prairie lake rare earth property · that trends north-northeast and extends for more than 600 km...

Prairie Lake Rare Earth

Property

Cairngrom Lake and Killala Lake Townships

Thunder Bay Mining Division, Ontario

49°01' 05" N, 86°43' 02" W

NTS Mapsheet 42E

Assessment Report Prepared for:

Canadian International Minerals Inc. Suite 950 – 789 West Pender Street

Vancouver, B.C., V6C 1H2

Report Prepared by:

14 November, 2011

1 Contents

Mackevoy Geosciences Ltd. 2011- Prairie Lake Property

1 Contents

1 Contents ................................................................................................................................................ 1 2 Figures ................................................................................................................................................... 2 3 Tables .................................................................................................................................................... 3 4 Summary ............................................................................................................................................... 4 5 Introduction .......................................................................................................................................... 5 6 Reliance on other experts ..................................................................................................................... 5 7 Property description and location ........................................................................................................ 5 8 Accessibility, climate, local resources, infrastructure and physiography ............................................. 9 9 Geological setting .................................................................................................................................. 9 10 Mineralization ..................................................................................................................................... 11 11 Prospecting ......................................................................................................................................... 13 12 Physical Work ...................................................................................................................................... 33 13 Geophysics .......................................................................................................................................... 96

13.1 Radiometric work ........................................................................................................................ 96 13.2 Magnetic data ............................................................................................................................. 98 13.3 Conclusions/Recommendations based on Radiometric work .................................................. 100

14 Assay Results ..................................................................................................................................... 122 15 Recommendations ............................................................................................................................ 128 16 References ........................................................................................................................................ 128 17 Appendices ........................................................................................................................................ 129

17.1 Summary Table of Expenses ..................................................................................................... 130 17.2 Work Done per Claim ................................................................................................................ 131 17.3 Workers Rates ........................................................................................................................... 132

2 Figures


2 Figures

Figure 1. Location map of the Prairie Lake Claim group relative to Marathon, ON. ................................... 7 Figure 2. Claim groupings located on the Prairie Lake Property.................................................................. 8 Figure 3. Selected entries for from the legend for OGS map MRD 126 1:250 000 Scale Bedrock Geology of Ontario. ................................................................................................................................................... 10 Figure 4. X-Ray Diffraction graph of rock sample 11-WJH-014. Sample was analyzed to determine the composition of an unknown red mineral.................................................................................................... 12 Figure 5. Locations of prospecting and scintillometer grids on the Prairie Lake Property. ....................... 14 Figure 6. Trenches 1-9, 12 located on claim block 4256252 ...................................................................... 36 Figure 7. Trenches 10 and 11 located on claim block 4256251. ................................................................ 37 Figure 8. TREO (%) values from channel samples collected from Trench 1. .............................................. 38 Figure 9. TREO (%) values from channel samples collected from Trench 2. .............................................. 39 Figure 10. TREO (%) values from channel samples collected from Trench 3. ............................................ 40 Figure 11. TREO (%) values from channel samples collected from Trench 4. ............................................ 41 Figure 12. TREO (%) values from channel samples collected from Trench 5. ............................................ 42 Figure 13. TREO (%) values from channel samples collected from Trench 6. ............................................ 43 Figure 14. TREO (%) values from channel samples collected from Trench 7. ............................................ 44 Figure 15. TREO (%) values from channel samples collected from Trench 8. ............................................ 45 Figure 16. TREO (%) values from channel samples collected from Trench 9. ............................................ 46 Figure 17. TREO (%) values from channel samples collected from Trench 10. .......................................... 47 Figure 18. TREO (%) values from channel samples collected from Trench 11. .......................................... 48 Figure 19. Index map of spectrometer grids on the Prairie Lake Property................................................ 97 Figure 20. Regional magnetics map of the Prairie Lake Property. Magnetic data was provided by the Ontario Geological Survey. ......................................................................................................................... 99 Figure 21. TREO values from rock samples collected on the Prairie Lake property ................................ 123

3 Tables


3 Tables

Table 1. Claim blocks contained in the Prairie Lake Property. ..................................................................... 6 Table 2. Locations, descriptions, mineralogy and assay numbers of rocks located on the Prairie Lake property. ..................................................................................................................................................... 15 Table 3. Soil samples collected on the Prairie Lake Property. ................................................................... 26 Table 4. Locations, descriptions, dates and mineralogy of outcrops on the Prairie Lake Property. ......... 27 Table 5: Charges from Belham Industries ................................................................................................... 34 Table 6. Trenches constructed on the Property, their sizes and rational for construction. ...................... 34 Table 7. Daily log, descriptions, location, mineralogy and Actlabs IDs of channel samples collected from trenches on Prairie Lake. ............................................................................................................................ 49 Table 8. Summary table of radiometric data collected using handheld spectrometers and the polymaster. ............................................................................................................................................... 101 Table 9. Summary table of assay values from trench channel samples containing >0.5% TREO (n = ?#?). .................................................................................................................................................................. 124 Table 10. Summary table of select assay results from soil samples collected on the Prairie Lake Property. .................................................................................................................................................................. 126 Table 11. Summary table of select assay results from rock samples collected on the Prairie Lake Property. ................................................................................................................................................... 126 Table 12. Summary table of expenses. .................................................................................................... 130

4 Summary


4 Summary

The Prairie Lake Property (“The Property”) is an intermediate stage exploration property located in the Killala Lake Township and in the Cairngorm Lake Township in the Thunder Bay Mining Division. The Property consists of 19 contiguous claim blocks, containing 256 claims in total, covering 4,096 hectacres. The blocks can be accessed by the Deadhorse Creek dirt road that joins the Trans-Canada highway 43 km east of the town of Terrace Bay and 25 km west of the town of Marathon in Northern Ontario. Property boundaries are marked with corner posts located the corners of the claim blocks and the boundaries are blazed and marked with flagging tape. Claims are currently un-surveyed.

Current exploration work on the property commenced June 16th, 2011 and was completed July 28, 2011. Work involved prospecting, rock sampling, spectrometer (radiometric) surveys, soil sampling, trenching and channel sampling. Work was carried out by personnel of both Canadian International Minerals Inc. and Mackevoy Geosciences Ltd., as well as by independent contracters procured by Canadian International Minerals Inc.

5 Introduction


5 Introduction

Canadian International Minerals (CIN) retained Mackevoy Geoscience Ltd. to conduct work on the Prairie Lake Property during the summer of 2011 and to prepare an assessment report for the Ontario government.

6 Reliance on other experts

Mackevoy Geosciences Ltd. has confirmed that all the claims are registered to Rudolf Wahl, the property vendor. No other opinions or experts were relied upon for preparation of this report

7 Property description and location

The Deadhorse Creek property is located along the Deadhorse Creek all-weather dirt road that extends north of Provincial Highway 17 (Figure 1). The property consists of 19 mineral groups, containing 256 claims that comprise a total area of 4096 hectares (Figure 2 and Table 1). The claims are located in Walsh and Grain Townships, which are contained within the Thunder Bay Mining Division. The approximate center of the claim blocks is 524758 mE, 5411073 mN (Nad83 Zone 16N). Grid north is used on all maps. The claims are unsurveyed, but the property boundaries are marked with blazed trees and flagging tape. Each claim corner is marked with a corner post. Surface rights are maintained by the Province of Ontario, and the mineral claims extend only to the mineral rights.



Table 1. Claim blocks contained in the Prairie Lake Property.

PROPERTY CLAIM HECTARES Claims TOWNSHIP DATE DUE RECORD NAME

Prairie Lake North 4256251 48 3 Killala Lake Apr-12 Rudolf Wahl 100%





Prairie Lake South 4256256 176 11 Killala Lake Apr-12 Rudolf Wahl 100%

Prairie Lake South 4256257 192 12 Killala Lake Apr-12 Rudolf Wahl 100%

Prairie Lake North 4256258 208 13 Killala Lake Jun-12 Rudolf Wahl 100%

Prairie Lake South 4246258 192 12 Killala Lake Jan-12 Rudolf Wahl 100%





Prairie Lake South 4256259 256 16 Killala Lake Nov-12 Rudolf Wahl 100%

Prairie Lake South 4256260 256 16 Cairngorm L. Nov-12 Rudolf Wahl 100%

Prairie Lake South 4256261 256 16 CairngormL. Nov-12 Rudolf Wahl 100%

Prairie Lake West 4246255 208 13 Killala Lake Jan-12 Rudolf Wahl 100%



TOTAL 4096 256



Figure 1. Location map of the Prairie Lake Claim group relative to Marathon, ON.



Figure 2. Claim groupings located on the Prairie Lake Property.

9 7BAccessibility, climate, local resources, infrastructure and physiography


8 Accessibility, climate, local resources, infrastructure and physiography

The Property can be accessed by the Deadhorse Creek road which begins at Provincial Highway 17, the Trans-Canada Highway, about 43 km east of the town of Terrace Bay and 25 km west of the town of Marathon in Northern Ontario. The Dead Horse Creek block is about 30 km north of Highway 17 along the dirt road.

The Prairie Lake Property is located Archean Superior Shield. Physiographically, the region consists mainly of low terrain, including swamps separated by hills that rise 100-200 m above the swamps. Aspen, birch and spruce cover the claim area; low lying areas are covered in thick alders and underbrush. Overburden on the property is quite thin on the hills (between 0-20 cm on average) and consists mainly of sand and clay-sized particles, overlain by a thin organic layer. In the valleys and swamps, the overburden and organic layers can be substantially thicker. There are small sand and gravel deposits located nearby for the purposes of constructing gravel roads, but there are no deposits on the property.

9 Geological setting

The Prairie Lake property is located in the Wawa Subprovince of the Superior Province (Ayres et al., 1971; in Sage, 1987) and has been dated at 1033 ± 59 Ma by the Rb-Sr isochron method (Bell and Blenkinsop, 1980; in Sage, 1987). The Wawa Subprovince was emplaced into a fractured-faulted continental shield environment along the Trans Superior Tectonic Zone (TSTZ) which is a fault system that trends north-northeast and extends for more than 600 km through the Lake Superior Basin (Sage, 1987). From 1.2 to 1.0 Ga, alkalic magmatis occurred in the TSTZ; this magmatism resulted in the emplacement of the Coldwell Complex, the Killalla Lake Alkalic Complex, the Chipman Lake fenites and carbonatite dykes and the Prairie Lake Carbonatite Complex. The TSTZ was also responsible for the emplacement of diatremes at Deadhorse Creek and at McKellar Creek and Slate Islands (Sage, 1987).

Appendix 17.5 shows the regional geology of the Prairie Lake Property. The underlying geology consists of Neo- to Mesoarchean (2.5-3.2 Ga) supracrustal migmatized and metasedimentary rocks of the Superior Province. Intruding into these units is a gneissic tonalite suite and mafic and ultramafic rocks, which are also Neo- to Meso-Archean in age and belong to the Superior Province. These were followed by the intrusion of a massive granodiorite to granite unit, which also belongs to the Superior Province. The alkali intrusive suite and carbonatite was the final unit to be emplaced in the the Prairie Lake area and it is considerably younger then the other rock units; it is Mesoproterozoic in age and is part of the Upper Keweenawan Supergroup of the Grenville Province.

10 8BGeological setting


Figure 3. Selected entries for from the legend for OGS map MRD 126 1:250 000 Scale Bedrock Geology of Ontario.

11 9BMineralization


10 Mineralization

The geology and mineralogy of the Prairie Lake property has not been mapped or studied to rigourous detail. The mineralogy in particular is quite complex. Rock sample WJH-11-014 was sent to the University of British Columbia for analysis using X-ray diffraction to determine the identity of an unknown red mineral present in the rock. The mineral was identified as possibly a garnet with the formula CaY2CrAl3SiO12(Figure 4). Also identified were the minerals microcline (KNaAlSi3O8), dolomite (CaMg(CO3)2), albite (NaAlSi3O8), quartz(SiO2), and a mineral with the formula ZnLaTiO3, which may be a perovskite (CaTiO3) with La impurity.

Many of the minerals on the property are red in colour, some of these were identified as ferritized potassium feldspar using a filtered UV lamp (Marianos, 2011).

12 9BMineralization


Figure 4. X-Ray Diffraction graph of rock sample 11-WJH-014. Sample was analyzed to determine the composition of an unknown red mineral.

13 10BProspecting


11 Prospecting

Prospecting occurred on the property between May 19, 2011 and July 28, 2011. Prospecting began with areas that were easily accessible and then focused on areas that had unusual radiometric signatures, as delineated from the hand-held spectrometers (see geophysical section for a description of the spectrometers). Prospecting was carried out based on access via several old roads leading into the property, and on constructed grids. The prospecting grids were also walked with the hand-held radiometric spectrometers. Figure 5 shows the location of the prospecting/spectrometer grids.

Table 2 contains sample IDs, assay numbers, locations, descriptions, daily logs and grid references for rock samples collected while prospecting on the Prairie Lake Property. Table 3 contains sample IDs, assay numbers, locations, descriptions, daily logs and grid references for soil samples collected while prospecting on the Prairie Lake Property.

Table 4 contains sample IDs, assay numbers, locations, descriptions, daily logs and grid references for outcropss collected while prospecting on the Prairie Lake Property. A total of 56 rocks samples were collected, of which 48 were submitted for assay. Four soil samples were collected and sent for assay.

14 10BProspecting


Figure 5. Locations of prospecting and scintillometer grids on the Prairie Lake Property.

15 10BProspecting


Table 2. Locations, descriptions, mineralogy and assay numbers of rocks located on the Prairie Lake property.

Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing

Location Description Sample Description

Mineralogy

Associated O

utcrop N

ame

Comments

19-May-11

W. Harm

an

G. Quist

11-WJH-003

985001

101

518374

5432106

fizzes with acid pink(Kspar), black, w

hite

19-May-11

L. Marshall

S. Vachon

11-LAM-001

985002

101

518736

5431808

moss covered outcrop

grey/red/brown, med-fine grained arenite

Picture #4. Scint 2424-A46501 (Th: 114.9, U:12.8)

19-May-11

L. Marshall

S. Vachon

11-LAM-002

985003

101

518666

5431824

Fine grained alkalic granite w/qtz. Dark figure vein (highest scint rdng)

qtz

Pictures 1,2,3. Scint 2424-A46555 (Th: 126.6, U: 5.0)

20-May-11

L. Marshall

S. Vachon

11-LAM-003

985004

101

318

518715

5431826

loose outcrop highly indurated, fine grained, rusty weathering rim

Red/grey/ arenite, qtzite?

high U + Th reading. // picture #5

20-May-11

L. Marshall

S. Vachon

11-LAM-004

985005

101

320

517592

5432001

outcrop, grey/red qtzite? With minor alkalic intrusive veins

Pic #7

16 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

20-May-11

L. Marshall

S. Vachon

11-LAM-005

985006

101

320

518736

5431994

float, red/grey sed rock

Picture #9,

21-May-11

G. Quist

L. Marshall

11-GMQ

-005

985007

101

516624

5433124

next to road adjacent to magnetite

very radioactive!

29-May-11

Wes

G. Quist

11-GMQ

-006

985008

101

317.5

518814

5431754

Top of Rudys cut block between two upturned trees

pink green and white crystalization

29-May-11

Wes

G. Quist

11-WJH-006

985009

101

330

518325

5432989

Bottom of cliff grey white rock with pink and white crystalization

pyrite

N/A

30-May-11

L. Marshall

G. Quist

11-LAM-021

985011

101

317.5

518793

5431747

Rudy's trench Orange/pink felsic intrusive K-feld and qtz, mg

cleared showing

this sample was taken at top of trnech hill but has lower GPS indicated elevation than the sample taken from near the bottom of the trench hill just minutes from each other (?) reliability of elevation indicator is questionable

17 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

30-May-11

L. Marshall

G. Quist

11-LAM-022

985012

101

317.5

518840

5431754

Rudy's trench Light grey Meta sed/volcanic with mm0scale red/orange veins, also mm-scale qtz crystals

qtz, amphiboles

cleared show

ing

700 cps on scint 2483-A

1-Jun-11

D. Gritsaenko

Wes

11-WJH-014

985013

16

517488

5433487

mound after pond area

white with red swirls (zones) Kspar, Quartz, hornblend3, hematization(?) red zones are composed of unknown mineral

OC-DG-041

scint to 2000 cps. Sent as a research sample

1-Jun-11

D. Gritsaenko

Wes

11-WJH-015

985014

14

517310

5433775

past upturned tree

pink with possible grey black

Dug out of ground

1-Jun-11

D. Gritsaenko

Wes

11-WJH-016

985015

14

517158

5433225

along cliff near less steep slope

grey fine grained mafics, with bits of white, kspar and others

OC-DG-042

4-Jun-11

D. Gritsaenko

M. Dalsin, L. M

arshall

11-DG-012

985016

N/A

517480

5433516

dead log by overturned tree, roots exposing bacon zone #2 in small clearing

aphanitic grey rock (metased?) hosting thick swirls of red medium grained crystals intermixed with black and quartz

thick swirls or bands of unknown red, mgr mineral intermixed with mafic minerals and quartz. Host rock is grey and aphanitic

OC-11-M

LD-039

other samples have a darker grey breccia with hornblende crystals several mm wide

4-Jun-11

D. Gritsaenko

M. Dalsinlory,

L. Marshall

11-DG-013

985017

N/A

517374

5433575

on mossy hill with scattered short pine trees near marsh

Gossan-extremely weathered, brownish/orange/red. Red soil around is red/brown colour

Black – mafics, red – unknown

originally found as soil anomaly, possible bacon rock, Assay: A1111

18 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

4-Jun-11

M. Dalsin

L. Marshall, D. Gritsaenko

11-MLD-010

985018

N/A

517312

5433777

dug out of a soil anomaly found with the scint. It is in a small clearing near lots of overturned trees. The soil was dug out to take a sample

mostly mgr red w/ qtz and feldspar. There is some dark grey

unknown red mineral, kfspr, plag, qtz and mafics

5-Jun-11

Wes

M. Dalsin

11-WJH-017

985019

101

330

516859

5433001

Near large boulder sticking out of cliff, sample from along fault

Redish pink rock from middle of fault kspar OC-11-M

LD-040

6-Jun-11

L. Marshall

G. Quist

11-LAM-032

985021

101

329

516425

5432843

beside logging road on cut block, this sample was beside/under (had to dig) a felsic/mafic intrusive (granite or gneiss) that appeared to have undergone magma mixing and or magma intrusions.

This rock is another classic example of the "bacon rock" previously described in another sample from Prairie Lake. The "meaty" part is reddish/pink and coarse grained with blackisk flecks and up 2 cm wide and then pinching out. The "fatty" part resembles a vfg light grey rock (meta-wacke?, carbonatite?) with approximately the same dimensions

The light gy fatty part appeared to be primarily qtz fg to vfg mainly aphanitic. The "fatty" part which we think is responsible for the high radioactivity is coarser grained with possibly some K-spar, qtz, and amphibole and an unknown red mineral

Up to 4000 cps on outcrop face

19 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

6-Jun-11

L. Marshall

G. Quist

11-LAM-033

985022

101

328

516839

5432812

halfway up/down ~15 m cliff face

same as above same as above

OC-11-M

LD-053

Up to 2500 cps. If this mineralization occurs in a meta-sed horizon, there may be a bedding strike and dip associated with it, which may be relatively easier to trace subsurface than an igneous dyke or vein complex. There was bor of the same rock found 3-5 m along the same cliff face... interesting indeed.

9-Jun-11

M. Dalsin

G. Quist

11-MLD-011

985023

101

322

516987

5432268

on old logging road. Rock found after digging up around scint high

very weathered. At surface weathered to a gossan. Hard to see orginial fabric and mineralization. Some beige host rock visible with some red minerals

red minerals and vfgr to fgr. Some dark mafic possible xenoliths

10-Jun-11

L. Marshall

Wes

11-LAM-040

985024

108

F

518748

5431856

Large roadside outcrop, easily seen

The surface is dark grey to light (rusty) brown. This outcrop appears to contain 2 distinct parts. The larger part is massive aphanitic meta-vol/sed. The second part appears to be veins or other felsic intrusions of pink/orange/red which apeared to resemble "bacon rock" which what was sampled as it seemed to be scinting the highest

meta-rock is aphanitic, felsic rock contained k-spar and qtz

The area of the sample had 700 cps but approx 30 cm down face from where sample was taken had 1300 cps which was too flat to obtain a sample from. 1 photo of outcrop and 1 of sample surface showing contrast between meta and felsic.. BUT NONE OF SAMPLE ITSELF…yet

19-Jun-11

B. Quist

11-BCQ-0165

985025

518739

5431769

north of PT-PL-11-002, north side of a gully,old flagging tape present, 2x3m, lightly vegetated

rock is pink and green, oxidized on the weathered surface, crystalline

pink mineral may be garnet, green may be pyroxene. Appears to be banded., quartz, pyroluscite staining, finely disseminated sulphides

OC-11-BCQ

-003

20 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

16-Jun-11

B. Quist

M. Dalsin

11-BCQ-0162

985026

517153

5433210

near PT-PL-11-11. looks similar to a gabbro, very mafic, little quartz. Might be hornfelsed. Overlain by mystery red/pink mineral

plag-pheric, sulphide (pyrite), magnetite, possibly fine-grained galena.

plag-pheric, sulphide (pyrite), magnetite, possibly fine-grained galena. PT-PL-11-11

17-Jun-11

L. Marshall

D. Gritsaenko

11-LAM-044

985027

109

A

518708

5432735

Approx E-W trending outcrop, ~20m long ~3m high. Fairly dense foliage.

Quite an interesting rock consisting of a mg meta-volcanic light grey intrusion with Qtz, k-spar and plag. This is intruding a fg to vfg aphanitic dark grey meta-sed that also appear as > 1m xenoliths. The highest scinting area appeared to be a vein and/or fauly

intrusive- qtz,k-spar, plag. Meta-sed aphanitic

OC-11-DG-088

Some dark grey meta-sed is extremely fine grained (clay)

22-Jun-11

B. Quist

Wes

11-BCQ-0174

985035

518602

5431902

trench cuts off the main road

country rock appears to be an alkalic-granite, sample is taken from a hydrothermally altered vein, contains sulphides (pyrite, bornite? And other), sulphides are also presnt in country rock

pyrite, bornite?, other, maganese staining

Tr-PL-11-006

21-Jun-11

B. Quist

A. Ya’acoby

11-BCQ-0172

985042

518674

5431823

in TR-PL-11-006 perfect rhomdehedral crystals are present. Rock is hyrdothermally altered, oxidized on the surface. O/C covers both sides of the trenches

absolutely loaded with sulphides, stringers, blebs, finely disemminated, sulphides have the colour of pyrite, but the cubic xstal struc was not observed (chalcopyrite?), slight green alteration on surface, pink mineral present, possible bornite. Malachite staining?

TR-PL-11-006

21 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

22-Jun-11

B. Quist

11-BCQ-0173

985043

518602

5431902

small trench with wall on southside

Country rock appears to be an alkalic-granite, sample is taken from a hydrothermally altered vein contains sulphides (pyrite and bornite? + unknown), sulphides are present in country rock, maganese staining, sulphides are finely disseminated to coarsely disseminate, gains ~.8 cm,

TR-PL-11-008

22-Jun-11

B. Quist

Wes

11-BCQ-

0173

985043

518602

5431902

trench cuts off the main road

country rock appears to be an alkalic-granite, sample is taken from a hydrothermally altered vein, contains sulphides (pyrite, bornite? And other), sulphides are also presnt in country rock

pyrite, bornite?, other, maganese staining

see field notes for sketches

11-Jul-11

D. Cameron

G. Quist

11-DTC-004

985049

121

C

519605

5432426

Off of a slight ridge, sparsly forested

Fine grained rock. Effervesent fizzing with hcl (possibly carbonatite). purple Flourite present and some red to red pink minerals. Pod of coarse grained dark purple flourite that scint the highest. Pyrite and possible pyrochlore present.

