -- -- kaolinite illite aspectral null


RB-09-256 RB-09-256-006 fair -- kaolinite -- illite montmorillonite kaolinite null


RB-09-256 RB-09-256-008 poor -- montmorillonite -- kaolinite illite opal null

RB-09-256 RB-09-256-008a poor lab replicate montmorillonite -- illite kaolinite montmorillonite null


RB-09-256 RB-09-256-009a poor lab replicate kaolinite montmorillonite -- illite montmorillonite null

RB-09-256 RB-09-256-010 fair -- kaolinite montmorillonite -- illite opal halloysite

RB-09-256 RB-09-256-011 fair -- illite (phengite) CO3-siderite chlorite -- siderite phengite

RB-09-256 RB-09-256-012 fair -- montmorillonite -- illite -- montmorillonite brucite

RB-09-256 RB-09-256-013 fair -- montmorillonite -- CO3 Int_chlorite montmorillonite Int_chlorite

RB-09-257 RB-09-257-001 fair -- kaolinite CO3-dolomite illite -- kaolinite dolomite

RB-09-257 RB-09-257-002 fair -- montmorillonite kaolinite CO3-ankerite illite montmorillonite ankerite


RB-09-257 RB-09-257-003a noise lab replicate; no SWIR minerals -- -- -- -- dark null

Page 8 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments



RB-09-257 RB-09-257-005 poor -- kaolinite illite -- montmorillonite dickite null

RB-09-257 RB-09-257-005a poor lab replicate kaolinite illite -- montmorillonite kaolinite null


RB-09-257 RB-09-257-007 very poor -- -- -- montmorillonite kaolinite montmorillonite null

RB-09-257 RB-09-257-007a very poor lab replicate -- -- kaolinite montmorillonite aspectral null

RB-09-257 RB-09-257-008 poor -- montmorillonite -- -- kaolinite montmorillonite null

RB-09-257 RB-09-257-008a poor lab replicate montmorillonite -- -- kaolinite montmorillonite null

RB-09-257 RB-09-257-009 good -- montmorillonite kaolinite -- -- montmorillonite kaolinite

RB-09-257 RB-09-257-010 good -- montmorillonite illite -- -- montmorillonite brucite

RB-09-258 RB-09-258-001 good -- montmorillonite illite CO3-calcite -- montmorillonite calcite

RB-09-258 RB-09-258-002 fair -- kaolinite -- CO3-calcite montmorillonite kaolinite calcite

RB-09-258 RB-09-258-003 very poor -- -- -- montmorillonite CO3 aspectral null

RB-09-258 RB-09-258-003a very poor lab replicate -- montmorillonite illite -- montmorillonite null



RB-09-258 RB-09-258-006 very poor -- -- -- kaolinite illite prehnite null




RB-09-259 RB-09-259-001 fair -- montmorillonite -- illite kaolinite montmorillonite brucite



RB-09-259 RB-09-259-003 fair -- illite -- CO3 chlorite brucite null


RB-09-259 RB-09-259-005 good -- kaolinite illite CO3-calcite -- halloysite calcite

RB-09-259 RB-09-259-006 good -- kaolinite -- illite CO3-ankerite kaolinite ankerite


RB-09-259 RB-09-259-008 very poor -- montmorillonite -- -- montmorillonite null

RB-09-259 RB-09-259-008a poor lab replicate montmorillonite -- illite -- montmorillonite null

RB-09-259 RB-09-259-009 poor -- montmorillonite -- illite kaolinite montmorillonite null

RB-09-259 RB-09-259-010 very poor no SWIR minerals -- -- -- -- opal null


RB-09-259 RB-09-259-011 good -- Fe_chlorite illite (muscovite) -- montmorillonite Fe_chlorite muscovite






RB-09-260 RB-09-260-005 fair -- montmorillonite kaolinite -- illite montmorillonite dickite

RB-09-260 RB-09-260-006 very poor -- -- -- kaolinite illite kaolinite null

RB-09-260 RB-09-260-006a very poor lab replicate -- -- kaolinite illite halloysite null

RB-09-260 RB-09-260-007 poor -- montmorillonite -- -- illite montmorillonite null

Page 9 of 10


DDHNumber

SampleNumber

SpectralQuality

SpectralComments


RB-09-261 RB-09-261-001 poor -- kaolinite illite -- montmorillonite halloysite null

RB-09-261 RB-09-261-001a good lab replicate kaolinite -- illite -- kaolinite null


RB-09-261 RB-09-261-003 fair -- kaolinite montmorillonite -- illite kaolinite montmorillonite


RB-09-261 RB-09-261-005 very poor -- -- -- kaolinite illite kaolinite null

RB-09-261 RB-09-261-005a very poor lab replicate -- -- kaolinite illite kaolinite null


RB-09-261 RB-09-261-007 fair -- illite (phengite) -- montmorillonite kaolinite phengite null


RB-09-261 RB-09-261-009 good -- kaolinite Fe_chlorite -- -- kaolinite Fe_chlorite

RB-09-262 RB-09-262-001 poor -- illite (muscovite) CO3-calcite -- chlorite muscovite calcite

RB-09-262 RB-09-262-001a fair lab replicate Int_chlorite -- illite kaolinite Int_chlorite null