Dark purple flouite that is mgr to cgr. Pyrite, and calcite present

Same location as assay 2424-A4127

22-Jun-11

B. Quist

Wes

11-BCQ-

0175

985101

518608

5431918

directly across road from TR-PL-11-006

aphanitic, dark-grained, oxidized, finely disseminated sulphides

3-Jul-11

B. Quist

L. M

arshall

11-BCQ-

0178

985102

518761

5431998

low lying outcrop running ~40 degrees for 180-200m

fizzes, coarse grained calcite

Rudy's prospect #28

28-Jun-11

B. Quist

D. Gritsaenko

11-BCQ-0177

985103

518633

5432091

gougey; limonite in fault/vein; dirty oxidized looking rock; fizzes slightly with acid; unknown red/pink minerla (different from TR-Pl-11-007); non magnetic; small amounts of qtz; unknown black mineral; unknown fine grained grey mineral; scints high ~2000 CPS

carbonates, qtz, TR-PL-11-008

22 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

3-Jul-11

B. Quist

L. Marshall

11-BCQ-0181

985104

516717

5432087

OC is in a ditch (culvert) off a logging road; outcrop is very oxidized, rusty, scints>1000; fizzes with acid.

Rock looks layered (similar to the "bacon"); red layered with more silicious looking, lighter layers; dark clasts embedded in it that contain sulphides at both two types (arsenopyrite?, pyrite?); possibly chalcopyrite; some weathering; very bronzy; the black/dark clasts are very quite magnetic.

3-Jul-11

B. Q

uist

L. M

arshall

11-BCQ

-0179

985105

518761

5431998

coarse grained, fizzes with acid, strange red mineral

Rudy's prospect #29

11-Jul-11

M. Dalsin

S. Todd

11-MLD-

016

985106

N/A

518655

5432246

Trench 9 Vein running along the edge of rock. Quartz vein w/ a dk red mineral present and minor py.

Unknown dk red mineral and minor py w/ some dk gy metallic mineral. This is possibly tetrahedrite or galena?

TR-PL-11-009

11-Jul-11

D. Cameron

G. Quist

11-DTC-005

985107

121

C

519601

5432653

Top of a ridge that has swamp to the west, forested. Dug through 2ft of overburden

Red and white bretcha surrounded by host material. Bretcha is matrix supported. Bretcha looks similar to k-feltsbar but more vivid red.

23-Jul-11

B. Quist

M. Dalsin

11-BCQ-0188

985108

5189600

5432417

At DTC-04 high scinting value, hole was dug. Soil is dark red/rusty. Rock fizzes slightly with acid, oxidized, very slightly magnetic, weathered, strange red mineral present. Sub crop, possibly float, very angular, mostly likely in place or very local

23 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

20-Jul-11

M. Dalsin

S. Todd

11-MLD-017

985109

518671

5431849

on TR-PL-11-005, sampled inside a fault that could not be sampled by channel sampling due to small cave

rock si weathered on the surface (limonite). Fresh surface is very fine grained gy to purpleish grey. There is some fgr unknown red mienralization and hematite staining.

unknown red mineral, trace disseminated pyrite TR-PL-11-005

scint to 2000 cps

28-Jul-11

B. Quist

S. Todd

11-BCQ-0189

985111

518718

5431798

Pit of doom on mega trench

chip hand sample of weird, red crumbly rock at bottom of pit (south end). Also some weird black dyke was also sampled. Banded outcrop, the mafic dyke is magnetic and contains yellow-speckled rock (similar to TR-PL-008). Unknown red mineral. Very weak, friable rock, no reaction with acid

28-Jul-11

B. Quist

S. Todd

11-BCQ-0190

985112

518717

5431800

north end of pit of doom. Three lithologies present: 1. small f.g. mafic dyke, very magnetic. 2. bright yellow phenocrysts in a dark matrix. 3. layered red and white rock (looks like bacon). Nothing fizzes with acid, extremely friable and weak (in a fault zone).

24 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

20-Jun-11

B. Quist

A. Ya’acoby

11-BCQ-

0166

985324

518628

5432081

Taken from TR-PL-11-007.

banded, lots of purple fine grained minerals (cerium rich), oxidized, not magnetic, fizzes with acid, massive black layer, silicious

TR-PL-11-007

28-Jun-11

B. Quist

D. Gritsaenko

11-BCQ-0176

No Assay

518608

5432094

on TR-PL-008, top north end.

rock appears to be a granite (?) or quartz syenite (qtz=30%, K-fds=60%, plag=10%); rock is quite pink, oxidized on some surfaces; extensively veined; qtz grains look very rounded (but I don't think it’s a sed rock); grain sizes vary (med-coarse grained); biotite present; occasionally contains purpule fluorite.

qtz, k-fds, pl, bt, fl

TR-PL-11-008

21-May-

11

D. Gritsaenk

o

Wes

11-DG-004

No Assay

101

324

518386

5432384

on hill side weathered colour pink/gray, fresh surface is dark gray

approx 5m height exposed, fairly wide

19-May-11

G. Quist

Wes

11-GMQ

-002

No Assay

101

518556

5432092

fizzes, no lustre Kspar + black

20-May-11

G. Quist

Wes

11-GMQ

-003

No Assay

101

321

518837

5432108

21-May-11

G. Quist

L. Marshall

11-GMQ

-004

No Assay

101

516661

5432650

next to road biotite, qtz, kfspr

25 10BProspecting


Date

Nam

e

Nam

e 2

Sample

Nam

e

ActLabs Sam

ple ID

Grid #

Line #

Easting

Northing


Mineralogy

Associated O

utcrop N

ame

Comments

25-May-11

M. Dalsin

G. Quist

11-MLD-006

No Assay

101

313

518402

5431291

in burnout area lamprophyre dyke mafics and plag or carbonate nodules

OC-11-M

LD-023

21-May-11

M. Dalsin

S. Vachon

11-SJV-001

No Assay

101

518757

5432290

clearing w/ small trees

pink granite w/ kfspr, bt, some pronounced veins

kfspr, qtz, plag, bt

24-May-11

Wes

S. Vachon

11-SJV-002

No Assay

101

316

518682

5431528

forested bottom of a hill

pink red rock with some grey intermixed

1-Aug-11

G. Quist

D. Cameron

11-GMQ

-012

122

A

521197

5426488

high scinting 3400 cps (Assay 2424-A4320),middle of significant incline over gravel

majority of rock is extremely weathered, dificult to split in the field.

26 10BProspecting


Table 3. Soil samples collected on the Prairie Lake Property.

Date Name Name 2 Sample Name Easting Northing Error (m) Elevation (m) Location Description Soil Description Comments

7/8/2011 B. Quist M. Dalsin 11-BCQ-0184 518607 5431873 2 342

at the end of trench TR-PL-11-006

Clay with pebbles and rocks, some small rocks, soil is grey brown to grey orange, located in the center of two intersecting faults, TR-PL-11-006



light brown/red, lots of clay sized particles, but also some pebbles and cobbles, see sketch in notes for location, on TR-PL-11-006



brown orange to brown red, loamy clay with some small pebbles, near top of outcrop on fault



sample possibly contaminated with soil falling down from above, reddy brown clay, some small pebbles

27 10BProspecting


Table 4. Locations, descriptions, dates and mineralogy of outcrops on the Prairie Lake Property.

Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)

Location Description Rock Description Mineralogy

Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay # Comments

6/16/2011

B. Quist

M. Dalsin

OC-11-BCQ

-001

517588

5433290

2

1646

near trench 11

banded, with quartz and k-feldspar overlying a layer rich in epidote/pyrrhotite; gniess underlies all units

epidote, pyrrhotite, finely disseminated sulphides

6/19/2011

B. Quist

OC-11-BCQ

-003

518739

5431769

2

1683

north of PR-PL-11-002, north side of a gully,old flagging tape present, 2x3m, lightly vegetated

rock is pink and green, oxidized on the weathered surface, crystalline

pink mineral may be garnet, green may be pyroxene. Appears to be banded., quartz, pyroluscite staining, finely disseminated sulphides

5/21/2011

D. Gritsaen

ko

Wes

OC-11-

DG-008

101

324

518434

5432398

5

on hill side, aprox 5m height exposed,fairly wide

weathered colour is pink/grey,fresh surface is dark grey

~250 cps, K: 1%, U: 5ppm, Th: 25 ppm

11-DG-004

sample taken from section of rock ~10m further

5/21/2011

D. Gritsaen

ko

Wes

OC-11-

DG-009

101

322

517793

5432207

6

large area of exposed rock after dense, swampy forest,

weathered surface dark gray + mossy, fresh surface is pink

pink contains qtz, plag & kspar

Scint ~ 95cps (no high) no acid reactions

5/21/2011

D. Gritsaenko

Wes

OC-11-DG-

010

101

322

518003

5432196

4

open space showing some outercrop through moss

Black rock North, contact with Pink Rock south (trend continues – pink rock generally south etc)

5/27/2011

D. Gritsaen

ko

G. Quist

OC-11-

DG-028

101

327

518268

5432701

6

371

downhill on cliff side pink weathered rock kspr, biotite +

qtz

2483-

A8634

Assay #8634 was taken 5m away from this outcrop, has picture***

28 10BProspecting


Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)


Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay #

Comments

5/27/2011

D. Gritsaen

ko

G. Quist

OC-11-

DG-029

101

329

518398

5432902

6

366 coarse grained and pink

large grains of qtz, fdspr + biotite (?)

2483-

A8925

Assay #8925 was taken at outcrop and has photo***

31/201

Wes

itsae -D

101

18

517704

3314 6

336 After really marshy area

Lots of pink colouring with grey Quartz, Kspar

o fol 300 N/A N/A

5/31/2011

Wes

Gritsaenk

11-DG-

101

18

517699

5433297

6

338

lots of pine trees, logs of deadfall

grey/pink weathered surface

Kspar, quartz and hornblend

300 N/A N/A

5/31/2011

Wes

D. Gritsaen

ko

OC-11-

DG-040

101

18

517612

5433278

7

336

on West side of swamp

pink red and brown weathered surface

Quartz veins and Kspar

1000 (on brown/red line)

N/A

2483-

A9807

Too flat of a surface to break off a sample

6/1/2011

D. Gritsaenko

Wes

OC-11-DG-041

101

16

517494

5433491

7

327

Clearing ten meters from small pond, thorny bush on top of OC

2x2m exposed very pink weathered surface with white areas

Ksapr, Quarts (fine grain), bits of hematization (? Something making the pink/red colour), medium grained hornblende

2000cps 11-

WJH-014

A10147

On June 4th this outcrop was revisited by M. Dalsin, L. Marshall and D. Gritsaenko. It was further exposed and appears to be overlain by a coarse grained granite. Some mafics are present in the red bands. "The Bacon Zone"

6/1/2011 Gritsaenk

Wes

11-DG-

101

14

517163

5433231

7

320

Uphill lots of deadfall beside cliff

small cliff dark grey fine grained

mafics, bits of white, kspar and others(?)

1200 11-

WJH-016

A10671

29 10BProspecting


Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)


Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay #

Comments

6/17/2011

D. Gritsaenko

L. Marshall

OC-11-DG-088

109

A

518705

5432726

5

331

area by long 2m high, 30m long cliff surrounded by mainly deciduous trees

2m high, 30m long --> mega breccia! Large intermingling of aphanitic, dark grey unit and coarse grained white/pink volcanic intrusion(?) through out OC. Clasts are dark grey/black and up to 1m. Micro-veins of quartz run through pink/white unit.

volcanic intrusion: qtz, plag, kspar, mafics? Dark gray host (metased?): too fine grained to tell

breccia?

1200cps 11-

LAM-044

2424-

A293

host was extremely fine grained! More so than seen previously on both properties

5/29/2011

Wes

G. Quist

OC-11-

GMQ

-001

101

517945

5433072

5

339

Flat area of exposed rock folds in rock

folds 150 N/A N/A

5/21/2011

M. Dalsin

S. Vachon

OC-11-

MLD-010

101

325

518884

5432501

pink granite kfspr, plag, bt

5/21/2011

M. Dalsin

S. Vachon

OC-11-

MLD-011

101

325

518473

5432492


2483-

A8507

5/21/2011

M. Dalsin

S. Vachon

OC-11-

MLD-012

101

323

517777

5432282


5/21/2011

M. Dalsin

S. Vachon

OC-11-

MLD-013

101

323

517943

5432288


30 10BProspecting


Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)


Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay #

Comments

5/25/2011

M.

Dalsin

G. Quist

OC-11-

MLD-

016

101

314

518609

5431418

2

312

burn out area with deadfall

pink granite outcrop ~10m accross. Gneiss like textures with felsic and mafic bands

kfspr, plag, 1-3% mafics

25/201 Dalsi Quis -MLD

101

314

518356

3140

351 pink grainite kfspr and mafics


101

314

518080

3141



101

314

517409

3139


5/25/2011

M.

Dalsin

G. Quist

OC-11-

MLD-

020

101

313

517247

5431309

2

346 clearing

pink granite with mgr to fgr mineralization with some layering and pronounced veins

kfspr, plag, qtz, w/1-3% mafics

at lunch spot

5/25/2011

M.

Dalsin

G. Quist

OC-11-

MLD-

021

101

313

517331

5431314

2

346

very obvious and pronounced gneiss texture with mafic and felsic banding

5/25/2011

M.

Dalsin

G. Quist

OC-11-

MLD-

022

101

313

518259

5431290

2

331

burnout close to cliffs

pink granite outcrop with near by cliffs the same rock type

kfspr, mafics

2483-

A8780

5/25/2011

M. Dalsin

G. Quist

OC-11-M

LD-023

101

313

518402

5431291

3

331 in burnout area

lamprophyre dyke. Green to grey green with grey to brown on weathered surface. White nodules (plag or carbonates?) possible contact with pink granite near by as there are rock rubble with both

31 10BProspecting


Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)


Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay #

Comments

6/4/2011

M. Dalsin

L. Marshall, D.

Gritsaenko

OC-11-M

LD-039

N/A

517481

5433515

2

340

small clearing w/ an over turned tree exposing the outcrop

outcrop exposed by tree. Dark gy host rock that is fgr with possible dark grey breccia fragments and 1-10cm bands of mgr red mineralisation

unknown red mineral in the bands along with some qtz and plag. Hbl in the possible breccia fragments. Rest of host is vfgr

11-DG-012

Close to OC-11-DG-041

6/5/2011

M. Dalsin

Wes

OC-11-M

LD-040

101

330

516856

5432997

3

334

at the edge of cliff in a small gully

most of the outcrop appears to be gneiss. There is a fault running through that is pink to pink red and scints the highest

mgr to cgr kfspr is the majority w/ some qtz, plag and <1% mafics

fault at 60-70 degrees average 500

up to 1200

11-WJH-017

2483-

A10810

6/9/2011

M. Dalsin

G. Quist

OC-11-M

LD-053

101

328

516830

5432813

5

339

halfway down a cliff face

granite to gneiss overlying "bacon" rock. Light gy w/ red disseminated grains to red bands. Area w/ fgr disseminated red is still high scinting

red mineral, vfgr gy host rock, dark mafics

5/24/2011

Wes

S. Vach

on

11-SJV-

101

316

518345

5431728

4

Burnt section of trees white and pink rock

white meets red, contact?

24/201

Wes Vach

-SJ

101

315

517473

3151 6

burnout area with deadfall

large pink and white crystals

5/23/2011

Wes

S. Vach

on

11-W

JH-

101

317

518827

5431708

7

316

three toppled trees

pink red exposed triangular rock

120 Scint stayed around 120-150 cps for much of the line

23/201

Wes Vach

-WJH

101

317

518681

3170 7

325 start of large outcrop area

pink and grey intermixed rock

128

23/201

Wes Vach

-WJH

101

317

518106

3171 7

346 opposite small swamp grey rock

130

24/201

Wes Vach

-WJH

101

317

518385

3169 7

340 swampy area black cut through pink rock

32 10BProspecting


Date

Nam

e

Nam

e 2

Outcrop N

ame

Grid #

Line #

Easting

Northing

Error (m)

Elevation (m

)


Description

Structures

Polymaster

/Scint

Rock Sam

ple N

ame

Assay #

Comments

5/24/2011

Wes

S. Vach

on

11-W

JH-

101

316

517797

5431604

6

332

vertical face through poplar trees

pink grey swirl looking rock

70

5/24/2011

Wes

S. Vach

on

11-W

JH-

101

315

518660

5431507

7

305

moss covered side of hill with slabs

Large slabs of pink and red

33 11BPhysical Work


12 Physical Work

Physical work was conducted on the Prairie Lake property between June 16th, 2011 and July 28th, 2011. Figure 6 and Figure 7 show the location of the 12 trenches that were dug on the property using an excavator. Figure 8 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-001. Figure 9 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-002. Figure 10 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-003. Figure 11 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-004. Figure 12 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-005. Figure 13 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-006. Figure 14 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-007. Figure 15 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-008. Figure 16 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-009. Figure 17 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-010. Figure 18 shows the total rare earth element oxide (TREO) percentages for samples taken from TR-11-PL-011.

Table 6 presents the location of samples taken from the various trenches, as well physical and mineralogical descriptions of the rocks. Assay results can be found in the Appendix located at the end of this document. A total of nine trenches were dug on the Prairie Lake, the total combined area of the trenches was 2846 m2. A total of 238 channel samples were collected from the trenches and sent for assay along with 24 blanks.

Trenches were channel sampled using a diamond bit rotary rock saw. The samples were described, photographed under plain light and bagged on site; samples were later photographed under UV light in the office; UV light can reveal the presence of fluorescent rare earth minerals that are not visible under plain light.

Belham Industries of Thunder Bay were contracted to construct exploration access, trenching, face washing and rock sawing services. Invoices were inclusive for fuel and accommodation. Two men were supplied for face washing and rock sawing of samples under the supervision of Mackevoy Geosciences. Mobilization costs were from Thunder Bay to the property (Terrace Bay.) A Belt Link 240XL was supplied and the associated costs are displayed below in Table 5.

34 11BPhysical Work


Table 5: Charges from Belham Industries

Expense Type Cost per Unit Total Cost ($)

Mob-Demob $125.00/hr $3,828.12

Truck Km $0.65/km $3,065.40

Travel for operator/crew $40.00/hr $5,365.00

Standby crew $40.00/hr $460.00

Standby equipment $140.00/hr $1,400.00

Labour $40.00/hr $14,840.00

Supply of excavator $140.00/hr $17,640.00

Supply of quad $100 and $70 $2,815.00

Rental/repair charges Various $6,748.63

Meals and accommodation

Various $16,618.87

Fuel Various $8,927.68

Table 6. Trenches constructed on the Property, their sizes and rational for construction.

Trench Rational for construction Area covered (m2) UTM Samples taken

TR-11-PL-001 Up hill, sample with high REE values was collected from here 517 518819 mE,

5431753 mN 37

TR-11-PL-002 High radiometric values 53 518812 mE, 5431744 mN 15

TR-11-PL-003 Perpendicular to trench 1 10 518853 mE, 5431716 mN 22


TR-11-PL-005 High radiometric values 60 518674 mN, 5431839 mN 11


TR-11-PL-007 Flat lying area at top of hill, 392 518747 mE, 79

35 11BPhysical Work


reasonably high radiometric value 5431995 mN

TR-11-PL-008 Fault, high radiometric vlaues 517 518625 mE, 5432088 mN 16

TR-11-PL-009 Fault, high radiometric vlaues 267 518647 mE, 5432233 mN 21

TR-11-PL-010 Possible carbonatite, high REE values 52 519635 mE, 5432631 mN 8

TR-11-PL-011 Possible carbonatite, high REE values 5 519634 mE, 5432654 mN 3

TR-11-PL-012 Constructed to get an idea of

structure and wether high radiometric zones are continuous

885 518702 mE, 5431797 mN

TOTAL 2846 238

36 11BPhysical Work


Figure 6. Trenches 1-9, 12 located on claim block 4256252

37 11BPhysical Work


Figure 7. Trenches 10 and 11 located on claim block 4256251.

38 11BPhysical Work


Figure 8. TREO (%) values from channel samples collected from Trench 1.

39 11BPhysical Work



40 11BPhysical Work



41 11BPhysical Work



42 11BPhysical Work



43 11BPhysical Work



44 11BPhysical Work



45 11BPhysical Work



46 11BPhysical Work



47 11BPhysical Work



48 11BPhysical Work



49 11BPhysical Work


Table 7. Daily log, descriptions, location, mineralogy and Actlabs IDs of channel samples collected from trenches on Prairie Lake.

Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth

Description Mineralogy Comm

ents

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-030

984591

518808

5431759

top trench

214

110

6 6 light gray matrix that fizzes weakly (dolomite). Small red clasts and units of unknown minerals. Possible vfgr purple flourite. Some disseminated red minerals. Sample is cut across a 'bacon' intersection between 2 vertical faults.

dolomite, unknown red mineral, fluorite?

19/07/11 M

. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-031

984592

518805

5431757

top trench, taken

through a fault

188

102

8.5 11

sample taken through a fault. Limonite altered rock through the middle (~30cm) w/ light gray vfgr rock on either side. The fault may be dipping just under the rock. This would explain rubbly bits at the under a solid piece at surface.

the light gray rock has dolomite with some small red fragments and units. Red is composed of unknown minerals and is locally disseminated. Minor perovskite.

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-032

984593

518801

5431758

top trench, xcutting a fault

224

97 8 8 sample is x cutting a fault. Mostly lt gray rock that weakly fizzes locally. There are tonnes of liminote alteration that mostly is at surface and following fractures. Some local spots close to the fault are weakly brecciated. There is irregular veins and clasts of red minerals and local zones with some pyrolusite. Some vfgr silver looking minerals that are a little smeared.

carbonates? Limonite alteration, unknown red mineral, pyrovskite

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-033

984594

518801

5431755

top trench

212

82 8 7 going across close to the fault. Mostly amphibolite w/ xcuting veins of dolomite and red mineralization. Some of the red veins produce halos into the amphibolite. Some minor perovskite.

dolomite, unkown red mineral, perovskite, pyrolusite

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-034

984595

518800

5431755

top trench,

up a vertical

face xcutting a fault

220

85 8 7 xcutting a thrust fault going up a vertical face. Next to 033. fault is mostly limonite altered rock with some pink rock. The rest of the interval is weakly brecciated kspar rich granite (qtz syenite?) w/some qtz. breccia fragments are small, veins are xcutting the rock and creating the breccia texture. There are some minor local amphibolite fragmetns. Some pyrolusite present.

kfspar, qtz, amphibole, pyrolusite

50 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-035

984596

518803

5431753

top trench, verticall

y up from

sample 034

220

89 7 6 vertically up from sample 034. very similar to breccia from 034 only getting less brecciated as you move certicall up the hole. Possible pyrolusite present and an unknown yellow mineral. Small breccia fragments

possible pyrolusite present and unknown yellow mineral

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-036

984597

518799

5431755

top trench,

fault and

fracture zone

208

109

7.5 5 xcutting a fault and fracture zone. Pink and brown to gy breccia. Pink to pink/red clastss that are 4cm in size. Some local limonite staining and fgr pyrite. Clasts look to be made up of mostly kfspr. Unkwon dk metallic mineral

limonite, pyrite, kfspr, unkown drk metallic mineral

19/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

PL-TR-001-037

984598

518797

5431754

top trench, verticall

y up from 036

208

90 10 7.5

up vertically from 036. mostly pink kfspr (qtz syenite?) w/some white qtz fgr disseminated pyrite fractures infilled with possible pyrolusite. Local biotite. Locally brecciated near the bottom.

kfspr, qtz, pyrite, possible pyrolusite, local biotite

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-001

984556

518839

5431765

60 60 9.5 9 Dark blue-grey to dark blue-green amphibolite with lesser amounts of greyish dolomite or ankerite? Magnetic (hydrothermal alteration?) fine grained with no distinguishable crystal structures. Minor limonitic weathering in some microfractured areas. Located on the footwall of a major thrust fault. Minor bacon (red mineral) increases as fault is approached as well as the light grey ankerite? which is present intergranular and in small veins

Unknown reddish mineral, light grey mineral (ankerite, qtz carb), magnetite, limonite.

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-002

984557

518840

5431763

60 82 9 9 Dark blue-grey to dark blue-green amphibolite with lesser amounts of greyish dolomite or ankerite? Magnetic (hydrothermal alteration?) fine grained with no distinguishable crystal structures. Very limonitic weathering as it is located across a major thrust fault, and into the hanging wall. Minor bacon (red mineral) increases as fault is approached as well as the light grey dolomite/ankerite which s present intergranular and in small veins.

Unknown reddish mineral, light grey mineral (ankerite, qtz carb), magnetite, limonite, amphibole.

90% recovery

51 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-003

984558

518837

5431770

64 91 9 8 Same dark grey blue amphibole mineralization as 001 and 002 with light grey (dolomite, ankerite, qtz carb). A cross section of a "bacon" fault can bee seen clearly in this hole and the center of the hole crosses the fault, located vertically with the dip of the fault being only 1-2 degrees. There is about 1 cm limonitic weathering in the fault "baconite". The fault is layered with alteration halos. The very center of the fault is a very thin line of the unknown reddish mineral. This mineral is disseminated through the light grey host immediately below the live which may suggest a slight gravity control or approximate orientation with respect to the horizontal when the hydrothermal? vein formed, perhaps as an offshoot of the nearby carbonatite complex. The halo then proceeds into an aphanitic orange red to light grey HCl reactive mineralization, then into fg orange-red and light grey horizon, then into fg orange/whitish mineralization with minor disseminated dark grey mineralizatoin (perovskite?), then a thin vein 0.5 cm (the common Ca-mineral), then orange/pink mineralization grades back into the amphibolite host. (ankerite?) veins run mainly parallel to fault. NOT magnetic

Unknown reddish mineral, light grey mineral (ankerite, qtz carb), magnetite, limonite, amphibole.

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-004

984559

518840

5431766

52 90 7.5 8 Same dark grey blue amphibole mineralization as 001 and 002 with light grey (dolomite, ankerite, qtz carb). A cross section of a "bacon" fault can also be seen clearly in this hole as the fault crosses the top of the hole, located vertically with the dip of the fault being only 1-2 degrees. There is about 1 cm limonitic weathering in the fault "baconite". The fault is layered with alteration halos. The very center of the fault is a very thin line of the unknown reddish mineral. This mineral is disseminated through the light grey host immediately below the live which may suggest a slight gravity control or approximate orientation with respect to the horizontal when the hydrothermal? vein formed, perhaps as an offshoot of the nearby carbonatite complex. The halo then proceeds into an aphanitic orange red to light grey HCl reactive

Unknown reddish mineral, light grey mineral (ankerite, qtz carb), magnetite, limonite, amphibole, magnetite

90% recovery

52 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

mineralization, then into fg orange-red and light grey horizon, then into fg orange/whitish mineralization with minor disseminated dark grey mineralizatoin (perovskite?), then a thin vein 0.5 cm (the common Ca-mineral), then orange/pink mineralization grades back into the amphibolite host. (ankerite?) veins run mainly parallel to fault. Magnetic

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-005

984560

518843

5431761

116

106

8 7 Crosses a 40cm fault near bottom of trench. Fault rock is highly weathered to limonitic "mud". Same common dark grey-blue amphibolite host rock. "bacon" rock in fault is similar to bacon described in 003 but with brighter and more prevalent orange-red mineralization. Pyrite is quite common, with up to 1 cm ankerite/qtz carb veins which pinch-out throughout. Non magnetic

Unknown red-orange mineral, light grey mineral (ankerite, qtz carb), limonite, amphibole,

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-006

984561

518839

5431762

50 98 7 5 Crosses a 40cm fault near bottom of trench. Fault rock is highly weathered to limonitic "mud". Same common dark grey-blue amphibolite host rock. "bacon" rock in fault is similar to bacon described in 003 but with brighter and more prevalent orange-red mineralization. Pyrite is quite common, with up to 1 cm ankerite/qtz carb veins which pinch-out throughout. Non magnetic

Unknown red-orange mineral, light grey mineral (ankerite, qtz carb), limonite, amphibole,

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-007

984562

518844

5431759

50 84 8 7 Vertical hole up face of (hanging wall?) Same dk grey-blue amphibolite. Minor red/orange 'bacon" mineralization with 2cm ankerite/qtz-carb vein. Either side of vein has unknown black vfg mineralization. Minor pyrite pyrite plus magnetite. Also has small amount of unkonwn pinkish-white mineral disseminated in the common ankerite? qtz carb? dolomite? veins and intergranular. Part of alteration halo?

Unknown red/orange mineral, as well as unkown pinkish white mineral. (ankerite, dolomite,qtz carb?) magnetite, pyrite, amphibole, unknown black mineral.

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-008

984563

518839

5431763

50 80 7 7 Crosses small "bacon" fault, otherwise same common dark grey-blue amphibolite, magnetic, HCl reactive in micro fractures

Unknown "bacon mineral", (ankerite, dolomite, qtz carb?), magnetite, amphibole

95% recovery

53 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-009

984564

518840

5431760

50 100

7 9 Crosses small "bacon" fault, otherwise same common dark grey-blue amphibolite, magnetic, HCl reactive in micro fractures. This hole is vertical and has yellow/green staining in the micro fractures.

Unknown "bacon mineral", (ankerite, dolomite, qtz carb?), magnetite, amphibole, limonite

95% recovery

7/15/2011

L. Marshall

S. Todd

TR-11-PL-001

TR-PL-001-010

984565

518835

5431754

112

106

8 7.5

Crosses zone with many small "bacon" faults, and mized with same dark grey-green amphibole, limonitic weathering

95% recovery

16/07/11 S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-011

984567

518838

5431756

Vertical hole

crossing the

face of a major thrust fault.

184

101

8 109

f.g orange matrix with light green-grey (riebeckite?) and equigranular unknown black-blue mineral. Numerous <1cm ankerite/qtz carb veins running parallel to dip of fault. Some veins contain parallel burgandy veinlets. Only veins seem to be HCl reactive, non magnetic. limonitic weathering on exposed surface and fractures.

riebeckite?, unknown, ankerite? Qtz carb? Unknown burgandy (hematite?), limonite

90% recovery

16/07/11

S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-012

984568

518829

5431764

Located on

thrust fault plane (foot wall?)

316

96 7.5 6 Limonitic weathering, light grey ankerite/qtz carb matrix with orange/red breccia clasts which also contain dark grey disseminated anhedral fg crystals, Non magnetic, HCl reactive (when scaped into a powder) see comment

ankerite/qtz carb? Orange/red unknown, unknown dark grey crystals (perovskite?)

80% recovery. Original

thought #1, the

"Baconite" is breccia that

has undergone

plastic deformation.

16/07/11 S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-013

984569

518830

5431753

crossing the

largest thrust

fault on the

trench.

26 107

6 4 High limonitic weathering. This hole has large "baconite veins" with the common light grey (ankerite?) matrix with whispy and pinching-out reddish mineralization (hematite enrichment?). The edges of the largest fault vein consist of a line of unknown orange mineralization that disseminates into what appears to be the common amphibolite (dark grey-blue amphibole but is almost blask in some areas. The limonitic weathering is quite reddish (hematitic) or residual

90% recovery

54 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

"bacon" (reddish) unknown mineral within veins. Non-magnetic, HCl reactive, very minor pyrite.

16/07/11 S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-014

984571

518829

5431764

vertical hole on hanging

wall above thrust fault.

316

100

10 7 Blue-grey amphibolite host with fg dark to light grey equigranular anhedral crystals. Very well indurated (qtz present?) non-magnetic

amphibole? Ankerite? 80% recovery.

16/07/11 S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-015

984572

518824

5431748

Crossing small fault.

138

120

7.5 7 Appears to be a breccia with two types of clasts. (as seen at DHC?). The vein matrix is the common light gray ankerite? Mineralization. The less abundant clast appears to be the "baconite" (orange/red) with dark grey anhedral (perovskite?) mineralization. The more abundant clast is a dark blue-grey euhedral/subhedral (amphibloite) with other minor inequigranular pink/red/burgandy/orange mineralization, these breccia clasts are semi-magnetic

unknowns, magnetite, perovskite, ankerite, amphibole, limonite.

85% recovery

16/07/11 S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-016

984573

518822

5431754

Located on

thrust fault plane (foot wall?)

396

68 8 8 Same dark grey-blue amphibolite/ankerite host with minor ankerite veining, and the entire rock appears to host the minor "orange baconite" mineral. HCl reactive , fg, non-magnetic, minor pyrite, limonitic weatheriing.

ankerite?, unknown, pyrite, limonite, amphibole

95% recovery

16/07/11

S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-017

984574

518820

5431755

On thrust fault plane above

016

396

100

7 8 dark grey amphibolite/ankerite? Host, fg, with a large ankerite/dolomite/qtz-carb vein slightly brecciated and slightly lined with the orange/red "bacon mineral". There was also a very red hematitic? Alteration present within the +/- 6 cm vein which appeared to originate from a breccia clast

ankerite? Amphibole, unknowns, pyrite

55 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

16/07/11

S. Todd

L. Marshall

TR-11-PL-001

TR-PL-001-018

984575

518820

5431756

On thrust fault plane above

017

396

100

7 8 Same dark grey-blue amphibolite/ankerite host with minor ankerite veining, limonite weathering in fractures and exposed surfaces. There is a white ca-rich crust on some fracture surfaces as well, non-magnetic, HCl reactive. Also has an aphanitic blackish clast 2-3 cm wide

ankerite? Amphibole, unknowns, limonite.

90% recovery

18/07/11 M

. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-019

984577

518828

5431751

near fault

215

98 7 7 Mostly bacon with a small 15cm contact with amphibolite. The "bacon rock" fizzes weakly with acid. The red clasts are fgr w/ unknown minerals. There is a wt to lt gy area that weakly fizzes (possibly dolomite). Clasts are elongate and appear to be plastically deformed. in the red there is some dk gy metallic mienrals (perovoskite?). Minor limonite weathering on the surface. Amphibole is dk green to dk green gy.

unknwon red minerals, dolomite, perovskite, limonite

90% recovery

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-020

984576

518821

5431758

mid trench

198

82 6 7 Mostly amphibolite and local zones of pink mineralization and red with some vienings. Vienings fizzes slightly (dolimite). Within the vienins there are some red zones of mineralization. Within the red is some perovskite (fgr) and fgr pyrite. The amphibolite is dark green and very fine grained, too fine grained, One local area with a dark black mineral within the core.

Mostly amphibolite and local zones of pink mineralization and red with some vienings. Vienings fizzes slightly (dolimite). Within the vienins there are some red zones of mineralization. Within the red is some perovskite (fgr) and fgr pyrite. The amphibolite is dark green and very fine grained, too fine grained, One local area with a dark black mineral within the core.

95% recovery

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-021

984581

518820

5431758

mid trench

212

92 6 6 Mostly bacon rock. Localized area that fizz (dolomite) with red to red pink ineral that appears slightly elongated and irragular. Some dark grey metalic

90.00%

56 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

minerals (perovskite) and local finge grained pyrite. Near the end of the sample is a fine 2-3 cm layer of amphiblolite appears.

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-022

984582

518822

5431757

mid trench

214

120

6.5 5.5

Through the fault (apprx. 4 cm) appears to be white to grey dolomite (weakly fizzes) with cores of red mineralization, same as above. This is followed by amphibolite with some local zones of red mineralization with white veins

dolomite, amphiboles, unknown red minerals

Recovery due to being cut through a

fault, a lot of clay was washed

away. 70% 18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-023

984583

518823

5431755

mid trench

18 116

6 4 Amphibolite with cross cutting veins, composed of some dolomite (weak fizz) and irregular lines of red mineralization. In general, the veins seem thicker and more horizontal close to surface with smaller veins at steeper angles further at depths in the cut

amphiboles, dolomite, Recovery 90%

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-024

984584

518824

5431757

mid trench, vertical

cut through amphib

olite and

thrus fault

20 106

6 6 The amphibolite is dark green to dark green grey with fined grained and ore veinlets running through it. The veinlet is one cm including the alteration halo. At the margin of the vein is a pink red mineralization, throught he middle is fine grained pyrite and a black mineral (pyrolusite?) possible sphalerite. Where the cut hits the fault is heavily faulted amphibolite. This goes to a black colour then about 10cm of dolomite vein with red mineralization.

pink red mineralization, black mineral (pyrolusite?), possible sphalerite

80% recovery

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-025

984585

518820

5431752

mid trench

232

109

7.5 8 Mostly bacon rock. White part weakly fizzes (dolomite) with long elongated red clasts.

Minor galena, perovskite(?) and pyrite. Some amphibole at the end of the sample. Dolomite

Recovery 95%

57 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-026

984586

518817

5431750

mid trench

208

89 8 6 Some rubble has sluffed into the hole.Middle of the hole is heavily weathered with limonite fault (?). Most likely part of the fault. After the fault is mostly red to pink red mineralization, some white to grey that weakly fizzes (dolomite). Unknown red minerals.

Unknown red minerals, local perouskite and pyrite in the amphibolite is some minor red mineralization

Recovery 85%, around fault some

recovery lost

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-027

984587

518812

5431754

top trench, xcutting 1 fault

and breccia

252

110

7 4 hole x cutes 1 fault and 1 fault breccia. Fault is limonite altterd with a halo of white (no fizzing, still dolomite?) and red mineralization

The breccia is class supported. The clasts are limonite stained and altered, Clasts are subangular to subrounded. The matrix is quartz and carbonate. Some minor pyrite. In between the fault and the breccia is amphiblolite is dark green to dark grey green, fine grained with some local pyrite.

Recovery 85%, around fault some

recovery lost

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-028

984588

518817

5431750

top trench

254

99 7.5 7 Mostly pink to pink red bacon rock. The rock clasts and smaller and less elongated than previously described. Clasts are only about 1cm.

Withinthe matrix is possible dolomite, some possible hematite and pyrolousite (black to very dark purple) staining close to the surface. Some limonite alteration possible, perovskite and pyrite present. Localized areas where more weathering occurs.

Recovery 90%

18/07/11

M. Dalsin

D. Gritsaenko

TR-PL-11-001

TR-PL-001-029

984589

518811

5431749

top trench

226

124

7 4 mostly bacon rock with some amphibolite breccia at the top of the hole near the contact with fault and amphibolite. This area has some pink mineralization and dark bergundy mineralization

Some pyrite is present, within the rest of the breccia there is some dolomite (weakly fizzes), near hte bottom

Recovery 85%

58 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

there are fewer clasts and they are more regularly shaped. Others on and near the ceter of the fault have undergone more plastic deformation. The centre of the fault also has a fair amount of limonate staining.

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-001

985189

518811

5431748

North West

corner Near

top of hill

208

104

6.5 11

very mixed fault rock, dolomotic veins, altering to limotic veins indigo to light green host fg with hematic staining, some areas . Some area highly reactive to HCL, mostly aphanitic, non-magnetic

along fault

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-002

985190

518815

5431744

North West

corner Near

top of hill

230

104

8 10

Very limonitc, altered fault rock, primarily light brown , can have unknown dark green/black mineralization, as well as HCL reactive dolomite, non magnetic

90% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-023

985175

518806

5431741

North West

corner Near

top of hill

208

109

7 8 65 plag, 30 kspar, 5qtz, brown limonotic weathering around crystals, 1-2% pyrite mg to cg, no mag, no HCL reactivity, soft, not well indurated. Well fractured.

65plag, 30kspar, 5qtz. 1-2% pyrite mg-cg. No mag.

85% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-024

985176

518806

5431742

North West

corner Near

top of hill

188

100

7 9 80 plag, 15kspar, 5qtz, cg otherwise same as above. Limonitic/hematitic mineralization in veinlets. Also has minor intergranular black (amphibole?)

80plag, 15kspar, 5qtz, amphiboles?

85% recovery

59 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-025

985177

518806

5431743

North West

corner Near

top of hill

202

92 6.5 7 same as above, slightly more qtz. 80plag, 15kspar, qtz, amphiboles?

90% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-026

985178

518806

5431744

North West

corner Near

top of hill

214

93 7.5 7 much more qtz 50%, coarser grained. Same orientation passing through small fault fracture where the rock becomes black/green (amphibole) intergranular in place of limonitic, not HCL reactive, nonmagnetic

50% qtz, 40% plag, 10%kspar, amphibole? No mag.

90% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-027

985179

518808

5431746

North West

corner Near

top of hill

216

99 5.5 8 Cg – 10qtz 40 plag 50kspar, same orientation. Hematitic/limonitic veinlets and limonitic weathering around crystals. No fizz, non mag.

10qtz, 40plag, 50kspar. hematitic/limonitic veinlets

90% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-028

985181

518809

5431746

North West

corner Near

top of hill

226

93.5

7 7 Cg – 80 kspar, 15 plag, 5qtz, minor limonitic weathering around grains, light pasted green mineralization (intergranular) non mag no fizz.

80 kspar, 15 plag, 5qtz

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-029

985182

518808

5431739

North West

corner Near

top of hill

200

69 7 7.5

large qtz crystals (up to 1mm) – 30qtz 50kspar 20plag. Cg limonitic weathering in veinlets, no fizz, no mag, start of line cut top of SW corner

30qtz, 50kspar, 20plag, 95%-100% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-030

985183

518808

5431739

North West

corner Near

top of hill

206

58 7 8 same as above, 2mm qtz veins. Limonitic weathering around where it crosses a fracture, pyrite mineralization along hematized veinlets here too. Less plag, more kspar, end of line only 2 holes in this cut.

30qtz, 60kspar, 10plag, pyirte, hematization

90% recovery

60 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-31

985184

518808

5431744

North West

corner Near

top of hill

214

100

8.5 8 limonotic weathering also contains pastel green mineralization and closely associated with a minor whitish/cream mineralization which reacts readily with HCL. Hard to tell if it is the pastel green mineralization that is fizzing (calcite?) also has monor green/black mineralization amphibole?

10qtz, 50kspar, 30 plag, 5 mafic, 5other, limonotic weathering

90% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-32

985185

518810

5431749

North West

corner Near

top of hill

220

90 8 10

Limonitic weathering near fractures planes,qtz appears in veinlets

50kspar, 10plag, 40 either quartz or qtz has been altered to green mineral

85% recovery

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-33

985186

518808

5431748

North West

corner Near

top of hill

230

72 7 10

limonite (dark brown) weathering around grains, HCL reacts, non-magnetic

80kspar, 10 pastel green mineral, 5plag, 5 limonite

Top of fault

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-34

985187

518806

5431745

North West

corner Near

top of hill

230

81 8 10

beautiful rock, (marble like texture) light green, dark green, hematitic, lg qtz crystal, limonite (light brown,dark brown , pink) Fine grained

Fault Face

7/8/2011

L. Marshall

S. Todd

TR-PL-11-002

TR-PL-002-35

985188

518809

5431747

North West

corner Near

top of hill

208

106

8 12

fg primarily, aphanitic, blue/green/grey with dolomitic veinlets (HCL react) hematite? Stained in certain areas . Limonitic weathering new fault planes

along fault

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-001

985151

518856

5431724

244

63 7 7 Rockis moderately hard, but extensively fractured. Rock is dark and mafic looking some areas, highly magnetic, doesn't fizz with acid, medium to fine grained, crossed with more felsic veins, brecciated in areas (fault breccia?). Cut is located in close proximity to a vertical fault or lineament. Rock has been metamorphosed, but is probably sedimentary or volcanic in origin, it's crystalline, quite

Lots of pyrite, usually concentrated along beins, some of the veins are red, hematite alteration is present, quite oxidized on surface. Pyroxene,

Recovery: 80%. A vertical

systematic cut

61 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

silicious and oxidixed in areas. Also a light green mineral is present (epidote). Rock looks similar to a gabbro, but I can't ID plag.

chlorite are present. A light green mineral is also present (epidote???)

7/4/2011 B. Q

uist

L. Marshall

TR-11-PL-003

TR-PL-003-002

985152

518855

5431724

250

80 7.5 7.5

Rock is much coarser grained than TR-PL-003-001. Containes extensive veining (some plag, cross-cut by dark mafic veins), very magnetic with some small calcite veins that fizz with acid. Sample appears to cut through a vein. Some chlorite alteration present. Still no idea what the host rock is. Slight hematite alteration around some of the veins. Pyrtie and chacopyrite present (mainly in veins, but some is finely disseminated)

magnetite, chlorite, hematite alteration, pyrite, chalcopyrite

Recovery: 85%, a vertical

systematic cut

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-003

985153

518856

5431724

270

98 7 9 Dark grey vfg to aphanitic, magnetic, reacts readily with HCl. Limonitic weathering in fractures with occasional dark-green semi-fibrous (chlorite?) and minor lighter green/blue copper oxide staining. Sulphide-rich with occasional pyrite

magnetite, qtz, chlorite?, copper oxide, pyrite, limonite, very minor k-spar

Recovery: 95%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-004

985154

518857

5431724

248

66 7 8 Dark grey vfg to aphanitic, magnetic, reacts readily with HCl. Limonitic weathering in fractures with occasional dark-green semi-fibrous (chlorite?). Has iridescent green/yellow/olive (sulphide?) in fractures and very minor purplish (feldspar?), very minor pyrite, and very thin <0.25mm qtz-carb veins

magnetite, qtz, chlorite?, pyrite, limonite, sulphides?, qtz-carb

Recovery: 95%

7/4/2011 B. Q

uist

L. Marshall

TR-11-PL-003

TR-PL-003-005

985155

518854

5431720

280

70 8.5 10

Dark grey/green fg. The dark grey crystals are slightly larger <1mm than the greener crystals (amphiboles). There is a 1 cm qtz-carb vein and adjacent to it on either side is orange/red k-spar rich mineralization which decreases moving into the "host". The k-spar/qtz-carb can also occur within veins (smaller). Magnetic in certain areas, reacts nicely with HCl. Limonitic weathering and yellowish qtz in larger fractures.

Recovery: 95%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-006

985156

518853

5431720

264

59 7 9.5

Black, mafic looking, some finegrained, some medium grained, highly magnetic, felsic veins cross-cut sample (many look fich in k-spar). Some hematite alteration present. Doesn't fizz with acid. Some "epidote?" alt. Present, but it still looks a bit like a gabbro or a porphyry

Recovery: 95%

62 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-007

985157

518851

5431718

258

76 8 8 Another vertical cut (systematic), slightly finer grained than 008, more green looking chlorite (?) alt. Than before. Fizzes vigoursly with acid. Veined, but veins aren't cross cutting as much as before. Matrix/host rock is the same as before, no visible sulphides.

Recovery: 90%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-008

985158

518856

5431716

260

70 12 7 Part of rock is same host rock as before (dark, mafic, altered, chlorite, grey + dark greyish looking, magnetic); part appears to be very felsic (some qtz, K-fds); looks quite brecciated; small mafic veinlets (as before); pyrite cubes (~2mm) on felsic stuff; felsic vein is mainly med. grained sized).

Mafics, chlorite, magnetite, Qtz, K-fds, pyrite

Recovery: 95%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-009

985159

518854

5431722

265

80 8 7 vfg to fg dark grey to black and light grey-green, minor pyrite and blackmineralization in veins. Qtz-carb and orange k-spar occur in mm scale veins which randomly criss-cross. The light green mineralization also occurs in >mm veins and is disseminated throughout. Limonitic brown/rusty weathering in larger fractures.

qtz-carb, magnetite, and unknown

Recovery: 90%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-010

985161

518853

5431719

324

96 7 4.5

vfg to fg dark grey to black and light grey-green, minor pyrite and blackmineralization in veins. Qtz-carb or calcite and orange/red k-spar occur in >mm scale.. The light green mineralization also occurs in >mm veins and is disseminated throughout. Limonitic brown/rusty weathering in larger fractures. HCl reactive, magnetic

qtz-carb, magnetic, k-spar, calcite?

Recovey: 90%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-011

985162

518850

5431717

308

113

6 4.5

Systematic channel on a ~45 degree angle . Some aphanitic dark mafic host rock as before. Extensively cut by felsic veins, some chlorite alteration. Several of the veins are quite rich in hematite. Lightly magnetic, not fizzing with acid. Parts are quite silicious.

Recovery: 90%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-012

985163

518850

5431714

324

94 6.5 6 same matrix with host rock, but lots of altered hematized clasts; slight magnetic; fizzes with acid; vertical cut in a really fractioned area; Fault?; silicious in some areas; messed up breccia; oxidized; hematite alteration

Recovery: 90%

63 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-013

985164

518851

543174

308

68 6.5 6 fine grained, silicious, very crumbly, brecciated; super oxidized (red-brown in colour); a subvertical cut (systemcatic); hematite alteration; hematite alteration in veins; slight chlorite alteration; light rock (not very heavy

Recovery: 95%

7/4/2011 B. Q

uist

L. Marshall

TR-11-PL-003

TR-PL-003-014

985165

518851

5431712

318

102

8 6.5

Rock is much more competent; strong; oxidized on surface; but quite "fresh" inside; contains fine grained aphanitic magnetite, chlorite, alt. host that has been x-cut with flesic (K-fds rich) veins; some light green alteration present; sulphides are present, fine grained many pyrite; one really broght red (hematite) vein present that crosscuts everything; a vertical cut that's very close to the large, main fault on the trench; some of the small white veins are calcite (fizz with acid).