RB-09-262 RB-09-262-002 very poor -- -- -- chlorite montmorillonite aspectral null

RB-09-262 RB-09-262-002a noise lab replicate; no SWIR minerals -- -- -- -- magnesium_clays null

RB-09-262 RB-09-262-003 fair -- montmorillonite -- illite -- montmorillonite epidote

RB-09-263 RB-09-263-001 fair -- illite -- CO3 chlorite illite null

RB-09-263 RB-09-263-002 poor -- montmorillonite -- CO3-ankerite illite montmorillonite ankerite

Page 10 of 10

…A10

APPENDIX 10: ENVIRONMENTAL ASSESSMENT REPORT

ENVIRONMENTAL REPORT ON GROUND DISTURBANCE ON THE ROCKY BROOK PROJECT, MINERAL LICENSES 007897M & 016221M, DEER LAKE

AREA, WESTERN NEWFOUNDLAND, NTS SHEET 12H06

for

Altius Resources Inc. Suite 202, 66 Kenmount Road, St. John’s, NL, A1B 3V7

&

JNR Resources Inc. Suite 204, 315 – 22nd Street East, Saskatoon, SK, S7K 0G6

by

Dale O’Reilly, B.Sc. (Hons) Jessica Ivany

& Jason Flight

ALTIUS RESOURCES INC.

January 2010

Altius Resources Inc. / JNR Resources Inc. …i

SUMMARY The Rocky Brook Project is a joint venture mineral exploration project being conducted in the Deer Lake Basin in western Newfoundland by Altius Resources Inc. and JNR Resources Inc. The property is comprised of 258 claims (6,450 hectares) that are held by two contiguous mineral licenses (007897M and 016221M). The focus of exploration has been to locate the bedrock source(s) of high-grade uranium-silver-bearing boulders that were discovered by Westfield Minerals Ltd. in the 1970’s. In 2008, the Forestry Division of the Newfoundland and Labrador Department of Natural Resources photographed (aerial photographs) some of the ground disturbance on the Rocky Brook Project. A report was prepared by Altius and JNR to address their concerns and to clarify that the ground disturbance is the result of well-planned exploration work, spanning several, consecutive years and not the result of reckless use of equipment (O’Reilly, 2008). During the summer of 2009, a total of five days were spent assessing the ground disturbance on most of the drill trails and sites at the project. This was an appropriate time for such an assessment as there were no drilling operations in 2008 and the “true” extent of the disturbance could be evaluated. Several hundred photographs were taken during this time documenting historic and current ground disturbance, natural re-growth of the local vegetation and areas that will require reclamation. The surficial disturbance observed at the Rocky Brook Project is not as severe as depicted in the 2008 aerial photographs. While there are a few areas that will require reclamation (once exploration ceases), the majority of the landscape has regenerated naturally with little to no evidence of mineral exploration activity.

Altius Resources Inc. / JNR Resources Inc. …ii

TABLE OF CONTENTS SUMMARY ........................................................................................................................ i 1.0 INTRODUCTION .................................................................................................... 1 2.0 LOCATION, ACCESS, INFRASTRUCTURE & PHYSIOGRAPHY ............................... 4 3.0 PREVIOUS WORK .................................................................................................. 4 4.0 EXPLORATION METHODOLOGY .......................................................................... 6 5.0 AREAS OF DISTURBANCE ..................................................................................... 7

5.1 Wigwam Brook Area ............................................................................................... 8 5.2 Goose Anomaly Area........................................................................................... 10 5.3 Birchy Hill Brook Area ............................................................................................ 15 5.4 Anomaly H Area .................................................................................................... 18

6.0 PROPOSED RECLAMATION AND CONCLUSIONS ................................................. 21

6.1 Anomaly H Area .................................................................................................... 21 6.2 Wigwam Brook Area ............................................................................................. 21 6.3 Goose Anomaly Area........................................................................................... 22 6.4 Birchy Hill Brook Area ............................................................................................ 23

7.0 BIBLIOGRAPHY & REFERENCES .............................................................................. 24

LIST OF FIGURES FIGURE 1. PROPERTY LOCATION MAP ................................................................................................................... 2 FIGURE 2. CLAIMS LOCATION AND TRAIL MAP ....................................................................................................... 3

LIST OF TABLES TABLE 1. HISTORIC MINERAL HOLDINGS, ROCKY BROOK PROJECT ........................................................................... 1 TABLE 2. CURRENT MINERAL HOLDINGS, ROCKY BROOK PROJECT .......................................................................... 1

Altius Resources Inc. / JNR Resources Inc. …1

1.0 INTRODUCTION Altius Resources Inc. initiated exploration on the Rocky Brook Project in 2001 after acquiring the rights to mineral license 007897M from a local prospector. Altius continued to add to the land position by staking additional, contiguous claims in 2001 and 2002 (the latter being done as part of a joint venture agreement with Cameco Corporation, which was terminated in 2004). In late 2004, an agreement was reached with JNR Resources Inc. of Saskatoon, SK whereby JNR may earn an interest in all of these claims by conducting mineral exploration and making payments to Altius. In May 2009, a series of reductions and groupings were completed on the claim group to preserve the most prospective areas. The Rocky Brook Project currently consists of 258 claims that are held by two mineral licenses (007897M and 016221M). Exploration work to date includes 359 drill holes (sonic and diamond combined), two ground geophysical surveys, two airborne geophysical surveys, a water sampling survey, a differential GPS survey, trenching, till pit sampling, test pit sampling, line cutting and prospecting. The following tables provide details pertaining to the mineral holdings and the location of the claim group is shown in Figures 1 and 2.