Recovery: 95%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-015

985166

518849

5431713

204

85 7 4.5

really weathered rock; altered; oxidized; lots of sulphides present; slightly magnetic; doesn't really fizzes woth acid; quite silicious looking in areas; large areas of pyrte or marcasite; pyrolucite staining present; lots of veins with altered rims; chlorite; hematite; iron oxide alteration; vertical systemtic cut that is~30 cm from large fault or fracture.

sulphides, py, marc, pyrolucite, chl, hem

Recovery:90%

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-016

985167

518850

5431712

240

72 7 6.5

This rock looks like the "bacon rock" with black/very dark green patches. The whitish/grey part of this wavy "interbedded" rock is primarily qtz (fg) with minor reddish/orange k-spar? The other patches consist mainly of fg k-spar and minor qtz. Qtz-carb appears very minor. the dark patches are aphanitic. magnetic/reacts slightly to HCl

qtz, k-spar, amphibole/magnetite?

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-017

985168

518854

5431713

240

88 8 7 pink clasts in a light green matrix; also dark clasts in a felsic matrix; some hematite alterations; slightly magnetic; slightly fizzes with acid; cerium staining (purple); occasional sulphide; 1.5 m from main fracture zone.

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-018

985169

518854

5431708

238

92 7.5 5 xenoliths of dark mafic rock in a fine grained felsic matrix with lots of hematite stained "layers" (thin bands); fizzes with acid; slghtly magnetic; some of the xenoliths are cut by felsic veins with green alteration halos; clasts are non-spherical; angular-subangular; breccia on vertical

64 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

systematic channel cut; finely disseminated sulphides; some cerium staining; lots oxides

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-019

985171

518853

5431708

270

94 7 4 rock is quite pink, massive, magnetic, fizzes with acid; x-cut; fine grained pyrit; rock is oxidized; finely disseminated sulphides; vertical systematic cut; hematite alt.; some purple (cerium rich?) stained, silicious looking areas+ dirty oxidized qtz

py, hem,

7/4/2011

B. Quist

L. Marshall

TR-11-PL-003

TR-PL-003-020

985172

251

92 7 6 much more felsic; lots of hematite alterations; slightly magnetic; some small areas fizz slightly; small mafic xenoliths present, because many veins are running in the same directionl rock almost looks banded; oxidized; rusty; meta-something; messed up rock.

7/21/2011 S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-001

985192

518721

5431829

This hole is

immediately

above 002 and comes out of mafic dyke.

84 100

7 8 Comes out of mafic dyke (5cm) into 50/50 orange fg k-spar and fg dk grey amphibolite? Non-Magnetic, slight HCl reaction.

k-spar, amphibole? 100% recovery

7/21/2011 S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-002

985193

518719

5431832

Transects a ~1m wide mafic dyke. North end of trench

90 97 7 9 Very dark grey aphanitic matrix with disseminated yet mostly aligned parallel to dyke walls, tabular plate-like vitreous greenish up to 1 cm diameter crystals (lucite nepheline?). Magnetic, HCl reactive.

unknowns, leucite? Nepheline?

100% recovery

65 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-003

985194

518717

5431826

crosses normal

fault zone

with 2 50cm fault

blocks.

280

94 7 8 Dark to lt grey, vfg to fg, equigranular amphibolite? The vfg makes a sharp contact with the fg and vfg slightly more magnetic (does not appear to be breccia). Newly cut/fractured surfaces are very HCl reactive. vfg contains minor black disseminated mafics. Limonite in faults.

mafics, unknowns, magnetite, limonite, amphiboles?

95% recovery

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-004

985195

518715

5431822

crosses a thrust

fault immedi

ately down from 003

272

104

7 6 Has a chaotic marble-like texture/pattern consisting of ark pink mineralization. Minor qtz/calcite and light pink blebs, Orange/red feldspar-like localized spotting. Limonitic vuggy weathering near fault and surface. Very minor mg chalcopyrite with dk grn and malachite colored blotches. Non-magnetic, very HCl reactive, also dk grn aphanitic localized mineralization with vfg pyrite.chalcopyrte.

Pyrite, chalcopyrite, unknowns, limonite, malachite, qtz carbonate.

85% recovery

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-005

985196

518719

5431821

foot of vertical 2m cliff. (hanging wall)

276

96 8 11

Dark to lt grey, vfg to fg, equigranular amphibolite? The vfg makes a sharp contact with the fg and vfg slightly more magnetic (does not appear to be breccia). Newly cut/fractured surfaces are very HCl reactive. vfg contains minor black disseminated mafics. Limonite in faults. orange mineralization in veinlets and bacon-like patterns.

mafics, unknowns, magnetite, limonite, amphiboles?

85% recovery

7/21/2011 S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-006

985197

518717

5431820

going up cliff

face immedi

ately above

005 (foot wall)

280

97 8 8 Dark to lt grey, vfg to fg, equigranular amphibolite? The vfg makes a sharp contact with the fg and vfg slightly more magnetic (does not appear to be breccia). Newly cut/fractured surfaces are very HCl reactive. vfg contains minor black disseminated mafics. Limonite in faults. orange (feldspathic) and red (hematitic) veinlets. Non-magnetic

mafics, unknowns, magnetite, limonite, amphiboles?, feldspar? Hematite?

85% recovery

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-007

985198

518710

5431818

crossing

surface of

thrust fault

20 105

8 7 45% aphanitic amphibolite located more in veinlike masses (chloritized?) more teal colored than blue, closer to riebekite found in trench 7. 45% k-spar (fg), 5% qtz(fg), 5% carbonate.Limonitic weathering in fractures, also localized vfg lime grn epidote? and sugary purplish mineralization, very HCl reactive.

amphiboles, unknowns, rebekite? Limonite, epidote? Qtz-carb

95% recovery

66 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

plane, south side of trench

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-008

985199

518708

5431817

across fault

plane.

12 105

8 9 equigranular fg 47% kspar, 47% qtz, 2% mafics, 2% carbonate, 2% limonite. (syenite/granite?). Up to 1 cm qtz/qtz carb veins with chlorotized (green) contacts, some veinlets completely chlorotized, HCl reactive.

k-spar, qtz, mafics, carbonate, limonite, chlorite?

95% recovery

7/21/2011

S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-009

984901

518710

5431821

crosses a

limonitic

fracture on top

of trench

50 95 7.5 9 equigranular fg 57% kspar, 57% qtz, 2% mafics, 2% carbonate, 2% limonite. (syenite/granite?). Up to 1 cm qtz/qtz carb veins with chlorotized (green) contacts, some veinlets completely chlorotized, HCl reactive.

k-spar, qtz, mafics, carbonate, limonite, chlorite?

90% recovery

7/21/2011 S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-010

984902

518710

5431822

immediately north of 009 crossin

g 2 faults/fracture

s.

50 100

8 7 Marble-like texture, local fg pyrite, mg chalcopyrite (minimal <1%). Teal vfg aphanitic mineralization interfingering, purple/red sugary mineralization with veinlike red mineralization in veins (hosting the sulphides). Limonitic vuggy weathering near surface with occasional <1cm indigo aphanitic blotches.

pyrite, chalcopyrite, unknowns, limonite

90% recovery

7/21/2011 S. Todd

L. Marshall

TR-PL-11-004

TR-PL-004-011

984903

518710

5431822

immediately north of 010 crossin

g 2 faults/fracture

s.

52 100

7 6 Marble-like texture, local fg pyrite, mg chalcopyrite (minimal <1%). Teal vfg aphanitic mineralization interfingering, purple/red sugary mineralization with veinlike red mineralization in veins (hosting the sulphides). Limonitic vuggy weathering near surface with occasional <1cm indigo aphanitic blotches.

pyrite, chalcopyrite, unknowns, limonite

90% recovery

67 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-001

984977

518669

5431838

West wall of trench

(vertical)

304

85 7.5 7 Amphibole on top (cantact) granite on the bottom. Amphibole is dk green/grey, vfgr to fgr, some small granite fragments. vfgr to fgr, dsseminated py, local vfgr cpy. Granite is pink and green w/some chlorite alteration (35%), pink is mostly k-spar, (50%), qtz (15%)

amphibole, pyrite, chalcopyrite, chlorite, k-spar, qtz.

95% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-002

984958

518668

5431837

30-40 cm

north of 001,

also vertical

310

89 7.5 7 mostly amphibolite (amphiboles and chlorite alteration. The bottom 40 cm is dk grn with some small local pods of red mineralization and vfgr disseminated py. The top ~50cm is green w/chlorite & epidote alteration. Fgr to mgr py & mgr to cgr cpy. There is qtz carb weakly brecciating locally, some local zones of red mineralization, limonite alteration, possible sphalerite & malachite at the surface.

amphibole, pyrite, chalcopyrite, chlorite, qtz, limonite, sphalerite? Malachite, epidote.

95% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-003

984979

518669

5431839

300

91 8 9 mostly pink to pink-red granite w/ interfingering of amphibolite. Granite is k-spar (70) qtz(20)plag(8)mafics(2). Minor local fg to vfgr py. Few qtz stringers, local chlorite alteration.

amphibilote, k-spar, qtz, plag, mafics, py, chlorite

100% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-004

984978

518671

5431842

Vertical cut on west wall.

Contact b/w

amphibole &

granite. Dipping

35 degrees

.

296

94 8 7 Amphibole is vfgr w/few fractures. Granite is pink w/kfspar (80) qtz(15)plag(3)mafics(2). Equigranular and fgr

k-spar, qtz, plag, mafics 95% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-005

984997

518676

5431840

On the ledge

next to vertical face of

east wall.

130

87 8 6 Vein breccia w/ qtz carb matrix, clasts are subrounded and irregular, clasts are pink red-pink & grn chlorite altered clasts, local epidote &limonite staining. Vfgr to fgr py, mgr to cgr cpy, local unkonwn black minerals infilling fractures. 1% cpy

qtz-carb, chlorite, epidote, limonite, py, cpy

100% recovery

68 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-006

984599

518822

5431840

on plan map and

cutting fault

136

94 7 10

granite (qtz syenite?). Fault is heavily weathered to an orange brown but still relatively solid. On either side of fault is pink granite (qtz syenite) mostly k-spar (75) w/ some qtz & plag (25%) w/ minor mafics.

qtz, k-spar, plag, mafics

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-007

984996

518820

5431840

On vertical

face

36 77 7 6 Vein breccia w/ qtz carb matrix, clasts are subrounded and irregular, clasts are pink red-pink & grn chlorite altered clasts, local epidote &limonite staining. Vfgr to fgr py, mgr to cgr cpy, local unknown black minerals infilling fractures. 1% cpy. Same as 006 with less pink mineralization, more epidote & qtz carb, local malachite staining on and near surface.

qtz carb, chlorite, epidote, limonite, py, cpy, black minerals, malachite

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-008

985191

518820

5431833

To the south of 010

and 009

2 96 7 11

Pink granite (or qtz syenite) equigranular, fgr, 80% kspar, 10% lt green alteration, 10% qtz, plag and mafics. Some limoonite on fractures, local fgr disseminated pyrite

k-spar, qtz, plag, mafics, py

85% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-009

984999

518672

5431837

on plan view.

40 100

8 9 Vein breccia w/ qtz carb matrix. Clasts are granite, pink, with mostly k-spar, some red mineralization infilling fractures. Mgr py & cpy. Some limonite infilling fractures.

qtz carb, red unknown, py, cpy, limonite

95% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-010

985189

518673

5431837

connected to 009

28 93 7 9 At the the edge of the breccia. Some weak breccia throught the granite (k-spar rich vein material is qtz carb). Some mgr cpy in the veins, local limonite on fractures, some possible pyrolusite on fractures.

k-spar, qtz carb, cpy, limonite, pyrolusite?

95% recovery

7/20/2011

M. Dalsin

S. Todd

TR-PL-11-005

TR-PL-005-011

984998

518673

5431830

at a 90 degree angle over

fault & cpy

breccia zone.

218

100

8 10

Calcite infilled fault breccia w/elongate plastically deformed green clasts w/ some red. Rest is brecciated with qtz carb. Vertical part has chl, epidote, red mineralization & some amphibolite clasts. Bottom is mostly k-spar rich granite clasts fgr disseminated py & mgr cpy

red unknown, green unknown, amphibole, k-spar, py, cpy

69 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-001

984979

518609

5431887

just above a highly

jointed/fractured fault zone

240

70 7 6 m.g. equigranular orange and light grey (~50% qtz, 50% k-spar). Small qtz veinlets and limonitic fractures, non-magnetic, no HCl reaction.

qtz, k-spar, limonite 90% recovery

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-002

984981

518608

5435888

Immediately

below TR-PL-006-001

crossing a fault

230

79 6 7 m.g. equigranular orange and light grey (~65% qtz, 35% k-spar). Qtz veins are larger and more abundant than TR-PL-006-001 and limonitic fractures, non-magnetic, no HCl reaction.

qtz, k-spar, limonite, pyrite

90% recovery.

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-003

984982

518608

5431888

Immediately

below TR-PL-006-002

crossing a fault

230

84 7 7 Runs into a fault containing a very large~50cm qtz vein with the following features: orange (k-spar?, yellow,clear, light grey dark grey and burgandy red (hematite) whispy inclusions. (marble-like), The middle of the vein contains a precarious ~5 cm green-yellow aphanitic mineralization (epidote, altered chalcopyrite?), The hole also contains an aphanitic dark grey rock with conchoidal fracturing that is also pyrite-rich.

qtz, k-spar, limonite, pyrite, chalcopyrite, unknowns

90% recovery

19/07/11 D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-004

984983

518604

5431983

Runs into a fault

containing a very

large 50 cm qtz

vein comple

x

230

78 7 8 m.g. ~65%qtz 35% k-spar. Some of the k-spar is quite orange and appears to be running parallel to qtz vein mineralization. (veins and veinlets appear in both massive and granular forms. Abundant pyrite/chalcopyrite 1-2%. Some fractures appear stained with limonitic and perhaps greenish chalcopyrite weathering, no HCl reaction, non magnetic.


85% recovery.

70 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-005

984984

518605

5431892

Runs across a faulted

area

230

78 6 8 massive ~ 80% qtz, 20% k-spar. Abundant pyrite/chalcopyrite 1-2%. Vuggy qtz where it is weathered and filled with limonite. Some qtz staining (perhaps by iron-copper sulphides? Minor carbonate associated with the qtz. (possible ankerite?)


85% recovery

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-006

984985

518603

5431898

Runs across a faulted

area

96 77 7.5 7 m.g. ~60% qtz/40% k-spar equigranular, some grains altered to limonite, minor pyrite, limonite in fractures, abundant qtz veins <1cm


90% recovery

19/07/11

D. Gritsaenko

L. Marshall

TR-PL-11-006

TR-PL-006-007

984986

518604

5431898

Between a

bifurcated fault

204

92 7 6 m.g. ~60% qtz/40% k-spar equigranular, some grains altered to limonite, pyrite, limonite in fractures, abundant qtz veins <1cm with carbonate.


90% recovery

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-008

984987

518600

5431897

west side of trench

83 7 5 x cutting a fault mostly weathered rock. Heavily/limonite altered visible rock/areas locally. Rock is chlorite altered with small 4cm hemattie altered clasts. Potential units local fgr disseminated pyrite

limonite, chlorite, hematite, pyrite flecs

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-009

984988

518602

5431897

west side of trench

128

92 7 6 at the bottom of the pit. Dk green mostly chlorite, altered rock w/.some fgr pyrite local zones of hematite staining (possible clasts?)

chlorite, pyrite, hematite?

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-010

984989

518601

5431897

west side of trench

154

74 7 7 goin through a fault/fracture zone. Local areas of heavily weathered to limonite zones. Some yellow weathering on the surface. The rest of the sample is qtz vein w/green breccia clasts. Clasts are altered chlorite and epidote. There is some limonite infilling fractures. There is a burgandy mineral rim around some sulphates and epidote clasts and chlorite. Fgr to mgr pyrite throughtout mgr chalcopyrite, fgr yellow sulphide (oxidized pyrite or chalcopyrite?)

limonite, qtz, chlorite and epidote, burgandy mineral? Sulphides, pyrite, chalcopyrite

71 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-011

984991

518601

5431897

west side of trench

154

88 10 9 the top of the cut xcuts a fault that is heavily weathered to limonite. remanent texture is some chlorite altered fragments and qtz. The rest is mostly qtz veins q/some areas of kfspr clasts that have been silicified (silicified weak breccia). Fractures are infilled with limonite (possible pyrolusite?) dk gy to burgandy mineral. Disseminated py throughout. Localized areas of epidote? Alteration

limonite, chlorite, qtz, silicified kspar, pyrolusite? Burgandy mineral? Epidote?

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-012

984992

518601

5431897

west side of trench

138

77 8 6 mostly a qtz vein w/some dolomite local areas of possible slicified kfspr clasts. Fgr disseminated pyrite throught some limonite and a black mineral on fractures. Possoble yellow/orange sphalierite on fractures. Local areas of stronger kspar.

qtz, dolomite, kfspr, pyrite, limonite, black mineral? yellow/orange sphalierite

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-013

984993

518596

5431893

west side of trench

120

71 6 5.5

xcuts a small fault that consists mostly of gaige and limonite/altered rocks ]. the rest of the sample is mostly qtz on w/some possible dolomite. Qtz is fractured with limonite or a black mineral (pyrolusite?) small kfspr clasts that may have undergone silicification for disseminated pyrite. Possible yellow/orange sphalierite on fracture surfaces.

gaige, limonite, qtz, possible dolomite, pyrolisite? Kfspr, sphalerite

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-014

984994

518604

5431902

fenced off area

of trench

230

102

6.5 7 weak breccia zone w/kfspr and qtz rick areas. Where a small fault xcutes the hole the rock is heavily limonite stained. There is fgr disseminated pyrite throughout. Some fractures have limonite staining where as others are infilled w/possible pyrolusite. One small local zone w/green staining. Posible minor sphalierite

kfspr, qtz, limonite, pyrite, pyrolusite? Sphalerite?

19/07/11

D. Gritsaenko

M. Dalsin

TR-PL-11-006

TR-PL-006-015

984995

518606

541907

fenced off area

of trench

232

100

7 5 bottom cut intersects limonite altered fault. Top is mostly pink granite (probably a quartz syenite?) motly kfspr w/some qtz and mafics. Local fgr pyrite some possble pyrolusite. Some lt green alteration of some minerals.

limonite, qtz, kfspr, mafics, pyrite flecs, possible pyrolusite

6/27/2011

B. Quist

TR-PL-11-007

TR-PL-007-001

985051

518735

5431992

on vertical

face; vertical sample to get

an idea

0/180

70 7 6.5

dark mafic minerlas; magnetic (Hem/Mag); qtz; plag; weathering seen on finely dissemnated pyrite surface; unknown pink minerals; green stringers throughout

mafics, Hem, Mag, Qtz, Pl, Py, pink and green minerlas?

72 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

of depth of REE

minerals

6/27/2011

B. Quist

TR-PL-11-007

TR-PL-007-002

985052

518748

5431990

near 18m at 90 deg.

to S true

24 126

7.5 8 finely disseminated Py; not magnetic; not fizzes with acid; unknown red-pink minerlas; unknown green/blue fibrous minerals

6/27/2011 B. Q

uist

TR-PL-11-007

TR-PL-007-003

985053

518751

5431993

perpendicular

to structur

e; cross-cuts a really dark spot

24 110

8.5 dark green/black minerals (chlorite?); epidote; very weakly magnetic; fizzes with acid; small unknown pink minerals; crosses a fracture into extensive veining; same red green rock as before but with more qtz

Chl?, Epdt, pink and green minerals, Qtz

6/27/2011

B. Quist

TR-PL-11-007

TR-PL-007-004

985054

518739

5431994

20 120

8.5 7 sulphides along fracture planes; very layered; two distinct units: 1-red and green (as before), 2-purple fine grained looks slightly silicious; blue green alterations around red zones (green layers)

sulphides, greens, reds 90%

6/27/2011

B. Quist

L. Marshall

TR-PL-11-007

TR-PL-007-005

985055

518738

5431996

entire trench (small)

50 103

8 7 Across large pyrites (some oxidized, and appear to have formed last). Recovery ~98%. Two layers again. Red/green and purple, purple looks fine grained, layered, almost sedimentary, same features as previous descriptions

6/27/2011

B. Quist

L. Marshall

TR-PL-11-007

TR-PL-007-006

985056

518745

5431994


70 110

6.5 5 Across an ~ 12cm wide amphibole? Dyke (dark grn 60/120 cleavage, contains small amts of sulphides, magnetite. Dyke crosses the same red/green 'host' rock as before.

pyrite, magnetite

73 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/27/2011

B. Quist

L. Marshall

TR-PL-11-007

TR-PL-007-007

985057

518746

5431994


120

Vertical channel across cleavage face running 30 degrees, should give good insight into vertical extent of mineralization. Appears to be mainly red/green (pink) "host rock" with layer ~52-68 cm from the bottom that contains clue/green fibrousradiating mineral. Red/green rock looks slighlty more silicious than before.

6/27/2011

B. Quist

L. Marshall

TR-PL-11-007

TR-PL-007-008

985058

518754

5431993


20 108

8 6.5

crosscuts 2 small dark veins running 70 and 104 degrees respectively. Dark veins are slightly magnetic, fizz a little with acid, look similar to 006 amphibole. Most minerals are oft enough to scratch with tungsten carbide tip. Portions of the red/green rock are quite felsic looking (qtz/plag?)

qtz plag

6/27/2011

B. Quist

L. Marshall

TR-PL-11-007

TR-PL-007-009

985059

518759

5432000


50 130

8 6 Rock is different but difficult to locate contact. Much softer/weaker. Lots of oxidation &clay. Fizzes w acid. Fine grained. Not really magnetic. Strange dark purple mineral (fluorite/fluorapatite?), green mineral (fluorite?). Lots of phyllosilicates in areas (biotite). Also a peach-colored mineral almost imparting schistosity

6/28/2011

L. Marshall

A. Ya’acoby

TR-PL-11-007

TR-PL-007-010

985061

518754

5431992

small single

cut near

south east

corner

106

119

7 5 Red "host-rock", almost like a hematite-rich feldspar with disseminated or sporadic blue-grey fibrous mineralizationwhich also appears in thin veins and in fracture or cleavage planes. Has minor pyrite, qtz, and fairly abundant limonitic weathering.

minor pyrite, qtz, limonite, and unknowns

~96% recovery

6/28/2011

L. Marshall

A. Ya’acoby

TR-PL-11-007

TR-PL-007-011

985062

518736

5431987

first sample

on bottom of long cut on

far west side.

183

133

7 8 Similar to above with generally more qtz and minor biotite. minor pyrite, qtz, limonite, boitite and unknowns

~96% recovery

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-012

985063

518732

5431989

first 5m of the

line

183

146

6.5 4.5

green/blue fairly fine grained and fibrous mineralization intertwined with larger red minerals. Blue/green fibrous mineral appears in thin veins/fracture planes also.

chlorite?quartz,kspar?garnet?

74 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-013

985064

518735

5431987

first 5m of the

line

183

151

7.5 5 same as TR-PL-007-012, but blue/gray mineral more clearly fibrous and slightly larger percentage

chlorite?quartz,kspar?garnet?

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-014

985065

518738

5431987

first 5m of the

line

183

150

7.5 7 same as TR-PL-007-012,but smaller percentage of blue/green mineral

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-015

985066

518735

5431991

first 5m of the

line

183

185

5.5 5 coarse grained rock made of qtz, red minerals and black minerals (amphiboles). Equigranular, but black is thinner

qtz, kspar?garnet?amphiboles, biotite

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-016

985067

518735

5431994

first 5m of the

line

183

157

5 4.5

generally equi-granular texture, showing green/blue red minerals, some qtz present. green/blue min tend to concentrate in veins and along cleavage planes. Few or less dark minerals

chlorite, qtz, possibly hematite, amphiboles, others

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-017

985068

518735

5431996

first 5m of the

line

183

155

6 5 same as TR-PL-007-016 but with minor pyrite grains chlorite, qtz, possibly hematite, amphiboles, pyrite, others

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-018

985069

518736

5431996

first 5m of the

line

183

85 6 6 red mineralization and qtz crystals are larger than green and black crystals. Otherswise same as TR-PL-007-016

chlorite, qtz, possibly hematite, amphiboles, others

6/28/2011

D. Gritsaenko

L. Marshall,

A Ya’acoby

TR-PL-11-007

TR-PL-007-019

985074

518740

5431986

first 10m of the line

183

144

7 5 coarser grained, red minerals, qtz, finer green/blue mins which also occur in veins and tend to concentrate along cleavage planes. white/lighter colours zones in rock fizz qith acid indicating carbonate mins. Majority is blue/green (aprox 70%?)

chlorite? Qtz, carbonates, kspar?

fizzes!

75 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

D. Gritsaenko

A. Ya’acoby

TR-PL-11-007

TR-PL-007-020

985075

518741

5431988

183

146

8.5 3.5

coarse grained; mostly red/brown minerals (possibly garnet and other); fibrous green and blue minerals are fine grained; fairly equally distributed; fibres tend to concentrate in veins and cleavage planes; minor qtz; fizzes on white areas, suggesting carbonates; non magnetic.

qtz, carbonates, reds, blues

80%

6/29/2011

D. Gritsaenko

A. Ya’acoby

TR-PL-11-007

TR-PL-007-021

985076

518740

5431987

183

155

5.5 7.5

coarse grained; mostly red/brown minerals (possibly garnet and other); fibrous green and blue minerals are fine grained; fairly equally distributed; fibres tend to concentrate in veins and cleavage planes; minor qtz; fizzes on white areas, suggesting carbonates; non magnetic.

qtz, carbonates, reds, blues

80%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-022

984964

518742

5431990

hole on west side,

meridional

178/358

147

9 9 medium to coarse grained rock; granitoid; large greenish/turquoise grains, fibrous (chlorite?); plag; K-fds; qtz; areas with small darker crystals (garnets and asmphibole); no fizz; non magnetic

Chl, Pl, K-fds, qtz, gar, amph,

95%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-023

984965

518743

5431991

extension of

current channel

to North

178/358

140

7 7 same as before; more purple-brownish fine to medium grained zones; green minerals concentrated in veins and cleavage planes; no fizz; non-magnetic; sulphides are present mostly pyrite.

Chl, Pl, K-fds, qtz, gar, amph, py

95%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-024

984967

518743

5431993

extension of

current channel

to North

144

6 8 same as before; no pyrite; slight fizz with acid; non-magnetic

Chl, Pl, K-fds, qtz, gar, amph, slight carbonates

80%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-025

984968

518743

5431993

extension of

current channel

to North

153

7 8 same as before; more fed crystals and fine dark brown grains

Chl, Pl, K-fds, qtz, gar, amph, slight carbonates

90%

76 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-026

984969

518741

5431994

extension of

current channel

to North

150

6 5 same as before; more green minerals alterations Chl, Pl, K-fds, qtz, gar, amph, slight carbonates

80%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-027

984971

518740

5431997

extension of

current channel

to North

145

5 5 same as before; more pyrite present Chl, Pl, K-fds, qtz, gar, amph, slight carbonates; py

90%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-028

984972

518740

5431998

extension of

current channel

to North

151

6 6 same as before; little pyrite present Chl, Pl, K-fds, qtz, gar, amph, slight carbonates; py

95%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-029

984973

518737

5431995

extension of

current channel

to North

same Chl, Pl, K-fds, qtz, gar, amph, slight carbonates; py

75%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-030

984974

518739

5431999

extension of

current channel

to North

153

6 5 same; less py Chl, Pl, K-fds, qtz, gar, amph, slight carbonates; py

80%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-031

984974

518739

5431999

extension of

current channel

to North

77 5 6 same; very little py Chl, Pl, K-fds, qtz, gar, amph, slight carbonates; py

80%

77 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-032

984501

518745

5431988

Bottom of line 3

2 OR 182

134

4.5 6 Same red/green-blue rock. The red mineral could possibly be garnet or ankerite? The blue/green is fibrous, radiating, scratches and could possibly be aurichacite or wavellite (it's def an alteration mineral and it occurs mainly as sheets or friable layers between more solid layers composed mainly of the red mineral and a different green mineral ). Some k-spar present, no visible sulphides present in this sample. Layered with the fine-grained purple rock (purple may be hematite alteration), contains pyrite.

Systematic trench with

95% recovery. Bottom of

line 3

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-033

984502

518747

5431989

356

OR 176

151

5 6 Same red/green-blue rock (as previously described), interlayered/interfingered with the fine-grained purple (hematite stained?) rock. More pyrite concentrated along veins

systematic trench with

95% recovery

6/30/2011

A. Ya’acoby

TR-PL-11-007

TR-PL-007-034

984503

518747

5431990

357 or 177

138

6 8 sampling 3rd cut channel from west side of outcrop; channel parallel to previous ones (meridional orientation); as before, channel cuts perpendicularly several main joints or contact lines; 034 is the third segment on channel from south

massive granitoid with brilliant display of red-brown crystals; crystalline; equigranular texture; coarse grained (2-3 mm); no fizz; non-magnetic; fairly silicious with lots of qtz; K-fds; finer dark biotite and possibly hornblende grains; hematitic staining; many of the red-brown minerals look like garnet but most likely are not garnet; otherwise most red minerals are unknown; elongate planes in rock tend to concentrate greenish-bluish fibrous minerals and possibly chlorite;

95%

78 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

lots of alterations

6/30/2011

A. Ya’acoby

TR-PL-11-007

TR-PL-007-035

984504

518746

5431990

4th segmen

t on channel

from south.

357 or 77

139

6 9 no fizz; non-magnetic; granitic rock similar to previous one; except more dark or black mafic minerals (mostly biotite) that tend to concentrate in veins.Qtz; K-Fds; Bt; Hbl; Hem; Gar?; reds, blues, Chl?

95%

6/30/2011 A. Ya’acoby

TR-PL-11-007

TR-PL-007-036

984505

518746

5431991

5th segmen

t on channel

from south

357 or 77

143

7 7 mostly coarse grained granitoid as before, except grains are larger reaching 4-5 mm in length; zones with fine brownish-purpulish crystals that fizz with acid (associated with carbonates); also green-blue fibrous radiating minerals along cleavage planes; non magnetic; some hematitic alterations present; some of the red minerals form xenolith-like appearance (could be forms of cumulates or breccia ion host granitiod rock); sulfides present with pyrite grains; someveins consist of brown powdery clay-like mineral that resemble finely ground coffee (limonitic weathering) Qtz; K-Fds; Bt; Hbl; Hem; Gar?; reds, blues, Chl? Py, sulfides, lim

80%

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-037

984506

518747

5431995

356

OR 176

151

6.5 6 same red/green-blue rock as before. A fracture crossing the channel runs 110 degress, ruock beside fracture is extremely hard, pruple, silicious looking with hematite staining. In fracture, rock is oxidized, weak, high scinting. Some sulphides are present in the wall rock, fizzes slightly with acid, slightly magnetic

systematic channel, but it does cross

a fracture running 110

degrees 6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-038

984507

518746

5431995

356

OR 176

149

6.5 5.5

Rock again is significantly harder than what is typical for this trench. More silicious, lot so of the blue fibrous, radiating mineral on fracture surfaces. Same red mineral as before. Small amounts of pyrite, but not as much as further down this line. Rock crosses another high scinting fracture zone. zone is weak, oxidized and crumbly.

pyrite systematic channel

79 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-039

984508

518748

5431997

0 OR 180

144

6 7 Rock has changed into more of a granite or quartz-syenite (gradualy transition, not a sharp boundary). Contains k-spar, qtz, and a light green alteration mineral (looks kinda like malachite staining), some of the k-spar crystals are up to 8mm long, slight oxidation of unknown mafic minerals on surface. No visible sulphides

systematic channel

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-040

984509

518745

5431999

0 OR 180

149

7 6 very similar to TR-PL-007-040, Grades from the "granite" into back into the red and green rock. Does this mean that the unknown red/pink mineral is actual k-spar? Some of the same blue/green radiating fibrous mineral on cleavage or slip planes No visible sulphides.

systematic channel

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-041

984511

517846

5431999

0 OR 180

154

7 6.5

same red/pink and blue/green minerals as before. The blue/green mineral appears to be concentrating in the fractures and veins, giving the rock a brecciated look (although it isn't a breccia), very few visible sulphides and when they do occur, they are finely disseminated

sulphides systematic channel

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-042

984512

518746

5432000

6 OR 186

143

5.5 5.5

Rock is a bit coarser grained (up to a cm in places) and contains a light pink and a dark pink mineral, a bit more quartz presnt. There is also a green mineral present in the red rock.

See B. Quist's notes for sketch,

systematic sketch, 95%

recover 6/30/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-043

984513

518745

5432003

2 150.5

5 5 fizzes with acid; non-magnetic; coarse grained; equigranular; most grains 2-4 mm; largest are K-fds 0.5-1cm; lots of qtz 3-4mm; more of the typical granite; still lots of red minerlas but fewer green-blue fibrous radiating mineral than before; overall channel has same rock but with large compositional variations and alterations throughout; also present in rock biotite and plag.

K-fds, qtz, blues, reds, Bt, Pl

90%

6/30/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-044

984514

518747

5432007

360

247

7.5 5 not much different than before, but with less Qtz; Biotite tends to form lines or veins reflecting matemorphic processes; lots of alterations; lots of hydrothernal activity; Calcite present

K-fds, qtz, blues, reds, Bt, Pl, Cal

90%

80 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-045

984515

518750

5431983

0 OR 180

137

5.5 5 finer grained than top of line 3 (TR-PL-007-044), some of the green alteration staining looks like malachite (but copper doesn't really make sense with this setting), fizzes slightly with acid

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-046

984516

518751

5431987

0 OR 180

144

5.5 6 brecciated red/blue with pyrite concentrated along fractures. Rock is more brecciated in this part of the outcrop than before

See B. Quist's notes for sketch,

systematic sketch, 95%

recovery. 6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-047

984517

518749

5431989

0 OR 180

154

5.5 6 rock is cleaving out easily and in laters that look almost brecciated. Blue alteration mineral along fractures. "Clasts" of the red/green in the fine grained purple, whcih means that the purple stuff is not sedimentary. Some of the purple has small red minerals in it. Sketch in notes explains it better. a new rock type present: dark, fine-grained, non-magnetic, small red specs in it and small elongated, bladed crystals that are an orange colour

90% recovery, see

B. Quist's notes for

sketch

6/30/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-048

984518

518751

5431990

sampling 4th

channel from the

western end

of outcrop; 048 is the 4th segment from south

on channel; similar trends

356

145

6.5 6 pegmatitic granite clasts embedded in aphanitic greenish-bluish mineralized host; quite brecciated appearance; granitoid clasts have some qtz, plag, K-fds, Biotite, amphibole; fine texture host has chloritic areas + hematitic alterations; silicious zone; rock fizzes (some carbonates present, likely calctie); non-magnetic; biotite veins; busy rock!

K-fds, qtz, blues, reds, Bt, Pl, Cal, hem, chl, amph.

80%

81 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

as in previoi

us channel

6/30/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-049

984519

518748

5431992

4 147

5 5.5

similar characteristics to 048; larger green grains aggregating around red minerals; larger phylosilicates or biotite grains; lots of hydrothermal activity; also lenses of yellowish minerals radiating inward toward a common centrepoint as in a geode but without hollow cavities; biotite veins; lots of hydrothermal activity

K-fds, qtz, blues, reds, Bt, Pl, Cal, hem, chl, amph, yellowish minerals (geode like)

85%

6/30/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

TR-PL-007-050

984521

518750

5431993

360

147

4 5 back to granite; non-brecciated; more equigranular grains; medium graines; less altered; still quite silicious; biotite aggregates; hematitic and chloritic staining; usual green and red unfamiliar minerals.

90%

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-051

984522

518750

5432001

8 146

5.5 7.5

coarser grained, rock has transitioned into having more quartz, more plag, alteration mineral is green, not blue like before. Occasional plag crystal >1cm, no visible sulphides, but green-malachite looking weathing in fractures suggests sulphides, possibly chalcopyrite, also some hematite staining. Recovery 95% systematic channel.

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-052

984523

518749

5431997

4 OR 184

144

5.5 6 slightly finer grained than before, quite a bit of quartz (30% qtz, 55% k-spar?, 15% mafic (unknown, but weathering green), grain size ~3-5 mm), zone of massive biotite, possibly some hornblende)

systematic channel TR-PL-007-052

and Rock Sample TR-PL-007-052

6/30/2011

B. Quist

G. Quist

TR-PL-11-007

TR-PL-007-053

984524

518750

5431996

4 OR 184

143

6 6 systematic channel that goes up a vertical face, crystalline, medium grained, lots of red mineral, plus a bit of plag, plus blue/green fibrous mineral, fizzes quite a bit with acid same blue/green and red rock as before

TR-PL-007-053 and Rock

Sample TR-PL-007-053

82 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-054

984525

518750

5432001

Sampling 4th

channel from

western end

of outcrop

; channel runs N-

S, cutting trhough several joints

and/or contact

lines; overall

massive granitoid rock.

8 146

5.5 7.5

slight fizz; non-magnetic; granitoid with medium to coarse graines; crystalline grains 3-4 mm; Qtz~10%; K-fds~20%; reddish crystals (rhodonite?)~30-40%; green fibrous radiating mineral (Pyrolusite?) +chlorite~35%; not much plag; some sulfides (Pyrite); brown limonitic weathering in veins; chlorite+hematite alterations

Pl, Qtz, K-fds, Reds, greens, Chl, Py, Lim, hem, some carbonates

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-055

984526

518749

5432001

4 142

5.5 8 granite; coarse grained to 5mm; slight fizz; non-magnetic; felsic appearance; Qtz~30%; Pl~10%; Bt~2%; Hbl~1%; K-fds~10%; 30% are reddish crystals (look like rhodonite); 10% are green prismatic mineral + chlorite; hematitic staining; minor pyrite

Pl, Qtz, K-fds, Reds, greens, Chl, Py, hem, some carbonates

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-056

984527

518750

5432002

348

146

6 5.5

Granitoid more altered than previous segment, with variations in texture, veining and composition; high hydrothermal activity; fine to medium sized grains; Qtz~25%; Pl<2%; Reddish crystals~30%; green fibrous mineral and Chlorite~20%; K-Fds~20%; rock appears to have layers of red and green minerals; hematicized and chlorotized; not much sulphides present

Qtz, K-fds, Reds, greens, Chl, hem,

83 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-057

984528

518748

5432004

350

150

7 7.5

granitoid turns more mafic with a lot of biotite which tends to concentrate on veins that are a few mm thick but 5-10cm wide (layered); medium to coarse grained rock; Biotite~25%; Qtz~10%; Plag<5%; K-fds~10%; reds~20%; greens+chl~15%; hematitic+chloritic alteration; limonitic weathering mainly in biotite veins.

Bt, Qtz, Pl, K-Fds, Reds, Greens, Chl, Hem, Lim

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-058

984529

518752

5432006

356

145

7.5 5 Similar granitoid rock to previous segment, with a lot of hydrothermal alterations and oxidation, and variations in texture and composition; parts of rock are darker and more mafic looking; coarser grains to 1 cm; green-blue fibrous minerals tend to concentrate in veins; no fizz; non magnetic.

Bt, Qtz, Pl, K-Fds, Reds, Greens, Chl, Hem, Lim

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-059

984531

518754

5431989

On north

trending line,

start of line 5,

limonitic/fractu

red bottom

/

0 130

6.5 6 vfg to fg qtz k-spar and blue/grey/green fibrous (chlorite?), minor pyrite, and limonitic brown weathering in fractures.

qtz,k-spar,pyrite,limonite, chlorite?, and unknown

80% rec 0695, 0717

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-060

984532

518755

5431993

continuing up from 059,

minor fracturi

ng

0 141

7 6 same as above with minor pyrite in fractures in conjunction with limonite

qtz,k-spar,pyrite,limonite, chlorite?, and unknown

90% rec 0696, 0717

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-061

984533

518757

5431993


minor fracturi

ng

3 144

6.5 6.5

pink K-sapr, qtz, minor plag, minor biotite, blue/green/grey (chlorite-like) secondary mineralization. Nearly equigranular, HLC reactive, limonite/hematitic weathering in fractures. Also, as in 59 and 60 the fiberous b/g/g mineral tends to appear in fracture walls but apears as intergranular grains on cut surface with minimal connectivity.

qtz,k-spar,limonite, chlorite?, and unknown, minor biotite, minor plag

95% rec

84 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-062

984534

518756

5431993


minor fracturi

ng

0 147

7 7 Little to no faulting/fracturing mostly massive. K spar qtz and chlorite-like mineral, equigranular on cut surface. Same of the chlorite-like fibrous mineralization appears in small radiating clusters and is likely a deff mineral than chlirite. Large 2 cm calcite surficial cluster on broken surface. minor plag and altered green/black biotite.

qtz,k-spar,limonite, chlorite?, and unknown

95% rec 0642, 0649

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-063

984535

518756

5431997


minor fracturi

ng

0 131

6 6.5

very coarse grained granite/pegmatite with lg ~cm k-spar & intersertal? Qtz with minor biotite/plag. Green/Blue fibrous mineral present in same previous forms. Limonitic weathering (minor) in fractures, minor calcite.

k-spar,qtz, minor biotite, minor plag, unknown

95%rec 0644, 0650

7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-064

984036

518759

5431993


minor fracturi

ng

1 142

6 7.5

cg K-spar/qtz/minor plag/minor bio. Most biotite appears altered to the blue/green/grey radiating fibrous mineral. HCL reactive, minor limonitic weathering

in description 95% rec 0645, 0651

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-065

984537

518756

5431998

5th channel

from western end

of outcrop

358

148

6.3 7 no fizz; non magnetic; granite; medium grained; fairly equigranular crystals; Qtz~20%; K-fds~40%; Bt~15%; Pl<5%; Biotite in veins + peppered throughout; chloritic alteration; green-bluish fibrous minerals~10%; reddish minerals~10%

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch

7/2/2011 L. M

arshall

G. Quist

TR-PL-11-007

TR-PL-007-066

984538

518759

5431998

across a fault

zone in line with 063

2 147

7 6.5

Same as TR-PL-007-064 with highly limonitic weathering . 95% rec The fibrous mineralization is primarily in layers (as with previous samples), but the greener mineralization is more intergranular (partially chlorite?) There is also sl=mall layers of vfg dark purple mineralization. A redder hematized K-spar appears frequently in conjunction or adjacent to the limonitic horizons. and the purple mineralization occurs with the common sheeted/intergranular green/grey/blue fiberous

in description 0646, 0652

85 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

mineralization as well. 92% rec

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-067

984539

518756

5431999

Segment

crosses 3 joints

6 147

6.5 7 no fizz; non magnetic; granite; Qtz~20%; Pl<5%; K-fds~30%; Bt~10%; green-bluish mineral+chlorite~10%; similar rock to previous segemet but with sulphides present (minor amounts of pyrite)

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch, Py

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-068

984541

518757

5432001

340

150

6 6.5

Same as before but with more green alteration and mineralization


7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-069

984542

518757

5432004

Segment cuts

through a joint

360

148

7 6.5

Generally same as 069 and 070 but with even more green alteration; limonitic weathering in biotite veins; more Pyrite present than before; no fizz; non magnetic


7/2/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-070

984543

518759

5432005

End of line 5

2 110

7 6 cg K-spar/qtz/minor plag/minor bio. Most biotite appears altered to the blue/green/grey radiating fibrous mineral. HCL reactive, minor limonitic weathering

in description 95% rec 0647, 0653

7/2/2011 A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-071

984544

518762

5431991

Last channel

(on eastern-most side of

outcrop)

354

146

6.5 5.5

Highly alteres and variable; parts of rock show granitic textures and mineralogy as in 069-071 (Qtz~20%; Plag~5-10%; K-fds~15%; Biotite~5%; green minerals~10%; red minerals~10%); other parts of roxk have much more darker green minerals, mostly in veins; also reddish veins consisiting of K-fds and other red mineral; biotite tends to form schistosity; green-blue minerals are fibrous +radiating+mostly in veins and cleavage planes; sulphides are also present; limonitic weathering; a few hornblende crystals in granitic parts

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch, Py, Hbl

86 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-072

984545

518760

5431991

360

144

6.5 6.5

Highly alteres and variable; parts of rock show granitic textures and mineralogy as in 069-071 (Qtz~20%; Plag~5-10%; K-fds~15%; Biotite~5%; green minerals~10%; red minerals~10%); other parts of roxk have much more darker green minerals, mostly in veins; also reddish veins consisiting of K-fds and other red mineral; biotite tends to form schistosity; green-blue minerals are fibrous +radiating+mostly in veins and cleavage planes; sulphides are also present; limonitic weathering; a few hornblende crystals in granitic parts but with more sulphides+brown reddish fine crystal quarts (smokey)

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch, Py, Hbl

6/15/2011

L. Marshall

G. Quist

TR-PL-11-007

TR-PL-007-073

984546

518762

5431994

On line 6

through weathe

red zone.

174

174

7 6 Cut starts in south with vfg purple mineralization with minor qtz (5-10%). This section runs through a bit of a limonitic zone, then the hole transisions into th fg/mg red/pink/orange k-spar and now contains the b/g/g/ fibrous mineralization in fractures and intergranular as well, minor qtz <5%. All samples react with HCL.

in description 92% rec

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-074

984547

518763

5431996

360

151

7 5 Medium to coarse grained granitoid with lots of red and green crystals; lots of the green-bluish radiating minerals are in veins, showing limonititc weathering; Qtz~5%; K-Fds~10%; Plag<2%; Biotite~1-2%; Reds~50%; greens~30%; slight fizz (some carbonates); non magnetic; few pyrite grains.

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch, Py, carbonates

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-075

984548

518763

5431999

segment cuts

through a joint

fracture

346

145

6.5 5 Medium to coarse grained granitoid with lots of red and green crystals; lots of the green-bluish radiating minerals are in veins, showing limonititc weathering; Qtz~5%; K-Fds~10%; Plag<2%; Biotite~1-2%; Reds~50%; greens~30%; slight fizz (some carbonates); non magnetic; few pyrite grains.


7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-076

984549

518756

5431994

segment cuts

through a joint

355

154

7 6 Medium to coarse grained granitoid with lots of red and green crystals; lots of the green-bluish radiating minerals are in veins, showing limonititc weathering; Qtz~5%; K-Fds~10%; Plag<2%; Biotite~1-2%; Reds~50%; greens~30%; slight fizz (some carbonates); non magnetic; few pyrite grains.


87 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-077

984551

518758

5432000

segment cuts

through a

fracture

2 132

7 6 coarse grained; equigranular crystals; crystalline granite; less altered and more homogeneous texture and compositions through out segment; no fizz; non magnetic; Qtz~35%; Pl~10%; K-fds~20%; Biotite~2%; green minerals~10%; other red minerals~10%

Bt, Qtz, Pl, K-Fds, Reds, Greens, Ch,

7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-078

984552

518762

5432003

2 144



7/2/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-007

Tr-PL-007-079

984553

518763

5432008

360

140



6/28/2011

B. Quist

TR-PL-11-008

TR-PL-008-001

985071

518630

5432084

vertical channel

350

144

7 6.5

fizzes slightly; non magnetic; looks similar to rock at TR-PL-11-007; more granitic; qtz; plag; k-fds; chlorite alteration? (green oxidation mineral; dirty rock; lots of oxidation and green mineral alteration; hematite staining; then little blevs of stained uraninite?; slightly magnetic at bottom.

Qtz, Pl, Chl?, Hem, Ur?, 0587; 0588

6/28/2011

B. Quist

TR-PL-11-008

TR-PL-008-002

985072

518619

5432084

vertical channel

55 90 6.5 6 fizzes with acid; very slightly magnetic; bright yellow minerals again but quite rare in this sample; green alteration minerals (dark); red mineral (unknown); altered oxidized, hematitic staining

6/29/2011

B. Quist

D. Gritsaenko

TR-PL-11-008

TR-PL-008-003

985073

518632

5432093

south side of

fracture running down

the hill

4 85.5

8 5.5

felsic granite, veined, non magnetic, non acidic, Qtz (30), plag (20), kspar (50)

90%

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-008

TR-PL-008-004

984953

518364

5432093

transform

channel parallel to fault

81 62.5

6.5 7 Minor fizz with HCL; equigranular qtz; K-Fds; plag; granite; not magnetic; very minor limonitic weahtering in micro fractures

slight carbonates, qtz, pl, limonite

95%

88 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

crossing a fault

6/29/2011

B. Quist

D. Gritsaenko

TR-PL-11-008

TR-PL-008-005

984952

518633

5432093

fracture zone

360

152.5

7 5 Fracture zone, middle is rusty weathers. Doesn't fizz, not magnetic vugs are rusty. Equigranuler medium grained, green alteration mineral

Qtz (20), plag (20), Kspar (60)

90%

6/28/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-008

TR-PL-008-006

984951

518632

5432093

65 78 8 6 coarse grained granitoid; mostly equigranular; some garnet (brownish); qtz; hornblende; more significant fizz on north side; some K-fds; non magnetic; some reddish minerals, possibly hematitic alterations.