Table 1. Historic Mineral Holdings, Rocky Brook Project License Number

Number of Claims Hectares Issuance

Date

007897M 60 1,500 19-Feb-2001

008647M 152 3,800 06-May-2002

010141M 90 2,250 21-Sept-2001

010727M 135 3,375 06-May-2002

TOTALS 437 10,925

Table 2. Current Mineral Holdings, Rocky Brook Project License Number

Number of Claims Hectares Issuance

Date

007897M 60 1,500 19-Feb-2001

016221M 198 4,950 21-Sept-2001

TOTALS 258 6,450

2N

1M

2D

2L 2K

2F2E

2C

2M

11I 1L

11O 11P 1N

1K

12I12J

12O 12P

12H12G

12B 12A

11J

ROCKY BROOKPROPERTY

ROCKY BROOKPROPERTY

0 100

kilometers

50

St. Anthony

BaieVerte

Springdale

Stephenville

CornerBrook

Port-Aux-Basques

Marystown

ST. JOHN’S

Gander

Deer Lake

Grand Falls-Windsor

Buchans

PlacentiaBay

Con

cept

ion

Bay

St. M

ary’

sB

ay

St. Geo

rge’s Bay

BonavistaBay

Whi

te B

ay

Hare Bay

Notre DameBay

Fortune B

ay

Trin

ity B

ay

St. Pierre &Miquelon

Bay ofIslands

Atlantic Ocean

Gulf of

St. Lawrence

BonavistaGra

nd L

ake

GanderLake

Red Indian Lake

Lo

ng

Ra

ng

e M

ou

nt a

i ns

NEWFOUNDLAND

60°

58°

56°

54°

52°

52°

51°

50°

49°

48°

47°

46°

52°

60°

58°

56°

54°

52°

51°

50°

49°

48°

47°

46°

ROCKY BROOK PROPERTYProperty Location Map

Date Printed:

Revised By:

Drawn By:

19-Jan-2010

R. Churchill

R. Churchill

NTS:

UTM:

Scale:

Figure No:

N/A

As Shown

1


N/A

License(s)07897M

016221MALTIUSALTIUS

5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN5,480,000mN

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

490,

000m

E49

0,00

0mE

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January 15, 2010

Date Printed:

Date Revised:

Date Drawn:

A L T I U S R E S O U R C E S I N C .J N R R E S O U R C E S I N C .

Rocky Brook Project2005 - 2007 Drill Trails

NTS Sheet 12H06Map Projection: UTM NAD 27, Zone 21 for Canada

02

D.O'Reilly

Environmental_Basemap January 18, 2010

D.O'Reilly

Revised By:

Drawn By:

Scale:

Filename:

1:60,000

January 22, 2010

Figure No:

Legend

Mineral Claims

Forest Access Roads

Altius/JNR Drill Trails

Uranium Showings


2.0 LOCATION, ACCESS, INFRASTRUCTURE & PHYSIOGRAPHY The property is located in western Newfoundland (Figures 1 and 2), generally between the towns of Deer Lake and Hampden. The claims are between 5 to 10 kilometres northwest of the Trans Canada Highway (TCH) and are accessible by a number of secondary woods roads emanating from the TCH. The Town of Deer Lake is at the juncture of the Viking Trail (Northern Peninsula Highway) and the TCH, has a modern airport and a population of approximately 5,000. Topographically, the claim group can be divided into two areas: (a) a low, flat, boggy, prospective terrain and (b) an “upland” area along the eastern margin of the claim group. Vegetation within the prospective area consists of abundant alders and patches of stunted black spruce, birch and fir within larger areas of open bog with scattered ponds (flashes) whereas the upland area is more densely vegetated and locally harvested. The Humber River, a major west Newfoundland watercourse, flows southwest through the area. The majority of test pits, till pits, trenches, drill trails and sites are located within the low, flat, boggy terrain.

3.0 PREVIOUS WORK Several companies have explored the Deer Lake Basin since the mid 1970’s. The majority of Altius’ current claims were originally staked in 1974 by Westfield Minerals Ltd. who conducted extensive exploration from 1974 to 1984. During this 10-year period, Westfield completed extensive prospecting, soil and till sampling, geological mapping and related interpretation, trenching and more than 150 diamond drill holes. The only legacy of this exploration work is minor depressions in the bog (which are completely re-vegetated though were not rehabilitated), caused by less environmentally-friendly equipment such as skidders and/or tractors, and a set of open trenches at Birchy Hill Brook. The latter are completely stabilized and should be left open to avoid the necessity for future explorers to re-excavate, thereby adding to the footprint. There was no exploration in the area, post-Westfield era, until 1988 when INCO staked 452 claims and completed 24 diamond drill holes around the Birchy Hill Brook trenches. No anomalous results were recovered and the claims were allowed to lapse. INCO undoubtedly utilized the same network of trails, with minimal deviation (for accessing drill sites), constructed by Westfield. Further exploration was conducted in 1990 by NovaGold Resources Inc. however efforts were focused southeast of the Wigwam and Goose boulder fields where they conducted line cutting, soil and till sampling, test pits and


prospecting. Similar to INCO, no anomalous results were recovered and the claims were allowed to lapse. It is noteworthy to mention that there are several test pits, within this area, that are still open. These are usually marked by an approximately 1-metre high mound of soil/till nearby however this is the only evidence of exploration as the access trails are completely re-vegetated. The final exploration program, prior to Altius’ current campaign was completed by Plains Exploration from 1996 – 1997. Line cutting and geophysics (VLF-EM and induced polarization) were carried out during 1996 and diamond drilling in 1997. Once again, trails constructed by Westfield were utilized and surficial disturbance was kept to a minimum. Altius has held the mineral rights to the area since 2001 at which time they completed minor prospecting, trenching, sampling and compilation of historical data. A joint venture, with Cameco Corporation of Saskatoon, SK, was formed in 2002. Exploration within the first year of this joint venture consisted of an airborne geophysical (magnetic) survey followed up by prospecting and a small program of till pitting. Research, compilation and sampling of historical data and drill core continued in 2002 as well. During 2003, a ground geophysical (VLF-EM and magnetic) survey was conducted over 60 kilometres of cut line and was coincident with a 96-hole sonic drilling program. Cameco abandoned their interest in the property in 2004 and JNR Resources were attracted to the project late in the same year. As a result, there was no exploration program in 2004. It is noteworthy to mention that a total of 48 map-staked claims (1200 hectares) were surrendered to the Crown on December 14, 2004 from former license 010145M. These claims were surrendered voluntarily to ensure a buffer was provided between the Upper Humber Wildlife Reserve/Duck Management Units and the Rocky Brook Project. Since the inception of the Altius and JNR agreement, the project has seen extensive exploration consisting of 263 diamond drill holes (2005 – 2007 and 2009), an airborne geophysical survey (radiometric, magnetic and electromagnetic) with follow-up prospecting of anomalies (2006 – 2007), trenching (2007), a differential GPS survey (2007), a Quickbird satellite imagery survey (2007), a water sampling survey (2008) and an induced polarization/resistivity survey (2009). Furthermore, mineral license 010727M, which was proximal to the aforementioned Wildlife Reserve and Duck Management Units, was reduced and ultimately surrendered to the Crown in 2009.


4.0 EXPLORATION METHODOLOGY Exploration activities of a generative nature have been Altius’ main focus since its inception in 1997. For the most part, these activities involve little to no disturbance of the natural landscape. However, as exploration campaigns progress towards more advanced phases, programs of trenching, pitting and/or drilling are often carried out. These latter activities are usually conducted with the assistance of heavy equipment such as excavators, nodwells and/or muskegs. The machine(s) mainly travel along prepared access trails and set-up on prepared sites though natural trails/sites are sometimes utilized. As a result of the preparation and overland travel, the natural landscape exhibits varying amounts of surface disturbance (i.e. cutting, excavation, etc.). To minimize the impact of such activities, Altius has, and continues to be cognizant of and compliant with regulations governing these activities (Barrett et al., 2004). Prior to each exploration program on the Rocky Brook Project, all the necessary permits are obtained. These include: (1) an exploration approval permit which is issued by the Department of Natural Resources – Mineral Lands Division; (2) a fording and/or drilling within 15 metres of waterbodies permit which is issued by the Department of Environment and Conservation – Water Resources Management Division; (3) a temporary water withdrawal permit which is issued by the Department of Environment and Conservation – Water Resources Management Division but applied for through the Department of Natural Resources; and (4) an operating permit which is issued by the Department of Forestry. In addition to these, the Environmental Assessment Division of the Department of Environment and Conservation is contacted each year and a request is made for a ruling on whether the project needs to be registered under Section 47 of the Environmental Protection Act. Similarly, the Marine Environment and Habitat Management Division of the Department of Fisheries and Oceans is contacted each year and a request is made for a project review with respect to Section 35 of the Fisheries Act. Finally, Corner Brook Pulp and Paper, Woodlands Division is contacted for approval, as required by the exploration approval permit, to conduct exploration activities on grounds to which they hold timber rights. Upon the receipt of all permits and approvals, the Department of Natural Resources is notified regarding the commencement of work, as required. Once this notification is made, Altius/Contractor employees and equipment proceed to the project area to begin exploration. Altius has been exploring the environmentally sensitive Deer Lake Basin since 2001. Since this time, a total of 6 test pits, 64 till pits, 68 kilometres of cut line (21.1 kilometres of which was refurbished in 2009), 359 drill holes (sonic and diamond combined) and 1 trench have been completed (backfilled and contoured in