Gar, Qtz, Hbl, K-fds, carbonates, hem

90% similar to 077/078

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-008

TR-PL-008-007

984954

518625

5432096

18 122.5

7 7 granitic texture and mineralogy; mostly equigranular, coarse grained; qtz; K-fds; slight garnet; plag; rock peppered with dark mafic grains (hornblende); fizzes less with HCL; non magnetic; some reddish unknown minerals; hematitic alterations

Qtz, K-fds, Gar, Pl, Hbl, carbonates, Hem

90%

6/29/2011

L. Marshall

Dahsa

TR-PL-11-008

TR-PL-008-008

984955

518610

5432090

crosses a small fault 10

cm wide;

27 111

6.5 7.5

minor fizz; equigranular as before with pink K-Fds; slightly more qtz; fibrous chlorite alterations (green/grey) infracture planes, especially with dark brown limonitic weathering; grains align and give a sheen on plane surface;

K-fds, qtz, chl, lim, 90%

6/29/2011

B. Quist

D. Gritsaenko

TR-PL-11-008

TR-PL-008-009

984956

518630

5432089

Across fracturi

ng

75 78 8 7.5

Veined, lots of oxidation, slightly brecciated, at least two different types of sulphides. Occasionally a vein will fizz with acid, slightly magnetic

pyrite, purple sulphide (galena?, manganese staining?)

98%, drawing in field notes

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-008

TR-PL-008-010

984957

518632

5432039

a fracture

zone

72 103

9.5 7 medium grained granitoid; red and green alterations present (Hem/Chlorite); Qtz; K-Fds; Plag; some purpule and greenish mineralization (fluorite); slight fizz; non magnetic; some of the grains are elongated and may reflect starin or pressure directions; hydrothermal alterations and qtz veins present

Hem; Chl; Pl; Fl; carbonates;

90%

89 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-008

TR-PL-008-011

984958

518629

5432087

a fracture

zone perpendicular

to a major

fracture zone

86 115

7 6.5

no fizz; non-magnetic; equigranular, except for occasional elongated ~1cmx2mm qtz grains; grains are primarily qtz and K-Fds; minor plag.; altered to limonitic grains (brown); isolated areas have light green/dark green (chlorite?) alterations; black amphibole grains also present in isolated patches; also red mineralization occurs in even smaller patches.

Qrz, K-fds, lim, chl?, amph, red minerals.

85%

6/29/2011

B. Quist

D. Gritsaenko

TR-PL-11-008

TR-PL-008-012

984959

518632

5432087

going down

parallel to

fracture zone

340

106

7.5 7 very crumbly weak, fractured, veined, oxidized, hematite staining, lots of green alteration, pink mineral (plag?), hematite in veins, brecciated looking, manly pink and green w/ oxidized overprinting

hematite, pink mineral (plag?)

80%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-008

TR-PL-008-013

985077

518639

5432092

242

115

7.5 7 pegmatitic granite; K-fds are largest crystals visible to 1.5 cm; qtz; plag dominant; no fizz; non magnetic; some fine grained mineral aggregates sporadic throughout (unknown); possible chlorite alterations

K-fds, Qtz, chl 95%

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-008

TR-PL-008-014

984961

518631

5432086

hole is in

fracture parallel

to strike

350

73 8 7.5

dark to black aphanitic host with sporadic yellow grains and dark grained minerals following micro-fracture lines (hematite); larger limonitic alterationsin more weathered fractures; no fizz; non-magnetic;

Hem, lim, 95%

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-008

TR-PL-008-015

984962

518631

5432085

344

71 6 4.5

non mag; no fizz; only different than before in that the dark-grey "host" is now altered to dark green grey; much more yellow grains are present in areas (uraninite?); in proximity to the dark red (hematitic?) areas these grains are orange.

uraninite?, hem? 90%

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-008

TR-PL-008-016

984963

518631

5432082

340

92 9 6 back to very dark "host"; generally equigranular ~1mm; equal amounts of qtz and dark red (hematite) minerals; little to no yellow grains; very altered with limonite yellow/brown dark brown in more weathered fracture planes.

qtz, hem, lim, 90%

90 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-001

985078

5186500

5432244

305

50 8 6 vertical section on south facing wall fizzes with acid. Lots of sulphides, finely disseminated . Lsightly silicious looking. Appears to be a breccia with a slightly silicious carbonate-rich matrix. The clasts are composed of the pink-alkalic granite seen at trench 008. pyrite in the granite and in the matrix. Rock is really oxidized, weak, and crumbly, 2-3 directions of cleavage, also darker clases of a fine-grained rock present. majority of sulphides are in the matrix, not in the clasts

75%

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-002

985079

518650

5432238

horizontal

section; runs

parallel to main fracture on TR-PL-11-

009 (note; side wall

crumbled)

0 or 180

63 3 3 Brecciated rock; very crumbly; oxidized; weathered; it's loaded with pyrite; quite pink; fizzes very slightly with acid; dark magnetic minerals (magnetite?) in veins; quartz, K-Fds, lots of hydrothermal action; possibly chalcopytire.

Py, Mag?, Qtz, K-Fds, Clpy

70% 0256R; 0257T

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-003

985081

518648

5432239

100 or 280

110

6 6.5

Lots of pyrite, some finely disseminated - some coarsly disseminated; some chalcopyrite; some sulphides are concentrated in veins; fizzes slightly with acid; black mafic minerals; brecciated; pink; lots of hydrothermal action is evident; hydrothermal breccia

Py; Clpy; Sulphides; slight carbonates; mafics

80% 600R; 598T

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-004

985082

518948

5432237

230

Angular breccia with clasts of granite; K-Fds; qtz; py more concentrated in veins; clasts size vary (5mm-10cm long, possibly bigger; matrix supported; some py in the clasts; oxidized; hematite alteration

K-fds, Qtz, Py, Hem. 85% 596R; 597T

91 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-005

985083

518649

5432238

005 has a cut

across it; run

parallel to main fracture

zone

225

105

8 5 more of the breccia; clasts seem to be a bit finer grained; lots of small (3mm) white, rounded clasts; some angular pink clasts matrix; fine grained rock is rusty; hematitic staining as before; very little py visible.

Hem, Py 85% 601R; 603T

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-006

985084

518644

5432236

runs parallel

to fracture

zone

78 8 7 breccia; crosses severed dykes; lots of white clasts (round, elongated) large mafic clasts; mainly clast supported; fizzes rapidly with acid

mafics, carbonates 606R;

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-007

985085

518645

5432233

channel goes

across fracture

zone

310

127

7 6 slightly less brecciated; more consolidated; doesn’t really fizz with acid; magnetic; pink; mainly with darker blebs of mafic minerals (magnetic); py has returned mainly in small veins; parts are medium grained; crystalline; lots of K-Fds; lots of pink; py present (finely disseminated)

Mag, mafics, Py, K-Fds 604R; 605T

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-008

985086

518647

5432236

38 84 7.5 7 Granitoid; medium-fine grained; largest grains are qtz and K-fds; also plag, py, possibly garnet and fluorite present in small amounts; fizzes with acid on calcite grains; a few sulphides.

Qtz, K-fds, Pl, Py, Gar?, Fl, Cal,

90% 55H; 56R

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-009

985087

518645

5432238

45 81 9 9 Fine grained breccia; oxidized; almost clast supported; hematitic stains; very few sulphides; lots of oxidations; lots of plag

Hem; sulphides; Pl 85% 607R; 608T

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-010

985088

518647

5432234

314

75 7.5 7 Granitoid; medium to fine grained; lots of K-fds, plg, gar?, some chlorite, calcite and/or other carbonates (fizzes), some sulfides

K--fds, Pl, Gar?, Chl, Cal, Carbonates, sulfides

90% 59H; 58R

92 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-011

985089

518646

5432237

on north

side of outcrop

312

88 7.5 7.5

Similar Granitoid as before; biotite and possible hornblende grains are more conspicuous than before.

K-fds, Pl, Gar?, Chl, Cal, Carbonates, sulfides, Bt, Hbl?

85% 61R; 62H

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-012

985091

518645

5432233

parallel to fault

220

60 6.5 6 more breccia; fizzes with acid; small clasrts (~0.3mm); matrix supported; fine grained; crystalline; hematite staining oxidized; lots of hematite; many small white clasts.

carbonates; Hem; 75% 609R; 610T

6/29/2011 B. Q

uist

L. Marshall

TR-PL-11-009

TR-PL-009-013

985092

518647

5432237

channel crosses a dark mafic dyke; sharp

contacts with a

red rock

220

74 7.5 5 slightly magnetic; crystalline; fairly fresh; unknown oxidized, black dyke is very fine grained - difficult to determine minerlas.

75%

6/29/2011

B. Quist

L. Marshall

TR-PL-11-009

TR-PL-009-014

985093

518647

5432235

212 or 32

44 7.5 9 Bit of Pl; unknown red mineral; crystalline; Py; vertically cut mafic minerals; slightly magnetic; looks a bit coarser to be a granite, but still brecciated.

Pl, Py, Mag 80%

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-009

TR-PL-009-015

985094

perpendicular

to fracture

zone

151

69 7 6 polymictic paraconglomerate; clasts themselves are poly-mineralic and are rounded to sub rounded 1-5 cm across; contain other plag, qtz, K-Fds, amphibole; or K-fds, qtz; or mostly blackish amphibole + chlorite; matrix appears to be of qtz or limonitic brown; euhedral plag crystals are peppered throughout the matrix; non magnetic; both matrices react slightly to HCL.

Pl, Qtz, K-fds, amph, chl, lim

90%

93 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

6/29/2011

L. Marshall

D. Gritsaenko

TR-PL-11-009

TR-PL-009-016

985095

random orientat

ion

140

209

6 6 largely same as before; however clasts are much smaller with mm pyrite and what appears to be elongate K-fds crystals; the hole transforms into an impressive pegmatite with subhedral calcite grains ~5mm; 1x4mm K-fds; minor qtz; pegmitite clasts are about 0.75 m wide, then back to previous lithology.

Py, K-fds, Cal, 84%

6/29/2011

L. Marshall

TR-PL-11-009

TR-PL-009-017

985096

135

124

6 6 polymictic paraconglomerate; clasts themselves are poly-mineralic and are rounded to sub rounded 1-5 cm across; contain other plag, qtz, K-Fds, amphibole; or K-fds, qtz; or mostly blackish amphibole + chlorite; matrix appears to be of qtz or limonitic brown; euhedral plag crystals are peppered throughout the matrix; non magnetic; both matrices react slightly to HCL.

Py 88%

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-018

985097

518645

5432233

312

88 7.5 7 Granite with fine to medium grains; K-fds, cal (fizzes), qtz, plag, possibly fluorite (purple grains); some smaller brownish grains (garnet?); fizzes with acid; non magnetic; some amphibole present.

K-fds, Cal, Qtz, Pl, Fl?, Gar?, amph

95% 67R; 68H

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-019

985098

518646

5432230

312

83 7.5 5 Granite similar to that in previous cut K-fds, Cal, Qtz, Pl, Fl?, Gar?, amph

90% 65R; 66H

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-020

985099

518643

5432235

on south side of

outcrop

114

78 6 4.5

Pegmatitic granite with very coarse grains; K-fds, cal (fizzes), qtz, plag, possibly fluorite (purple grains); many crystals reach 1 cm in diameter; some smaller brownish grains (garnet?); fizzes with acid; non magnetic; some amphibole grains

K-fds, Cal, Qtz, Pl, Fl?, Gar?, amph

80% 63R; 64H

6/29/2011

A. Ya’acoby

D. Gritsaenko

TR-PL-11-009

TR-PL-009-021

984976

518644

5432233

312

72 6.5 6 granitoid with calcite phenocrysts; otherwise similar mineralogy and texture (granitic) as before; chlorite grain aggregations

K-fds, Cal, Qtz, Pl, Fl?, Gar?, amph, Chl

95%

94 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-001

984904

519641

5432686

across a topogra

phic high

200

57 7 8 possibly a hydrothermal breccia, clasts of pink rock (k-spar?) with a green mineral (chl-alt?), subangular, surrounded by green mineral. Crossed by white veins (possibly qtz, but it's translucent with small pink minerals in it). Unknown black mineral is also present, nothing is magnetic, nothing fizzes

80

28/07/11 S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-002

984905

519638

5432634

290

78.00

7 8 very strange rock that transitions from white-rock at the north to red-green rock at the south end. Not magnetic, doesn't fizz with acid. 1. red-green rock is medium grained with white, burgendy (hematite?), small specs of pyrite, chlorite alteration. unknown white/green mineral, slightly banded structure. 2. white rock contains massive white areas with brown swirls around it, wierd texture, not a breccia, carbonatite dyke? doesn't really fizz with acid

80% see figure in

notes

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-003

984906

519641

5432636

340

68 8 9 hydrothermal breccia? Red clasts (k-spar or hematite altered?) in a white matrix with brown specs. Some of the matrix is altered to chlorite. Clasts are 3-7 cm, subangular, matrix supported, no visible sulphides. Purple staining in areas (cerium?), also purple fluorite present

70%

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-004

984907

518639

5432635

vertical cut

309

79 6 9 texture varies quickly. This hole contains sections that are porphyritic, sections that are equigranular and sections that are completely messed up. 1. equigranular rock that contains green mineral (chl?) and red mineral (ferric k-spar?), and qtz. 2. Breccia -> pink (ferric-kspar) clasts surrounded by green, oxidized on surface (green minerals are slightly magnetic). Cerium staining is present elsewhere in the rock 4. very top of the cut is white, fizzes with acid and contains small amounts of an unknown brown mineral (carbonatite dyke?).

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-005

984908

519635

5432628

horizontal cut

0 61 10 9 hydrothermal breccia (?), lots of pink, red, purple, green, white mineralization (see sketch in notes), cerium staining, possible hematite staining, green mineral (chl?), lots of surface oxidation, crumbly, breakable rock, some of the white veins fizz, extremely hard to name

95% recov

95 11BPhysical Work


Date

Nam

e

Nam

e 2

Trench ID

Sample ID

Act Labs ID

Easting

Northing

Location on Trench

Azimuth

Length

Width

Depth


ents

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-006

984909

519637

5432633

32 53 9 9 Same red/green rock as before (TR-PL-010-004). Slightly more qtz, crossed by white veins, green alt mineral in matrix and in veins. Certain sections look almost banded, strange white/blue mineral present, not fizzing, not magnetic, no sulphides present

80%

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-007

984911

519635

5432633

sub horizontal cut

on a 45 degree angle

32 75 6 7 lots of crazy veining (see sketch in notes), Christmas rock again, but it's brecciated. Green mineral is slightly magnetic. Nothing is fizzing, christmas rock is medium grained, clasts are subangular, matrix supported

75%

28/07/11

S. Todd

B. Quist

TR-PL-11-010

TR-PL-010-008

984912

519634

5432630

32 107

8 8 Brecciated Christmas rock, possibly contains riebeckite when broken on edge, also contains a lime-green mineral (unknown) and possibly fluorite, contains finely disseminated pyrite. Christmas rock is surrounded by green mineral (magnetic). Hematite staining in some areas, oxidized on the surface. Doesn't fizz with acid

80%

28/07/11

S. Todd

B. Quist

TR-PL-11-011

TR-PL-011-001

984913

519635

5432658

west of fault

running through trench

54 72 10 11

brecciated k-spar/christmas rock. Contains qtz/carb veins, pyrite,

75% see sketch in

notes

28/07/11 S. Todd

B. Quist

TR-PL-11-011

TR-PL-011-002

984914

519634

5432658

east of fault


56 60 8 11

rock is brecciated, main host is pink with massive k-spar, and yellow/orange blotches between clasts, lots of oxidation, blue/green mineral (riebeckite?), patches of creamy coloured rock, purple fluorite and different mineral that is also purple. fluorite occurs in the creamy coloured areas that fizz. unusual texture. bottom of channel contains a chlorite altered area (due to veining or fault?). also contains green/pukey coloured mineral

80%

28/07/11

S. Todd

B. Quist

TR-PL-11-011

TR-PL-011-003

984915

519635

5432653

west of fault


56 86 8 9 Christmas rock (ferric k-spar? & chl? & riebeckite?) which is crossed by veins (mostly blue/green). Also contains an area that is creamy/white with red mineralization in it (REE?). Fizzes with acid (carbonatite?), some of the veins are offset, not magnetic, wierd purple mineral in some of the creamy veins

80%, see sketch in

note

96 12BGeophysics


13 Geophysics

13.1 Radiometric work

Private regional airborne geophysical radiometric maps were available for the Deadhorse Creek Property and were used to delineate targets in conjunction with hand-held, GPS-paired RS-125 Gamma Ray spectrometers capable of discriminating K, U and Th from total counts per second. The spectrometers were used primarily on regional grids (see Figure 19) but they were also used on reconnaissance traverses and on the trenches. Background counts per second (cps) ranged between 200 - 300. The spectrometer was very useful for guiding general exploration work; it provides a first pass approximation of Th-U-K geochemistry for any sample type and can be carried by non-specialist labourers for automated and georeferenced data collection during other tasks (such as soil sampling).

Measurements taken with the RS-125 spectrometer were all processed in the same way. The device was setup to take a measurement of the average background radiation every second, and to group those samples into 30 second blocks. After measurement, data was recovered from the device and opened in Microsoft Excel 2010©. Any data containing missing coordinates, obvious incorrect coordinates, data blocks with less than a full 30 units or impossible altitudes were removed from the data set as erroneous data. Each 30 second block was then averaged to create one data point. No data was removed based background radiation levels, ie extreme highs or lows. The averaged points were then imported into Surfer 10© in order to contour them. Surfer requires that imported data be gridded. All data sets were too large to grid all the data, so a search function had to be used in order to average points around each node. The search function was set to use a circle divided into 4 quadrants to scan a grid having a resolution off 300x300 points. Each search node was set to use a radius of 0.001 units, use a maximum of 64 data points, a maximum of 16 data points in each quadrant and was set to blank the node if there was less than 4 data points in all quadrants or if 3 or more quadrants contained no data. Once these parameters were set, the Kriging method was used to actually create the grid. This grid was then filtered using a low-pass Gaussian 3x3, then spline smoothed, both using Surfer. The created grid was then used to create a shaded relief map. Custom color scales were used for each map in order to best display data. It was common to find that the vast majority of data existed in the bottom fifth (or less) of the total scale, so most color scales used are exponential in form in order to show the general shape of the contour, while still including the peak values.

Also used on the property was the Polimaster (PM10703M), a personal gamma ray radiation detector. The Polimaster was only used for on outcrops and was not used for prospecting, as it was not outfitted with a GPS unit.

Radiometric maps (1:5000 scale) of counts per second as well as K, Th, and U levels on the Deadhorse Creek Property can be found in Appendix 3. Table 7 summarizes radiometric assays taken using the spectrometer; it also provides locations and descriptions of the rocks assayed.

97 12BGeophysics


Figure 19. Index map of spectrometer grids on the Prairie Lake Property

98 12BGeophysics


13.2 Magnetic data

Although there was no new magnetic geophysical data collected for the property, there was low resolution magnetic coverage of the area, as provided by the Ontario Geological Survey. This data is presented in Figure 20.

99 12BGeophysics


Figure 20. Regional magnetics map of the Prairie Lake Property. Magnetic data was provided by the Ontario Geological Survey.

100 12BGeophysics


13.3 Conclusions/Recommendations based on Radiometric work

Rare earth elements (REE) can be associated with areas of anomalous radioactivity; both high and low radiometric anomalies can be indicative of REE enrichment and Th in particular is known to be a useful vector to determine areas that may be anomalous in REE. The handheld spectrometers are an excellent prospecting tool and can be operated by people with limited experience and geological knowledge.

It is recommended that a fixed wing airborne radiometric and magnetic survey of the property be flown. This survey will provide a more complete picture of the property as a whole as well as good data coverage for parts of the property that are difficult to access. An airborne survey will allow for more detailed prospecting and target generation for future field seasons. After an airborne survey has been flown, the radiometric lows should be heavily sampled and drilled to test for REE potential.

101 12BGeophysics


Table 8. Summary table of radiometric data collected using handheld spectrometers and the polymaster.

Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing

Location Description Rock Description

Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

19-May-11

L. Marshall

S. Vachon

2424-A46501

101

318

518736

5431808

Moss covered outcrop grey/red/brown, med-fine grained arenite 48.8 3.

8 12.8 114.9 Picture #4

19-May-11

L. Marshall

S. Vachon

2424-A46555

101

318

518666

5431824

fine grained alkalic

granite w/ qtz,/dark fig vein (highest reading)

47.1 3.5 5 126.

6 Picture #s 1,2,3

19-May-11

Wes

G. Quist

2483-A7648

101

319

518756

5431901

Willow clearing, on incline. 1.

8 1.4 78.3 Significant Overburden.

19-May-11

Wes

G. Quist

2483-A7903

101

321

518374

5432106

Up ridge, next to road, opposite swamp 0.

9 18.3 125.8

19-May-11

G. Quist

Wes

2483-A7923

101

321

518556

5432092

Taken at side of ridge 5.4 8.4 79.7

20-May-11

G. Quist

Wes

2424-A46662

101

319

518750

5431921

side of hill, close to summit

exposed pink rock, no lustre 3.

6 6.5 59.8

102 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

20-May-11

G. Quist

Wes

2424-A47044

101

321

518837

5432108

side of hill, close to summit overburden 3.

6 6.5 59.8

20-May-11

L. Marshall

S. Vachon

2483-A7978

101

318

518766

5431820

leaves/moss/overburden 124.1 2.

2 0 35.2

20-May-11

L. Marshall

S. Vachon

2483-A7983

101

318

518735

5431817

leaves/moss/overburden 242.3 2 9.5 60.9

20-May-11

L. Marshall

S. Vachon

2483-A7988

101

318

518719

5431823

dark quartzite 439.8 2.6 18.9 112.

6

20-May-11

L. Marshall

S. Vachon

2483-A7995

101

318

518665

5431830

Moss covered outcrop Alkalic intrusive starts 333.9 3.4 7.8 91.5

20-May-11

L. Marshall

S. Vachon

2483-A8011

101

318

518534

5431822

top of small outcrop, moss covered

outcrop is pink/white alkalic intrusive but does

not five high scint reading ilke covered top, outcrop aprox 3m high.

226.4 1.6 4.3 67.5 Picture #6

(1885)

20-May-11

L. Marshall

S. Vachon

2483-A8189

101

318

517593

5431809

outcrop, grey/red

qztite(?) with alkalic intrusive veins

319.3 1.6 32 46.4

103 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

20-May-11

L. Marshall

S. Vachon

2483-A8293

101

320

518710

5431998

orange alkalic intrusive with emerald green

inclusions or oxidation patches

103.3 1.8 0.8 28.2 Pic #8 (1884)

20-May-11

L. Marshall

S. Vachon

2483-A8298

101

320

518736

5431994

Float – red/grey

sedimentary rock with unknowns

515.8 1.3 1 183.

1

could be float but

associated with small mound of (broken

bedrock?)

21-May-11

D. Gritsaenko

Wes

2424-A47156

101

322

518540

5432197

large patch of short (~2m tall) poplar(?) trees, small outcrop

visible, low overburden, end of first major uphill

3.9 1.5 37.6

aprox 25m East of the assay is a

small clearing with

a great view!

21-May-11

M. Dalsin

S. Vachon

2483-A8329

101

323

518757

5432290

Possible Outcrop moss covered rock, pink (kfspr) with white 210 65.8 2.

4 2.1 8.7

21-May-11

M. Dalsin

S. Vachon

2483-A8389

101

323

518757

5432290

walked past several boulders, in clearing

with small trees

granite type rock, kfspr, white mineral, biotite ///

white-pink weathered surface, some

pronounced veins

209 79.6 2.1 0.5 18.3

21-May-11

M. Dalsin

S. Vachon

2483-A8507

101

325

518472

5432492

just through dense small tree area

pink granite outcrop (pink on weathered

surface -> Kspr) 192.7 3.

1 2.8 13.6 after lunch

104 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

23-May-11

Wes

S. Vachon

2424-A47407

101

317

518426

5431688

uphill out of swamp Dark brown soil 475 1.8 6.2 88.8

outcrop beside soil

had low counts, dark soil had high

counts

23-May-11

Wes

S. Vachon

2424-A47617

101

317

518842

5431715

side of hill near top red brown soil with rock chunks 1100 3.