2009). Additional exploration has been conducted on the project however the aforementioned activities are the only ones that contribute to ground disturbance. In order to minimize ground disturbance, the same trails that were created in 2001, 2002 and 2003 were utilized during subsequent exploration programs (i.e. 2005 – 2007 and 2009). In addition, some trails constructed by other companies, who explored the area from the late 1970s to early 1990s, have also been used. This methodology has allowed for minimal cutting of local vegetation and minimal disturbance of the ground cover. However, the repetitive usage of some of the trails, especially the main access trails, has caused the vegetative mat to become broken in some areas. Though this methodology of trail development is not perfect, it is effective in that multiple trails emanating from a single point and spreading outward in a fan-like pattern has not occurred and that the ground disturbance is localized to specific portions of the boggy terrain versus the entire bog. Furthermore, there has been no haphazard usage of machinery (i.e. muskegs, ATVs, etc.) and the surface disturbance that is evident is the result of completing extensive exploration, mainly drilling operations, in areas that are basically impossible not to disturb (i.e. open bog). During the course of the exploration programs there has been ongoing interaction with the various Government departments. Field visits to the area have been conducted by both the Department of Natural Resources and the Department of Environment and Conservation. Altius has welcomed the input of these agencies and any recommendations for improvement have been incorporated into the exploration programs. Both departments have approved of the methodologies being used and raised no serious issues with the plans or their results.

5.0 AREAS OF DISTURBANCE There are four main areas of the Rocky Brook Project that have seen extensive exploration. These correspond to the (1) Wigwam Brook Area, (2) Goose Anomaly Area, (3) Birchy Hill Brook Area and (4) Anomaly H Area. The following descriptions of the areas and trails (including surficial disturbance) were paraphrased directly from the 2008 environmental report. Furthermore, this report does not discuss any surficial disturbance resulting from the 2009 drilling program.


5.1 Wigwam Brook Area Altius has conducted drilling, trenching, test pit and till pit operations in the Wigwam Brook area since 2001 on both the north-northwest and south-southeast sides of the brook. This area is one of the main sites of high-grade mineralization that was discovered by Westfield Minerals Ltd. in the late 1970’s. There are two main access trails that lead to the area. One of the trails, constructed by Westfield, is used to access all the drill sites and till pits north-northwest of the brook. The other, constructed by Altius in 2003, travels overland along the junction of the forest and bog and is used to access all the drill sites, test pits and trenches south-southeast of the brook, including those at the Goose Anomaly. The north-northwest trail, for the most part, has not been used since July 2006. The only portion of this trail still in use is the segment just south and sub-parallel to the brook. This area was significantly muddy and wet (due to the clay-rich, water saturated composition of the underlying soil) in 2007, however, the trail is now covered by a thick green grass (original state) with only minor wet spots locally along the trail as seen in photo 1.

Photo 1: Wet spot in north-northwest trail south of Wigwam Brook

The south-southeast trail has been in use since 2003 and was last used during the 2009 drilling program. The trail is in good shape though the upper sphagnum layer of the boggy ground exhibits signs of disturbance. The trail is locally muddy (minimal areas) where the equipment has penetrated the sphagnum layer and


into the underlying organic (peat) layer as seen in photo 2. There is one locality along this trail where the supply muskeg became stuck during the 2006 program and as a result an artificial bog hole was created (photo 3).

Photo 2: Typical ground disturbance along south-southeast trail to Wigwam Brook

Photo 3: Artificial bog hole along south-southeast trail to Wigwam Brook


There are several subsidiary trails (leading to sites) emanating from both main trails that lead into the open bog and through patches of forest. The Wigwam Brook trench which was excavated in 2007 was backfilled and contoured during the 2009 drilling program (photo 4). The trench was not excavated until October – November 2007 and during poor weather conditions. As a result, there was limited work performed and the underlying geology had not been reviewed in great detail. The trench remained open until November 2009.

Photo 4: 2007 Wigwam Brook trench backfilled and contoured in 2009

5.2 Goose Anomaly Area The Goose Anomaly is situated near an open bog. Exploration on this anomaly has consisted entirely of drilling (2003, 2006 - 2007 and 2009) with minimal prospecting. Similar to the Wigwam Brook area, it was discovered during the Westfield era. There are three trails which lead to the area. One trail constructed by Westfield, trends south along the eastern margin of the bog (forest-bog juncture) and was partially muddy due to travel in 2006 and 2007. The ground is solid but the uppermost layer is fairly wet and organic-rich, thus is easily disturbed. As with the historic trail at Wigwam Brook, this trail has now regenerated a natural cover of green grasses and low foliage (photo 5).


Photo 5: Westfield trail to Goose anomaly

The other two trails, a north and south trail, both travel overland (across the bog) between the forested area at Wigwam Brook and the forested area east of the Goose anomaly. Several subsidiary trails branch off the main trail(s) and were mainly used to access drill sites. The trails are in good shape for the most part though the upper sphagnum layer does exhibit signs of disturbance (photos 6 and 7). There are two localities where the drill became stuck and needed to be towed. As a result, two artificial bog holes, penetrating into the underlying organic layer, were created (photos 8 and 9). The circular nature of some of the trails proximal to the two holes is not the result of reckless ATV usage but from towing the drill out of the bog. It is noteworthy to mention that the drill became stuck en route to a drill site. Furthermore, to avoid getting stuck in this area again, a corduroy road was built leading to the aforementioned drill site (photo 10). There are several test pits to the east of the anomaly, at the base of Birchy Ridge, that remain open. The pits are on average of 1 – 2 metres wide and similar depth. These test pits, however, were not excavated during any exploration campaigns by Altius and are historical workings (photo 11).


Photo 6: Portion of the north trail to the Goose anomaly

Photo 7: Portion of the south trail to the Goose anomaly


Photo 8: Close-up of artificial bog hole #1 on Goose anomaly bog

Photo 9: Close-up of artificial bog hole #2 on Goose anomaly bog


Photo 10: Corduroy on Goose anomaly bog

Photo 11: Historic pit and mound located near center of photo (cluster of trees)


5.3 Birchy Hill Brook Area The Birchy Hill Brook area is situated between multiple open bogs. The area hosts high-grade mineralization at the south end of one of the bogs (Birchy Hill Bog) and was discovered during the Westfield era. Exploration in this area consists of prospecting, test pits, till pits and extensive drilling operations. There are two main access trails to the area however one has not been used since 2005. One trail, which was constructed by Westfield, emanates from the forest near Birchy Hill Brook. The portion of the trail which lies in the forest is wet and muddy however it has a solid base (photo 12).

Photo 12: Forest portion of the main Birchy Hill Brook trail (Westfield trail)

This portion of the trail was sporadically covered in thick green grass suggesting previous disturbance and has since regenerated grasses and low foliage with minor wet spots/depressions (photo 13). The remainder of the trail proceeds along the edge of the bog (on both sides) and is significantly disturbed (more on the north side versus the south). The bog is fairly muddy and track depressions are evident. The organic layer has been penetrated for a good portion of the trail, however the sphagnum cover remains though it is largely covered in mud/black organic material and is locally saturated (photos 14 and 15). There are several drill holes along the open bog and multiple trails leading to them. In addition, there are several trails which proceed through the forest north of Birchy Hill Bog that are locally muddy (photos 16 and 17).


Photo 13: Natural regeneration of grass along main Birchy Hill Brook trail

Photo 14: Birchy Hill bog main access trail


Photo 15: Birchy Hill bog main access trail (water saturated)

Photo 16: Drill trail to site RB-05-41, north of Birchy Hill bog


Photo 17: Trail entrance on bog northeast of Birchy Hill bog

There are several test pits along the Birchy Hill bog and to the north of it that remain open. They are similar in size to the ones observed in the south and some even exceed this size, resembling old trenches. Similarly, these are historic workings and are not part of Altius’ exploration programs. The second trail which was utilized to access the Birchy Hill area is located north of the Birchy Hill bog. The trail was constructed in 2002 for the purpose of collecting till samples (mechanized till pitting program) and was used again in 2005 to complete part of the regional drilling program. For the most part, the trail is in good shape except for very minor wet spots/depressions and muskeg track marks (locally evident) as seen in photo 18. In addition, there was more cutting (of timber) along this trail than the remainder of the property, as it passed through several of the forested “islands” which characterize the Upper Humber area (photo 19).

5.4 Anomaly H Area This area is located just south of the main access road to Riverside, a local cabin area along the Humber River. Two years (2006 – 2007) of exploration have been conducted in this area and consisted mainly of drilling and prospecting though historic excavations have been observed. The main access trail to the area is an old skidder/harvester trail. The trail was found as it is presently. Minimal cutting of alders was required to permit entry as well some fir, spruce and birch had to be cut to avoid the deep depressions left


Photo 18: North Birchy Hill trail across wet bog northwest of Birchy Hill bog

Photo 19: Area with cut timber along North Birchy Hill trail

by the skidder/harvester equipment of previous operations (photo 20). The area is largely cut-over and there is minimal surface disturbance. The majority of the disturbance in the area was done so by timber harvesting operations. The area, as of 2009, exhibits significant regeneration (both tree seedlings and bog grass) and will not require reclamation (photo 21).


Photo 20: Skidder/harvester trail and new cutting along right side of photo

Photo 21: RB-07-178 drill site showing natural regeneration


6.0 PROPOSED RECLAMATION AND CONCLUSIONS The ground disturbance evident at the Rocky Brook Project has been conducted in a manner which consistently tried to minimize the environmental impact. Efforts such as travelling along the edge of bogs versus across them unless absolutely necessary, avoiding merchantable timber, using tracked vehicles versus skidders, etc. were employed by Altius in an effort to mitigate the exploration footprint in an area that will show disturbance even with minimal activity. Furthermore, the disturbance is the result of well-planned exploration work, spanning several, consecutive years. As previously stated, the Deer Lake Basin is boggy terrain that is very difficult (with respect to disturbing the natural landscape) to conduct operations. Much of the exploration, especially drilling, has been concentrated in and near areas of open bog, making surface disturbance unavoidable given the nature of the drilling programs. The majority of areas that exhibit surficial disturbance require no rehabilitation assistance. These areas, in particular, are best left to regenerate naturally as the rehabilitation process would only add to the disturbance. There are several trails and/or sites on the property that can attest to the effectiveness of this practice. The following is a list of recommendations for the areas described in Section 5 of this report starting with the least severe.