6 17.4 197.9

23-May-11

Wes

S. Vachon

2424-A47648

101

317

518742

5431758

middle of hillside red rock showing through ground 600 1.

5 9.2 42.5

24-May-11

Wes

S. Vachon

2483-A8463

101

317

518843

5431718

side of hill under dead tree orange clay soil 760 616.5 2.

7 15.8 184.1

24-May-11

Wes

S. Vachon

2483-A8537

101

317

518431

5431688

pulled up tree lying across ridge orange and pink rock 353 442.3 1 4.1 76.6

24-May-11

M. Dalsin

G. Quist

2483-A8743

101

313

517844

5431306

forested area, marshy soil 880 367.7 0.6 13.3 106.

6 some rubble

but no outcrop

105 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

24-May-11

Wes

S. Vachon

2483-A8820

101

315

518682

5431528

forested area at bottom of hill pink red rock 488 265.7 3.

3 0.3 82.2

25-May-11

D. Gritsaenko

G. Quist

2483-A8462

101

326

517926

5432600

187 4.3 6.1 36.4

25-May-11

M. Dalsin

G. Quist

2483-A8780

101

313

518259

5431290

deadfall area and close to cliffs, walking in burn

out soil next to granite 775 352.1 2.

1 8.6 103 OC-11-MLD-022

outcrop is cgr pink

granite cliffs

25-May-11

M. Dalsin

G. Quist

2483-A8809

101

313

518492

5431293

assay over soil 925 386 1.1 0.4 137

25-May-11

M. Dalsin

G. Quist

2483-A8961

101

317

518844

5431712

uphill w/ lots of deadfall soil 850 357.2 1.

7 7.1 110.1

26-May-11

D. Gritsaenko

G. Quist

2483-A8634

101

327

518268

5432701

500 215 2.4 2.9 62.1 OC-11-

DG-028

27-May-11

G. Quist

Wes

2483-A8561

101

330

518342

5432986

Halfway up side of cliff Too weathered to tell 700 341.6 n 1.6 5.4 108

106 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

27-May-11

Wes

G. Quist

2483-A8730

101

330

519034

5433014

middle of the quad path Red soil 1200 584.7 Ngyh-

1 2.2 8.1 189.

9 N/A

27-May-11

Wes

G. Quist

2483-A8766

101

332

518802

5433246

Small birch trees dirt and moss overburden 800 301.9 Ngyh-

1 1.9 7.8 87.8 N/A

27-May-11

Wes

G. Quist

2483-A8812

101

317/318

518838

5431760

Rudys cut block lower outcrop

reddish orange weathering 1100 519.7 Ngyh-

1 7.4 8.2 140.

5 N/A

27-May-11

Wes

G. Quist

2483-A8815

101

317/318

518814

5431754

Top of Rudys cut block between two upturned

trees

some pink crystalization with red/orange

weathering 4800 2.4 Mgyh-

1 0 34.6 816.1 N/A

27-May-11

D. Gritsaenko

G. Quist

2483-A8925

101

329

518397

5432897

700 285.5 7 5.7 60.4 OC-11-DG-029

27-May-11

D. Gritsaenko

G. Quist

2483-A8952

101

329

518171

5432896

550 215.7 1.6 6.2 59.7

29-May-11

Wes

G. Quist

2483-A8614

101

335

517810

5433064

On incline sparse trees, mossy overburden Taken on Reddish Soil 900 422.8 Ngyh-

1 2.9 0 142.

8 N/A

107 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

29-May-11

L. Marshall

G. Quist

2483-A8896

101

332

518616

5433218

clearing next to conspicuous float pile soil 550 215.6 nano 3.

1 6 52.9 soil/none

29-May-11

L. Marshall

G. Quist

2483-A8947

101

333

518503

5433308

birch sapling stand soil 525 218.3 nano 1.6 9.2 54.8 soil/none

29-May-11

L. Marshall

G. Quist

2483-A9100

101

334

518604

5433396

birch/beech sapling stand soil 550 234.1 nano 2.

3 2.9 70.1 soil/none

29-May-11

Wes

D. Gritsaenko

2483-A9535

101

327

517597

5432734

denser, pine trees 1600 851 nGy 1.7 15 277.

5 assay over

soil black soil

29-May-11

Wes

D. Gritsaenko

2483-A9571

101

330

517695

5432976

open area pink granite 550-590 224.5 nGy 3.

2 4.8 58.2

29-May-11

Wes

D. Gritsaenko

2483-A9590

101

332

517703

5433191

by mossy pink granite area 700 324.1 nGy 1.

7 5.1 101.6

assay over soil

30-May-11

Wes

D. Gritsaenko

2483-A9714

101

340

517647

5433993

kind of opening orange weathered surface 600 242.2 nGy 2 8.2 63.8

108 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

30-May-11

Wes

D. Gritsaenko

2483-A9761

101

335

517608

5433509

some clearing with stumpy dead fall same pink granite 650 345.8 nGy 3.

4 6.6 98.8

30-May-11

Wes

D. Gritsaenko

2483-A9807

101

333

517613

5433281

west side of swamp pink, red and brown weathered surface 1000 594.4 nGy 3.

2 26.5 151.8

OC-11-DG-040

31-May-11

D. Gritsaenko

Wes

2483-A10039

101

14

517298

5433070

10-20m north of road 1m across pink granite, covered by moss 800 330.1 nGy 5.

9 13.1 67.5

31-May-11

D. Gritsaenko

Wes

2483-A10052

101

14

517309

5433095

small clearing with lots of dead leaves and

dead fall

pink coarse grained rock near by

1200-1300 598.3 nGy 4.

1 7.9 186.4

assay over soil

31-May-11

D. Gritsaenko

Wes

2483-A10069

101

14

517304

5433196

medium sized area with lots of dead leaves and

deadfall 1500 672.3 nGy 4.

4 20.1 187.7

assay over soil

brown soil, orangeish

tinge, intermixed

with various sizes of coarse

grained pink float

31-May-11

D. Gritsaenko

Wes

2483-A10146

101

16

517486

5433379

swampy area with large mossy mound in between poplars

650-700 297.8 nGy 6.

8 13.6 50 assay over soil

109 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

31-May-11

D. Gritsaenko

Wes

2483-A10147

101

16

517494

5433491

clearing 10m away from small pond, filled with

dead leaves and thorny bush

2x2 exposed, very weathered pink surface

with white area 2000 889 nGy 4.

1 54.7 199.9

OC-11-DG-041

Sample + Photo taken

31-May-11

D. Gritsaenko

Wes

2483-A10221

101

16

517493

5433628

lots of large deadfall near creek 1200 453.7 nGy 1.

7 38 83.8 assay over soil

possibly float

31-May-11

Wes

D. Gritsaenko

2483-A9908

101

333

517612

5433278

near small broken up rock pile (float) 600 289.4 nGy 4 5.2 77.7

31-May-11

Wes

D. Gritsaenko

2483-A9954

101

328

517500

5432803

up small hill, open area with scattered pine trees, float near it

fine grained pink granite 192.2 nGy 2.6 2.2 54.3

31-May-11

Wes

D. Gritsaenko

2483-A9991

101

328

517375

5432840

north side of road, across swampy lake 470-

500 180.4 nGy 4.9 2.8 37.4 assay over

soil

1-Jun-11

D. Gritsaenko

Wes

2483-A10412

101

15

517376

5433356

up little hill beside 2 huge toppled birches 1600 750.3 nGy 4.

5 9.4 237.9

assay over soil

1-Jun-11

Wes

G. Quist

2483-A10459

101

332

517119

5433208

Near toppled tree Over soil 700 244.5 nGy 2.9 9.6 57.6 N/A

110 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

1-Jun-11

Wes

G. Quist

2483-A10467

101

332

517121

5433228

20m from last assay, 2 criss crossed trees Over soil 1500 612.5 nGy 2 16.2 185 N/A

1-Jun-11

D. Gritsaenko

Wes

2483-A10498

101

14

517310

5433771

past pine trees, in area with deadfall in

between 2 birch trees

pink, coarse grained, possibly super fine grained qtz, mafics

(intermixed with soi)

2500-2700 1.1 mGy 4.

5 67.4 252.9

assay over soil

Sample + Photo taken // 1 ft of soil removed to

reveal pieces of

broken rock

1-Jun-11

D. Gritsaenko

Wes

2483-A10594

101

13

517183

5433705

along side of cliff, thick mossy area 600-

650 240.5 nGy 2.2 8 62.1 assay over

soil

1-Jun-11

D. Gritsaenko

Wes

2483-A10653

101

13

517201

5433339

ridiculous uphill deadfall 1200 518 nGy 3.

2 15.6 145.5

assay over soil

1-Jun-11

Wes

G. Quist

2483-A10661

101

336

518804

5433622

side of incline bedrock near by 825 339.6 nGy 2 3.5 109 Assay

over soil

pinkish white

bedrock near by

1-Jun-11

D. Gritsaenko

Wes

2483-A10671

101

13

517163

5433231

uphill, lots of dead fall, beside cliff

small cliff, dark grey, fine grained 1200 522.7 nGy 3.

8 15.2 144.8

OC-11-DG-042

Sample + Photo taken

111 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

1-Jun-11

Wes

G. Quist

2483-A10880

101

337

516597

5433699

side of incline, slight outcrop

Slightly red pink weathered rock 900 383.2 nGy 5.

2 1.7 113.7 N/A

1-Jun-11

Wes

G. Quist

2483-A10888

101

339

519211

5433905

slight mound bottom of incline birch trees 1200 530.9 nGy 2.

3 13 159.6

Assay over soil

1-Jun-11

Wes

G. Quist

2483-A10957

101

336

517001

5433633

foot of incline, dense brush Over soil 800 333 nGy 1.

6 16.7 82.3 N/A

2-Jun-11

Wes

G. Quist

2483-A10987

101

335

516800

5433489

incline near the top of ridge Over soil 725 262.5 nGy 2 12 63.4 N/A

3-Jun-11

L. Marshall

M. Dalsin&

D. Gritsaenko

1320-A1110

N/A

N/A

517477

5433517

outcrop exposed by fallen tree

this rock literally looks like bacon. The "meaty" part is red fg-mg quartzo

feldspathic and the "fatty" part is a light gray quartz-rich meta sed. The bacon "waves can be up

to 5 cm across the thickest part and then tapers off and pinches

out.

~800 cps 438.2 n 3.

7 21.9 72.3 oc-11-MLD-039

Dubbed the bacon zone, prospecting

episode

112 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

3-Jun-11

L. Marshall

M. Dalsin&

D. Gritsaenko

1320-A1111

N/A

N/A

517374

5433577

clearing next to alkalic intrusive

Gossan/soil sample with red patched similar to above "meaty bacon"

part, gossan is primarily weatherd orange/brown

with associated orange/red soil. Also has

blackish mineralization/weatherin

g appearing almost as superficial staining (perhaps mafic?)

~800 cps 810.5 n 3 48.4 136.

3 soil

3-Jun-11

L. Marshall

M.

Dalsin&D.

Gritsaenko

1320-A1112

N/A

N/A

517437

5433393

soil exposed by fallen poplar tree soil/ with gossan ~700

cps 349.4 n 6.4 3.5 69.2 soil

3-Jun-11

Wes

G. Quist

2483-A10569

516534

5433603

Swampy Area with small alders Over Soil 800 318.6 nGy 0.

7 14.2 86.3 N/A

3-Jun-11

Wes

G. Quist

2483-A10640

516133

5433494

near top of incline Over Soil 700 285.7 nGy 7.2 7.9 55.1 N/A

3-Jun-11

Wes

G. Quist

2483-A10657

516250

5433394

Flatter area with sparse tree cover Over Soil 850-

900 394.4 nGy 1.7 5.4 127.

2 N/A

113 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

4-Jun-11

Wes

M. Dalsin

2483-A10800

101

333

516811

5432999

near clearing with deadfall over soil 1200 615.2 nGy 1.

7 33.1 153 over soil

4-Jun-11

Wes

M. Dalsin

2483-A10810

101

330

516859

5433001

under big rock on fault Red/pink rock area 1100 564.7 nGy 5.5 33.5 115.

3 OC-11-

MLD-040

4-Jun-11

Wes

M. Dalsin

2483-A10856

101

517200

5432755

Side of incline near top over soil 1100 421.5 nGy 5.6 24 80.7 over soil

4-Jun-11

Wes

M. Dalsin

2483-A10867

101

517203

5432647

Near big dead tree over soil 750-800 301.5 nGy 2 7.1 83.9 over soil

114 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

4-Jun-11

Wes

M. Dalsin

2483-A10872

101

517201

5432647

beside lake river area over orange brown soil 1400 741.1 nGy 2.2 11.8 240.

6 over soil

4-Jun-11

Wes

M. Dalsin

2483-A10948

101

319

517115

5431912

closish to lake, alot of deadfall over soil 2800 1.3 uGy 1.

1 52.1 360 over soil

4-Jun-11

Wes

M. Dalsin

2483-A11171

101

330

517145

5432994

start of incline over soil 950 433.8 nGy 5.7 17.1 98.9 over soil

5-Jun-11

G. Quist

L. Marshall

2483-A11196

101

334

515992

5433384

Side of inline, sparse trees, close to road Overburden 600 243.8 n 1.

8 6.4 68.6

5-Jun-11

L. Marshall

G. Quist

2483-A11463

101

329

516418

5432888

soil sample on logging cut block soil sample 1000 391.1 n 3.

3 15.2 98.6 may be

"bacon rock" underneath?

115 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

5-Jun-11

G. Quist

L. Marshall

2483-A11466

101

328

516426

5432843

Middle of cutblock "Baconite" 3500 1600 n 3.2

132.1

322.9

5-Jun-11

G. Quist

L. Marshall

2483-A11544

101

328

516832

5432815

Side of tall cliff "Baconite" 2500 1300 n 1.4 72.1 325.

7

5-Jun-11

M. Dalsin

G. Quist

2483-A12452

101

323

516987

5432268

in clearing over old logging road. First scint

over soil soil

1000 -

1100 cps

530.7 nGy 5.2 24 123.

4 N/A

5-Jun-11

M. Dalsin

G. Quist

2483-A12453

101

323

516987

5432268

This scint over hole dug in the ground

possible REE mineralized rock below gneiss

2200 cps 923.8 nGy 9 31.9 234.

8 N/A

6-Jun-11

M. Dalsin

G. Quist

2483-A12637

101

516885

5432527

Over old logging road on gneiss

gneiss... Possibly something below? 900 418 nGy 3.

2 16.4 106.4 N/A

6-Jun-11

L. Marshall

Wes

2483-A12707

101

C

516587

5432921

clearing in cut block, orange/brown soil soil/leaves/moss ~100

0 491.3 n 4.1 24.9 112.

1 Last of grid 101

6-Jun-11

L. Marshall

Wes

2483-A12881

108

B

518347

5431732

clearing in cut block horizontal outcrop, fg intrusive pink/cream

colored ~600 275.2 n 2.

6 6.2 77.3

116 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

6-Jun-11

L. Marshall

Wes

2483-A12977

108

D

518547

5431545

low bush clearing soil/leaves/moss ~500 253.3 n 2.2 9.4 64.5

9-Jun-11

L. Marshall

Wes

2483-A12988

108

D

518538

5431655

dense woods soil SEE COMMENTS ~1100 468.6 n 2 4.7 155

soil was uncovered afterwards to reveal a float stone looking like the famous

"bacon rock". No other high readings

were found in the

immediate area.

9-Jun-11

L. Marshall

Wes

2483-A12996

108

D

518548

5431776

maple sapling stand soil orangish, appeared to contain weathered

"bacon rock" bits

~1150 553.1 n 3.

3 11 167

9-Jun-11

L. Marshall

Wes

2483-A13018

108

E

518649

5431841

slight clearing on hillside dark soil leaves/moss ~630 288.6 n 2.

3 6.6 82.7

generally traverse

area around this location

has relatively high cps

117 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

10-Jun-11

D. Gritsaenko

L. Marshall

2424-A203

109

C

518851

5432765

taken near top of OC same as OC-11-DG-088 750 316.2 nGy 2.9 27.2 48.6

GPS did not show Assay

Name, labeled in D. Gritsaenko's GPS as 2424-

A002?

10-Jun-11

L. Marshall

D. Gritsaenko

2424-A293

109

A

518709

5432731

Approx E-W trending outcrop, ~20m long

~3m high. Fairly dense foliage

Quite an interesting rock consisting of a mg meta-

volcanic light grey intrusion with Qtz, k-spar and plag. This is intruding a fg to vfg aphanitic dark grey meta-sed that also

appear as > 1m xenoliths. The highest scinting area

appeared to be a vein and/or fauly

~1200 572.7 n 1.

7 30.8 142.6

OC-11-DG-088

10-Jun-11

A. Ya’acoby

G. Quist

2424-A33

109

A

518503

5432286

side of incline, dense decidous trees (maple) Overburden 700 342.9 nGyh-

1 2.3 9.8 96.2

10-Jun-11

D. Gritsaenko

L. Marshall

2424-A565

109

C

518893

5433350

mossy open area, some rock surface visible Assay over Soil 1000 478.2 nGy 2.

9 19.9 123.3

Assay Over Soil

10-Jun-11

L. Marshall

Wes

2483-A13090

108

F

518761

5431778

hillside with dense cover

outcrop was cg red/orange felsic

intrusive

~1000 457 n 3.

1 16.8 120.7

118 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

10-Jun-11

L. Marshall

Wes

2483-A13093

108

F

518745

5431799

small inclined valley close to main road, bit

of a clearing dark soil/leaves ~800 353 n 2 10.2 100.

7

10-Jun-11

D. Gritsaenko

G. Quist

2483-A13232

108

G

518853

5432405

plateau, sparse deciduous trees assay over soil 1000 494.1 nGy 1.

8 3.3 168.1

assay over soil

10-Jun-11

G. Quist

D. Gritsaenko

2483-A13321

518752

5431984

Relatively flat, short, sparse deciduous trees Overburden 875 394.3 n 0.

8 10.7 120.7

11-Jun-11

L. Marshall

D. Gritsaenko

2424-A615

109

D

518945

5433133

Soil assay near boitite, k-spar rich ground-level

intrusive reddish/rusty soil ~750 758.4 n 1.

4 20.2 233.9 N/A

11-Jun-11

A. Ya’acoby

Wes

2483-A15471

113

518810

5432286

slight incline; spruce trees orange/red soils (podzol) 1500 845 nGyh-

1 5.4 0 287.

9

16-Jun-11

A. Ya’acoby

Wes

2483-A15486

113

518804

5432080

upturn with a flat alder tree area granitic rocks 2000 1043 nGyh-

1 3.3 15.5 339

17-Jun-11

G. Quist

Wes

2483-A15900

113

G

518805

5431628

Base of incline, deciduous to

carniferous transition Overburden 1300 572.2 n 1.

6 21.5 161.4

119 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

17-Jun-11

Wes

G. Quist

2483-A16027

113

E

518615

5431813

Generally flat area with some large trees Over soil 1400 591.2 nGy/h 3.

1 20.9 162.2 N/A

18-Jun-11

A. Ya’acoby

D. Gritsaenko

2424-A832

109

D

518958

5432942

slight incline; tall birch trees; thick vegetation. Assay on soil 970 536.1 nGyh-

1 2.6 24.2 137.

8

18-Jun-11

A. Ya’acoby

D. Gritsaenko

2424-A951

109

E

519047

5433019

forest clearing/old logging road; wood chip

piles Assay on soil 1300 815.9 nGyh-

1 3.3 0.5 175.

2

18-Jun-11

Wes

G. Quist

2483-A16133

113

B

518293

5432158

Near side of road with coniferous trees. Over soil 2700 1.3 mGy/

h 5.1 37.3 370.

5 N/A

7-Jul-11

D. Cameron

G. Quist

2424-A4131

121

C

519605

5432426

At the bottom of a light ridge, sparsly forested.

Lots of marshland

Pink to purple fine grained rock. Effervesent fizzing with hcl (possibly

carbonite). Flourite present and some red to red pink minerals. Pod of

course grained black minerals that scint the

highest, possibly an amplibole of some kind.

Pyrite and possible pyrochlore present.

11700 7.20 Micro 0 131.

8 2398

Dug through 2ft of

overburden, associatesm

d with sample 11-

dtc-004

120 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

7-Jul-11

D. Cameron

G. Quist

2424-A4147

121

C

519601

5432.653

Top of a ridge that has swamp to the west,

forested. Dug through about 2ft of over

burden

Red and white bretcha surounded by grey host

material. Bretcha is matrix supported.

Bretcha looks similar to k-feltsbar but more vivid

red.

1500 666.70 n 3.

9 74.6 78.3

Sample 11-dtc-005 was taken from

location

1-Aug-11

G. Quist

D. Cam

eron

2424-A4320

122

A

521197

5426488

middle of significant incline over gravel, dug

a hole. Assay on gravel 3400 1.7 micro 0 221.

6 168 11-GMQ-012

John Tecnowsky

1-Aug-11

G. Quist

D. Cam

eron

2424-A4481

122

B

521352

5425461

top of ridge, over soil assay on soil 450 205.6 n 1.9 12.2 42.5 John

Tecnowsky

1-Aug-11

G. Quist

D. Cam

eron

2424-A4526

122

B

521352

5425461

flat region over soil 550 287.4 n 1 15.1 71.5 John Tecnowsky

1-Aug-11

G. Quist

D. Cam

eron

2424-A4543

122

B

521358

5425993

flat, over soil over soil 720 327.4 n 1.5 14.5 84.8 John

Tecnowsky

1-Aug-11

G. Quist

D. Cam

eron

2424-A4554

122

B

521354

5426149

flat, over soil, dug a hole over soil 2000 919 n 0.

9 52.7 230.4 John

Tecnowsky

121 12BGeophysics


Date

Nam

e

Nam

e 2

Assay #

Grid #

Line #

Easting

Northing


Counts (cps)

DR

DR units

K (%)

U (ppm

)

Th (ppm)

Associated Outcrop

Name Comments

1-Aug-11

G. Quist

D. Cam

eron

2424-A4661

122

C

521502

5426076

top of topo over soil 520 223.3 n 0.4 10 60.5 John

Tecnowsky

122 13BAssay Results


14 Assay Results

Assay results can be found Appendix 17.1. Samples were sent to Activation Laboratories, located in Thunder Bay, Ontario. A total of 17 sample shipments containing 310 samples were processed. A blank (white marble sourced from?) was included for every 10 samples that were processed. Samples were processed using code 1A1 fire assay for Au (?) and Code 8 REE assay packages. The REE assay package requires a lithium metaborate/tetraborate fusion with subsequent analysis by ICP and ICP/MS. Mass balance was used as an additional quality control.

Figure 21 shows Total Rare Earth Oxide (TREO) values for rock samples collected on the propery. Table 8 gives selected assay results for trench samples that contain (TREO) values that are equal to or exceed 0.5%. Complete results can be found in Appendix 17.1 Table 9 gives selected results from the assays for soil samples collected on the property, complete results can be found in Appendix 17.1. Selected results from rock samples located on the property can be located in Table 10, complete results can be found in Appendix 17.1.



Figure 21. TREO values from rock samples collected on the Prairie Lake property



Table 9. Summary table of assay values from trench channel samples containing >0.5% TREO (n = ?#?).