6.1 Anomaly H Area As stated in the 2008 environmental report, there are no recommendations for the Anomaly H area. Altius and JNR have conducted limited exploration here and the amount of surficial disturbance is minor. It is noteworthy to mention that there were no drilling operations in this area in 2009. As of June – July 2009, significant regeneration of tree seedlings and bog grass was observed throughout the area. The significant disturbance (track depressions) along the access trail was caused by the person(s) who logged the area and the equipment that was used. There were no attempts to rehabilitate the trail upon completion of their operations though the depressions left by the skidder/harvester machinery could have been contoured to reflect the local topography. Furthermore, the surficial disturbance in the drilling area is largely the result of harvesting and not drilling operations.

6.2 Wigwam Brook Area Although extensive exploration has taken place in the Wigwam Brook area, much of the damage is surficial and is regenerating quickly and without


assistance. Historical trails were utilized where possible and newly developed trails were only constructed when necessary. The trench which was excavated during the 2007 field season has since been filled in and contoured to reflect the local topography. The muddy trail on the south side of Wigwam Brook was unsightly but has since regenerated with natural grass and only minor wet spots/depressions remain. Furthermore, natural grass has been observed in these wet areas and confirms that they are not always saturated and that natural regeneration is likely to occur if given time to do so. As previously mentioned, the original state of this trail in 2001 and 2002 (prior to Altius’ drilling operations) was that it was covered with a thick green grass that was esthetically pleasing but uncharacteristic to the area. The two main trails within the area do not require rehabilitation at this time, since they will continue to be used during future exploration programs. Once exploration has ceased in the area, both trails will have to be reassessed to determine whether or not the use of an excavator (to re-contour portions of the trails, specifically artificial bog holes) would be beneficial or detrimental to the natural regeneration process. In addition, an assessment of the uppermost (grassy) layer of the trails will have to be completed, to see if reclamation can be performed on the basis of accelerating regeneration. Once exploration has concluded, it is recommended that all leaning trees be felled along trails/sites in wooded areas and where potential for re-vegetation exists, tree (spruce/alder) seedlings should be planted, to assist in the natural regeneration process.

6.3 Goose Anomaly Area Similar to the Wigwam Brook area, the Goose Anomaly area has seen extensive exploration in recent years. The damage which is evident is mainly surficial and is regenerating naturally. The trails are largely the result of Altius’ exploration programs, however during this time, several ATV’s and Argo vehicles, possibly owned by outfitters and/or locals, were observed in the area. Most of the trails have disturbed the upper sphagnum layer only, similar to what is visible at the Wigwam Brook. The two artificial bog holes can be re-filled and contoured to reflect the local topography however a brownish-black colour will represent the repair for a short period of time (while the bog grass regenerates).


The sections of trail(s) that have been constructed in wooded areas are in some cases several meters wide. For these areas, leaning trees should be removed and seedlings (spruce and/or alder) should be planted to assist in the natural regeneration process.

6.4 Birchy Hill Brook Area The Birchy Hill Brook area has experienced the highest degree of disturbance by mechanized equipment. Most of the trail system along Birchy Hill bog is muddy and in several localities, holes have formed where equipment has been stuck and penetrated the underlying organic (peat) layer. Exploration in this area has been ongoing since 2002, and in accordance with “best practices”, the same network of trails have been utilized. It is recommended to wait until all exploration has ceased prior to commencing reclamation activities. Once exploration has concluded, the only option for rehabilitating these areas is to excavate and re-contour the trails to reflect the local topography. This will eliminate the depressions, which are locally present along the trail(s), and eliminate the pooling of water which restricts the regeneration of the sphagnum layer. The only consequence of performing such an activity is that the trail(s) will remain a brownish-black colour for a short period of time while the bog grass regenerates. Given the length of the trail(s), this will be very unattractive when compared to the surrounding natural landscape. However, given time, the area will undoubtedly return to its natural condition. The sections of trail(s) that have been constructed through wooded areas are in some cases several meters wide. Similar to the Goose area, leaning trees should be removed and seedlings (spruce and/or alder) should be planted to assist in the natural regeneration process.


7.0 BIBLIOGRAPHY & REFERENCES Devereaux, A., O’Reilly, D., Churchill, R. and Thurlow, J.G., 2009. Sixth, Seventh and Eighth Year Assessment Report on Mineral Exploration on the Rocky Brook Joint Venture, Mineral Licenses 007897M, 010141M, 016050M, 016051M and 016052M, Deer Lake Area, Western Newfoundland, NTS Sheets 12H06, 12H07, 12H10 and 12H11. 28 pages plus 8 appendices. O’Reilly, D., Devereaux, A., Churchill, R. and Thurlow, J.G., 2008. Sixth and seventh year assessment report on mineral exploration on the Rocky Brook Joint Venture, Mineral Licenses 7897M, 8647M, 10141M and 10727M, Deer Lake Area, western Newfoundland, NTS Sheets 12H06, 12H07, 12H10 and 12H11. 42 pages plus 14 appendices and 3 maps. O’Reilly, D., 2008. Environmental Report on Reclamation Activities and Ground Disturbance on the Rocky Brook Project, Mineral Licenses 7897M, 8647M, 10141M and 10727M. Deer Lake Area, Western Newfoundland, NTS Sheets 12H06, 12H07, 12H10 and 12H11. 12 pages plus 1 appendix. O’Reilly, D., Churchill, R. and Dalton, B., 2006. Trench and drill site/trail reclamation after one-year observation period report for Mineral Licenses 10409M (Mustang Trend), 11449M (Mustang Trend), 8992M (Exploits River), 9464M (Robert’s Arm), Mining Lease 141L (Rambler), 7897M (Rocky Brook), 8647M (Rocky Brook), 10141M (Rocky Brook) and 10727M (Rocky Brook), central and western Newfoundland, NTS Sheets 2D11, 2D13, 2D14, 2D15, 2E02, 2E05, 2E12, 12H06, 12H07, 12H10, 12H11 and 12H16. 6 pages plus 2 appendices. Barrett, S., Churchill, R. and O’Reilly, D., 2004. Trench and drill road reclamation report for Mineral Licenses 10409M (Mustang Trend), 8252M (Mustang Trend), 8992M (Exploits River), 9464M (Robert’s Arm) and Mining Lease 141L (Rambler), central Newfoundland, NTS Sheets 2D11, 2D13, 2D14, 2D15, 2E02, 2E05, 2E12 and 12H16. 5 pages plus 2 appendices and 6 maps.

Sm

Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20Mu20

Redox Front within

Middle Sandstone

oxidized

reduced

red

grey

St

MuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMuMu

SuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSuSu






Mu4

Mu20Mu7Mu10


Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25Mu25

Su20

Su10

Su30





Su20

Su30

Mu10

Su20

Su22

Su20

Su10

Su30

Mu25

Su10

Mu20

Mu10

Mu7

Mu25

Su20

Mu4

Mu7

Mu10

Mu20

Su10

5,4

72

,20

0 m

N

494,000 mE

5,4

72

,80

0 m

N5

,47

3,0

00 m

N5

,47

3,2

00 m

N494,000 mE

493,400 mE 493,600 mE

493,800 mE

493,800 mE

5,4

73

,20

0 m

N5

,47

2,8

00 m

N5

,47

3,0

00 m

N

5,4

72

,60

0 m

N5

,47

2,4

00 m

N493,600 mE493,400 mE492,800 mE

493,000 mE

493,200 mE

493,200 mE5,4

72

,00

0 m

N5

,47

2,2

00 m

N5

,47

2,4

00 m

N5

,47

2,6

00 m

N

493,000 mE

metres

0 100 200

RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_226RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227RB_09_227

RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228RB_09_228













RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_241RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242RB_09_242





Fault (unknown)

Middle Mudstone(Mm)


Lower Mudstone(Ml)

Lower Sandstone(Sl)

Historic JNR/Altius DDH

Reverse Fault

2009 JNR/Altius DDH

Area of Anomalous Radioactivity in Bedrock

Mu4

Su20

Su10

Upper Sandstone(Su)

Su30

Su22

Mu10

Mu7

Mu20

Mu18

Upper Mudstone(Mu)

Mu25


LEGEND

Map Number:

Area:

NTS Sheets:

Scale:

Filename:

Date Revised:

Geology By:

Drafted By:

Date Drafted:

Projection:

January 2010

April 2009

Map01_ddh_locs_W&G.wor

A. Devereaux

J.G. Thurlow

2009 DDH Locations

Wigwam Brook and Goose Anomaly Area



01

1/2,000

12H/06

5,4

77

,60

0 m

N5

,47

7,5

00 m

N5

,47

7,3

00 m

N5

,47

7,4

00 m

N

497,000 mE 497,100 mE

497,100 mE497,000 mE496,900 mE

496,900 mE

5,4

77

,70

0 m

N5

,47

7,0

00 m

N5

,47

7,1

00 m

N5

,47

7,2

00 m

N496,800 mE

496,800 mE

496,600 mE

496,600 mE

496,700 mE

496,700 mE

5,4

77

,00

0 m

N5

,47

6,9

00 m

N5

,47

6,9

00 m

N5

,47

7,3

00 m

N

496,500 mE

5,4

77

,10

0 m

N5

,47

7,2

00 m

N5

,47

7,5

00 m

N496,400 mE 496,500 mE

5,4

77

,40

0 m

N5

,47

7,6

00 m

N5

,47

7,7

00 m

N

0 100 200

metres





















Map Number:

Area:

NTS Sheets:

Scale:

Filename:

Date Revised:

Geology By:

Drafted By:

Date Drafted:

Projection:

January 2010

April 2009

Map02_ddh_locs_BHB.wor

A. Devereaux

J.G. Thurlow

2009 DDH Locations




02

12H/06

1/1,250

Prominent Magnetic Lineament(PML)


Reverse Fault

2009 JNR/Altius DDH

Historic JNR/Altius DDH

anomalous bedrock radioactivity(near or at till interface)

anomalous radioactivity in overburden

Fault (unknown)



A (mst)

Lower Mudstone(Ml)

Lower Sandstone(Sl)

B (sst)

Upper Sandstone(Su)

Upper Mudstone(Mu)

Middle Mudstone(Mm)


LEGEND




eighth & ninth year assessment report on...

Documents