Sample Name Easting Northing TREO ActLab Number Y La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Hf Th U

TR-PL-007-047 518749 5431989 2.49 984517 114 6310 10000 946 3050 363 97.4 260 24.9 61 5.5 6.9 0.58 3.2 0.45 1.3 360 2.2

TR-PL-007-032 518745 5431988 2.44 984501 191 5910 9860 957 3090 342 86.8 236 23.9 70 8.1 12.9 1.18 5.9 0.77 1.5 367 2.9

Tr-PL-007-072 518760 5431991 2.23 984545 208 5530 9090 873 2750 266 58.7 162 18.4 64.1 7.7 13.8 1.24 6 0.79 1.7 202 4

TR-PL-001-013 518830 5431753 2.21 984569 65 6230 9130 779 2270 209 47.8 94.9 7.5 23.6 3.2 6.9 0.76 4.2 0.63 1.9 164 15.1

TR-PL-001-022 518822 5431757 2.05 984582 68 6030 8280 707 2010 174 38.5 109 8.2 28.7 3.3 7.1 0.72 4.1 0.62 2.6 114 20

TR-PL-007-060 518755 5431993 1.93 984532 155 4610 7880 770 2480 252 60.5 163 17.5 55.7 6.6 10.1 0.91 4.5 0.6 2.2 221 4.6

TR-PL-007-004 518739 5431994 1.86 985054 134 4270 7390 772 2630 321 81 164 17 62.6 6.3 11.6 1.16 5.9 0.84 1.1 365 4

TR-PL-007-020 518741 5431988 1.85 985075 108 4370 7440 758 2540 276 65.7 155 13.6 44.5 5 8.3 0.75 4.1 0.56 2.3 298 3.6

TR-PL-007-002 518748 5431990 1.84 985052 83 4370 7300 747 2570 305 82.2 206 17.4 45.9 4.1 6.3 0.5 3.5 0.53 1.8 343 3.6

TR-PL-008-011 518629 5432087 1.80 984958 105 3790 7220 751 2700 374 91.8 241 20.4 61.5 5.7 7.2 0.6 3.4 0.53 3.8 447 19.5

TR-PL-007-073 518762 5431994 1.75 984546 150 4380 7150 676 2140 209 46.7 120 14 49.5 6.5 10.5 0.92 4.3 0.56 2.2 163 3.3

TR-PL-007-023 518743 5431991 1.71 984966 136 4130 6900 657 2180 263 69.2 202 16.9 51.9 5.9 12.2 1.26 7.2 1.08 2.4 308 3

TR-PL-007-038 518746 5431995 1.63 984507 207 3990 6380 629 2020 256 76 219 25 81.7 9.5 14.3 1.31 7.6 1.04 1.4 304 6

TR-PL-008-016 518631 5432082 1.56 984963 126 3290 6190 648 2340 328 81.4 216 19.4 63.7 6.2 9.3 0.72 3.5 0.46 2.6 292 11.8

TR-PL-007-027 518740 5431997 1.55 984971 115 3690 6280 601 1990 227 59.5 180 16.3 52.9 5.6 9.9 0.95 5.2 0.77 2.2 246 4.6

TR-PL-001-025 518820 5431752 1.51 984585 79 3480 6060 630 2150 260 56.7 129 10 31.8 3.4 6.3 0.6 3.2 0.45 1.3 183 20

TR-PL-008-002 518619 5432084 1.46 985072 184 2430 5210 674 2890 560 140 295 25.2 78.8 8.3 11.5 0.89 4.1 0.5 2.5 502 11.4

TR-PL-007-059 518754 5431989 1.44 984531 105 3560 5770 571 1860 196 47.3 99.7 10.7 40.2 4.6 7.3 0.59 3 0.38 1.6 196 5.4

TR-PL-001-019 518828 5431751 1.37 984577 93 3600 5580 515 1590 154 32.1 83.2 7.1 28.6 4.2 9.5 1.09 6 0.81 4.1 124 20

TR-PL-007-046 518751 5431987 1.29 984516 117 3140 5150 504 1640 198 53.8 143 14.8 44 5.1 7.6 0.77 4.5 0.61 2 225 2.8

TR-PL-007-036 518746 5431991 1.28 984505 108 2980 5080 510 1710 216 62.3 165 17 46.3 5 8.9 0.68 4.2 0.6 1.5 258 3.2

TR-PL-003-013 518851 543174 1.25 985164 58 2510 5150 556 2000 207 43.1 95.4 7.1 23.1 2.5 4.6 0.48 3 0.45 1.6 162 16.3

TR-PL-007-005 518738 5431996 1.23 985055 88 2860 5100 508 1550 179 44.7 101 9.5 38.6 4.3 7.5 0.71 3.6 0.52 1.3 199 4

TR-PL-007-026 518741 5431994 1.21 984969 110 2930 4870 464 1500 167 43.6 132 11.8 42.6 4.9 8.6 0.85 4.4 0.62 2.9 183 4.1

Tr-PL-007-067 518756 5431999 1.13 984539 109 2550 4520 448 1510 218 59.8 146 14.1 41.5 4.7 7.6 0.67 3.1 0.4 2.7 257 6.7

TR-PL-007-048 518751 5431990 1.13 984518 86 2550 4460 459 1580 209 58.5 152 15.6 42.3 4.2 6 0.51 2.9 0.43 1.8 219 5.6

Tr-PL-007-068 518757 5432001 1.11 984541 25 2640 4470 438 1430 186 52.6 140 14 41.9 4.9 8 0.68 3.3 0.42 4.3 198 2.8




TR-PL-001-029 518811 5431749 1.09 984589 434 2140 3870 424 1530 275 88.4 242 30.2 134 18.7 37 3.56 16 1.83 1.5 480 20.3

TR-PL-007-041 517846 5431999 1.07 984511 109 2560 4360 426 1360 152 39.3 103 11.3 38 4.6 7.5 0.7 3.6 0.43 2.1 159 2.2

TR-PL-007-025 518743 5431993 1.05 984968 93 2500 4160 416 1390 172 48 141 13.2 42.5 4.5 8.8 0.84 4.8 0.68 2.8 206 3.1

TR-PL-008-010 518632 5432039 1.03 984957 241 2030 3770 413 1560 288 82 216 24.8 97.7 11.5 16.6 1.23 5.5 0.67 3.1 373 14.7

TR-PL-008-014 518631 5432086 1.01 984961 170 1950 3690 430 1640 312 89.5 220 21.7 74.2 8.2 12.7 0.94 4.6 0.62 3.6 399 8.6

TR-PL-008-012 518632 5432087 0.98 984959 249 1820 3500 397 1540 316 98.1 251 27.6 102 11.7 17.5 1.32 6 0.7 3.3 497 7.9

TR-PL-007-017 518735 5431996 0.95 985068 94 2050 3700 398 1430 181 48.5 123 12.3 41.3 4.5 7.2 0.66 3.8 0.56 1.5 207 3

TR-PL-007-019 518740 5431986 0.94 985074 67 2160 3860 389 1280 134 33.1 79.1 7.6 26.4 3.2 5.5 0.48 2.5 0.35 2.7 161 2.6

TR-PL-007-033 518747 5431989 0.91 984502 108 2110 3660 371 1210 136 35.2 96.4 10.5 33.9 4.5 8.8 0.81 3.7 0.46 2.8 148 2.3

TR-PL-007-013 518735 5431987 0.90 985064 49 2020 3630 384 1310 150 35.4 81.3 7.3 22.9 2.3 3.8 0.32 2.1 0.31 2.3 178 2.3

TR-PL-008-009 518630 5432089 0.89 984956 129 1700 3350 379 1450 252 71 182 18.3 60.7 6.3 8.1 0.62 3.5 0.48 2.3 350 8.1

TR-PL-007-016 518735 5431994 0.86 985067 82 2110 3420 333 1070 118 31.4 94.5 8.5 29.6 3.6 7 0.74 3.8 0.54 2.8 138 2

Tr-PL-007-054 518750 5432001 0.85 984525 95 2000 3350 342 1140 148 40.4 93.3 9.6 32.9 3.7 7.4 0.5 2.4 0.3 2.5 164 2.2

TR-PL-001-014 518829 5431764 0.84 984571 59 2310 3440 288 892 81.7 19.1 40.3 3.9 16.3 2.4 6.6 0.77 4.6 0.74 3.7 62.4 7.1

Tr-PL-007-074 518763 5431996 0.82 984547 91 2010 3320 315 995 104 25 64.4 7.5 27.7 3.7 6.3 0.54 2.5 0.32 2.6 97 2.8

PL-TR-001-031 518805 5431757 0.81 984592 217 1680 3060 316 1090 204 65.2 168 17.6 71.4 9.6 19.9 2.14 11.3 1.47 4.4 311 20.7

PL-TR-001-030 518808 5431759 0.81 984591 53 1770 3170 339 1200 187 48.3 86 5.8 19.4 1.8 3.5 0.43 2.7 0.38 0.2 264 5.6

TR-PL-007-037 518747 5431995 0.80 984506 68 1850 3190 316 1050 132 38.1 104 10.7 30.9 3.2 4.7 0.44 2.3 0.29 2 162 1.9

TR-PL-007-070 518759 5432005 0.79 984543 85 1810 3230 318 1030 121 31.4 82.7 9 28.9 3.6 6.1 0.58 3.2 0.39 2.4 115 1.8

TR-PL-001-023 518823 5431755 0.79 984583 61 2150 3220 291 829 70.4 15.3 44.4 3.9 17.1 2.5 5.7 0.72 4 0.6 2.9 66.4 2.6

Tr-PL-007-058 518752 5432006 0.78 984529 46 1740 3270 314 1030 124 31.3 77.9 7.5 19.8 1.9 2.7 0.26 1.4 0.19 2.2 121 1.7

TR-PL-007-010 518754 5431992 0.74 985061 77 1760 2990 302 978 100 23.9 60.5 7.1 28.6 3.6 6 0.54 2.9 0.41 2.4 100 2.1

TR-PL-007-066 518759 5431998 0.71 984538 141 1550 2700 287 980 155 44.9 119 13.3 47.1 5.8 8.3 0.71 3.5 0.42 2.7 209 9.7

TR-PL-001-011 518838 5431756 0.71 984567 40 1940 2880 242 736 83 23.7 56.6 5.2 16.5 1.9 4.4 0.5 2.8 0.43 3 106 13.4

TR-PL-007-031 518739 5431999 0.68 984974 56 1560 2840 268 860 97 25.4 78.4 6.9 23.4 2.6 4.5 0.46 2.5 0.37 2.7 103 1.7

TR-PL-003-022 518844 5431711 0.66 985174 58 1400 2540 278 1010 178 51.2 115 9.1 25.3 2.5 4.2 0.43 2.3 0.31 1.4 248 9.3

TR-PL-007-049 518748 5431992 0.66 984519 101 1580 2620 249 791 91.8 26 74.4 9.1 32.9 4.3 7.2 0.71 3.5 0.47 3 105 2.7

TR-PL-007-045 518750 5431983 0.65 984515 75 1470 2630 260 858 98.1 25.7 68.5 7.4 24.1 3.1 5.3 0.52 2.9 0.36 3.3 104 3.3

PL-TR-001-032 518801 5431758 0.57 984593 686 711 1550 183 735 208 91.6 305 49.8 230 31.3 56.2 5.18 24 2.69 1.5 365 22.3




TR-PL-001-012 518829 5431764 0.57 984568 149 1190 2110 213 772 150 51.2 129 15.1 53.5 6.8 12.7 1.2 5.9 0.73 0.9 259 11.5

TR-PL-007-021 518740 5431987 0.54 985076 58 1170 2200 227 765 84.4 20.5 50.1 5.2 19.4 2.5 5.1 0.5 2.6 0.32 2.6 106 2.4

Tr-PL-007-075 518763 5431999 0.51 984548 131 1100 2010 203 670 94.6 28 77.8 10.3 42.4 5.7 8.9 0.77 3.6 0.46 2.6 117 6.1

TR-PL-007-042 518746 5432000 0.51 984512 60 1180 2050 204 659 77.2 21.6 58.2 6.6 21.4 2.6 4.1 0.35 1.8 0.22 2.6 88.6 2

TR-PL-001-017 518820 5431755 0.51 984574 46 1450 2050 169 495 43.5 10.1 23.3 2.5 11.2 1.9 5.1 0.65 3.9 0.59 2.8 42.9 5.8

TR-PL-003-012 518850 5431714 0.50 985163 30 1180 2040 197 653 68.8 15.4 36.8 2.9 9.7 1.5 3.8 0.44 2.5 0.34 3.2 43.2 5.2

Table 10. Summary table of select assay results from soil samples collected on the Prairie Lake Property.


11-BCQ-0184 518607 5431873 0.03 11-BCQ-0184 19 43.2 155 9.9 35.6 7.5 1.93 6.2 0.8 4.4 0.8 2 0.31 1.9 0.29 7.2 18.8 1.9

11-BCQ-0185 518605 5431892 0.03 11-BCQ-0185 22 36.2 121 8.77 33.1 7.6 2.29 6.9 1 5.1 0.9 2.2 0.32 1.9 0.29 7.2 16.1 1.7

11-BCQ-0186 518603 5431893 0.02 11-BCQ-0186 14 29.7 62.5 6.87 24.6 5 1.18 3.7 0.5 2.9 0.6 1.6 0.23 1.6 0.26 8.7 9.9 1.8

11-BCQ-0187 518608 5431896 0.04 11-BCQ-0187 17 46 170 10 36 7.4 1.89 6 0.7 4 0.7 1.9 0.28 1.7 0.28 6.9 18.4 1.8

Table 11. Summary table of select assay results from rock samples collected on the Prairie Lake Property.

Sample Name TREO ActLab Number Y La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Hf Th U

11-LAM-005 2.94 985006 280 6830 11900 1200 3920 438 107 274 26.7 88.1 11 21.8 2.51 13.6 1.64 2.5 483 4.9 11-BCQ-0166 1.97 985324 92 3970 7790 857 3190 476 119 242 21.1 55.4 3.8 5.1 0.31 1.2 0.16 1 496 13.1 11-BCQ-0165 1.34 985025 105 3090 5380 585 1860 213 49.5 117 10.5 38.6 4.7 8.7 0.92 5.3 0.71 2.1 256 4.1 11-WJH-006 1.18 985009 39 2690 4780 497 1710 205 45.9 106 8.5 21.6 1.7 1.5 0.1 0.6 0.09 0.9 199 8.4 11-GMQ-006 1.04 985008 161 2020 3960 458 1630 285 86.7 206 20.5 64 7.2 12.4 1.13 5.9 0.68 0.6 395 4.3 11-BCQ-0177 0.69 985103 322 1300 2360 250 921 213 80.9 240 32.3 126 15.2 23.1 1.45 6.2 0.69 1.3 343 13.8 11-LAM-033 0.67 985022 251 1320 2530 265 972 140 36.7 95.6 12.9 64.8 10.6 24.3 2.47 12.3 1.53 0.7 265 284 11-LAM-044 0.58 985027 168 1120 2180 247 884 125 31.9 81.8 10.2 47.4 7 15.2 1.5 6.9 0.82 1.4 124 13.4 11-MLD-017 0.58 985109 973 601 1340 164 692 208 97.7 341 63.2 284 38.5 65.1 5.9 25.1 2.75 2.3 451 50.9 11-DTC-004 0.48 985049 138 783 1750 215 862 122 32.8 92 13.5 46 5.5 12 1.44 8.8 1.32 0.7 1650 17.4 11-LAM-003 0.42 985004 774 483 958 118 459 116 50.6 182 37.8 210 32.6 63.8 5.6 22.4 2.21 5.8 333 50 11-BCQ-0188 0.39 985108 169 527 1330 182 786 111 31.2 96.4 15.1 59.5 6.8 13.7 1.5 8.2 1.09 1 2080 13.9 11-BCQ-0178 0.32 985102 158 501 1090 132 538 94.4 27 70.1 9.2 41.2 6.3 13.4 1.49 7.7 0.99 1.4 68 39.4 11-LAM-004 0.32 985005 238 444 1020 132 536 104 28.8 74.1 10.6 52.1 9 23.5 2.95 18 2.45 2 84.4 28



Sample Name TREO ActLab Number Y La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Hf Th U

11-LAM-032 0.25 985021 362 374 745 79.7 305 54 16.6 54.5 11 67.8 13.2 32.2 3.95 21.5 2.82 3.1 145 72.3 11-WJH-014 0.25 985013 254 396 824 90.7 351 55.5 16 45 7.2 40.1 8 21.8 3.05 19.1 2.59 0.6 221 47.3 11-BCQ-0181 0.23 985104 423 286 597 71.2 287 52.6 16.6 50.8 10.2 66.4 14.3 38.4 5.31 27.5 3.61 3.7 146 36.3 11-MLD-011 0.21 985023 263 289 613 67.5 266 51.3 16.9 54.3 10.1 54.7 9.6 23.2 2.77 15.1 2.03 4.6 225 34.4 11-LAM-040 0.20 985024 66 411 773 77.4 277 44.6 12.5 33.4 4.1 16.7 2.5 5.4 0.64 3.8 0.53 1 178 8.1 11-BCQ-0179 0.19 985105 25 315 733 81.7 321 62.8 18.4 41.9 3.6 9.4 1.1 2.1 0.23 1.5 0.25 9.8 109 4.8 11-WJH-015 0.19 985014 569 141 353 36.2 152 37.4 15.8 63.6 16.1 100 19.5 46.1 5.4 28 3.28 1.6 243 94 11-DG-013 0.16 985017 162 245 510 57.4 224 38.4 11.5 33.5 5.4 31.6 6.1 15.3 1.99 11.3 1.56 3.4 97.8 26 11-DTC-005 0.15 985107 114 191 461 61.8 255 51.5 16.5 43 6.4 28.8 4.4 9.3 1.14 6.3 0.86 1.3 50.6 130 11-MLD-016 0.15 985106 94 245 485 58.5 228 44.2 15.2 45.5 7.6 32.3 4.3 8.1 0.75 3.4 0.46 2.6 92 8.2 11-DG-012 0.14 985016 150 214 456 51.1 204 36 11.2 32.6 5.6 31.7 5.9 14.6 1.81 10.3 1.35 1.5 36.6 12.4

11-MLD-010 0.13 985018 333 122 285 30 119 28.3 11.6 46.3 11.9 71.2 13.2 30.7 3.55 18.1 2.18 2 166 53.8 11-WJH-017 0.11 985019 165 154 332 37.6 153 28 8.39 26.2 4.8 28.3 5.5 13.8 1.81 9.6 1.32 3.6 78.2 39.5 11-BCQ-0189 0.09 985111 11 197 339 35 123 26.2 7.33 18.3 1.7 5 0.6 1.2 0.13 0.7 0.1 1.3 47.4 2.9 11-LAM-002 0.09 985003 186 30.2 93.2 17.1 100 61.2 28.5 94.2 15.3 64.6 8.6 13.3 1.22 6.1 0.7 0.5 123 5.8 11-LAM-001 0.05 985002 64 63 126 16.7 72.8 24.3 9.99 31.2 5.1 21.8 3 5.6 0.51 2.6 0.32 3.8 46.9 4.5 11-LAM-022 0.04 985012 25 74.6 129 14.8 54.5 12.3 4.25 12.1 1.7 6.9 1 2.6 0.35 2.2 0.31 3 17.4 2.3 11-BCQ-0190 0.03 985112 27 58.7 78.9 11.8 44.9 9.8 2.81 8.6 1.4 7.7 1.5 3.7 0.5 3 0.43 4.8 7.7 8.5 11-WJH-016 0.03 985015 42 32.6 71.2 7.91 33.5 7.6 2.32 7.9 1.2 6.9 1.4 3.9 0.53 3.7 0.59 4.9 7.5 2.3 11-BCQ-0162 0.02 985026 30 30.1 60.5 7.78 32.1 7.2 2.15 7 1.1 6.2 1.2 3.3 0.5 3.2 0.5 5.2 6.8 1.8 11-BCQ-0172 0.02 985042 13 42.9 77.2 8.5 29.4 5.6 1.9 5.2 0.8 3.7 0.5 1.3 0.18 1.2 0.21 1 11.6 1.8 11-BCQ-0174 0.02 985035 44 21.7 44.9 6.12 25.2 6 1.78 6.8 1.2 8 1.7 4.8 0.75 4.7 0.77 3.5 6.9 0.9 11-BCQ-0173 0.01 985043 37 7.1 14.3 1.85 8.1 3.1 1.88 5.5 1.1 6.5 1.3 3.8 0.58 3.8 0.67 1.1 10.4 1.7 11-BCQ-0175 0.01 985101 7 13.8 32 4 16.4 3.1 0.82 2.5 0.3 1.4 0.3 0.7 0.1 0.6 0.09 1.3 2.1 0.6 11-GMQ-005 0.01 985007 16 21.4 42.5 5 19.1 3.8 1.16 3.5 0.6 3.2 0.7 2 0.28 1.8 0.26 5.3 27.7 110 11-LAM-021 0.01 985011 5 11.1 23.5 2.79 11.2 2.7 1.02 2.3 0.3 1.2 0.2 0.4 0.025 0.3 0.04 2.2 3.8 0.6 11-WJH-003 0.01 985001 26 9.7 20.4 2.62 11 2.9 0.92 2.8 0.6 3.6 0.8 2.7 0.43 3 0.46 3.6 4.4 1.8

128 14BRecommendations


15 Recommendations

Samples collected during the 2011 field season from the Prairie Lake Property, yielded anomalous results; 32 samples out of 240 trench samples contained more than 1% TREO. X and Y populations were identified indicating…

It is recommended that a fixed wing airborne magnetic and radiometric survey of the property be flown. After analysis of the regional radiometric and magnetic data, anomalous areas should be investigated, trenched if possible and drilled, especially if they lie under cover and swamps.

16 References

Ayres, L.O., Card, K.D., and Lumbers, S.B., 1971, Diagram A- Generalized Distribution of Major Lithologic Units and Structures; Ontario Department of Mines and Northern Affairs, Map 2196.

Bell, K., and Blenkinsop, J., 1980, Ages and Initial 87Sr-86Rb ratios from Alkalic Complexes of Ontario, p 16-23 in Geoscience Research Grant Program, Summary of Research, 1979-1980, Ontario Geological Survey, Miscellaneous Paper 93.

Marianos, 2011, Personal communication

Sage, R.P., 1987, Prairie Lake Carbonatite Complex, Geology of Carbonatite- Alkalic Rock Complexes in Ontario, District of Thunder Bay, Mines and Minerals Division, Ontario Geological Survey Study 46.

129 16BAppendices


17 Appendices

17.1 Summary Table of Expenses

17.2 Work Done per Claim

17.3 Workers Rates

130 16BAppendices


17.1 Summary Table of Expenses

Table 12. Summary table of expenses.

Work Done Associated Costs

Transportation

Food and Lodging

Company

Assa

ys

Geo

phys

ical

Pros

pect

ing

Phys

ical

Com

bine

d As

soci

ated

Co

sts

Com

bine

d Tr

ansp

orta

tion

Cos

t

Com

bine

d Fo

od a

nd

Lodg

ing

Cost

Mackevoy $43,166.68 $36,624.47 $40,601.55 $8,129.41 $22,375.33 $5,812.45 CIN $169.81 $3,966.09 $38,293.60

Belham $43,903.63 $3,828.12 $17,358.08 $16,618.87 ActLabs $36,752.64

TOTAL $36,752.64 $43,166.68 $36,624.47 $84,505.18 $12,127.34 $43,699.50 $60,724.92

131 16BAppendices


17.2 Work Done per Claim

Claim number

Expiry date

Work required

Claim units

Ownership Township Area (hectacres)

Prospecting

Amount prospecting

Physical

Amount Physical

Geophysical

Amount Geophysical

4256251

12-Apr 1200 3 Rudolf Wahl

100% Killala Lake 48 10% $3,662.45 5% $4,225.26 10% $4,316.67

4256252


100% Killala Lake 256 25% $9,156.12 95% $80,279.92 25% $10,791.6

7 425625

3 12-Apr 6400 16 Rudolf Wahl

100% Killala Lake 256 $0.00 $0.00 $0.00

4256254


100% Killala Lake 256 $0.00 $0.00 $0.00

4256255


100% Killala Lake 128 5% $1,831.22 $0.00 5% $2,158.33

4256256


100% Killala Lake 176 $0.00 $0.00 $0.00

4256257


100% Killala Lake 192 $0.00 $0.00 $0.00

4256258

12-Jun 5200 13 Rudolf Wahl

100% Killala Lake 208 $0.00 $0.00 $0.00

4246258

12-Jan 4800 12 Rudolf Wahl

100% Killala Lake 192 $0.00 $0.00 $0.00

4246259


100% Killala Lake 256 $0.00 $0.00 $0.00

4246260


100% Killala Lake 256 20% $7,324.89 $0.00 20% $8,633.34

4246261


100% Killala Lake 256 20% $7,324.89 $0.00 20% $8,633.34

4246262


100% Killala Lake 256 20% $7,324.89 $0.00 20% $8,633.34

4256259

12-Nov 6400 16 Rudolf Wahl

100% Killala Lake 256 $0.00 $0.00 $0.00

4256260


100% Cairngorm

L. 256 $0.00 $0.00 $0.00

4256261


100% Cairngorm

L. 256 $0.00 $0.00 $0.00

4246255


100% Killala Lake 208 $0.00 $0.00 $0.00

4246269


100% Killala Lake 256 $0.00 $0.00 $0.00

4246270


100% Killala Lake 128 $0.00 $0.00 $0.00

TOTAL 4096 100.00% $36,624.47 100% $84,505.1

8 100% $43,166.68

132 16BAppendices


17.3 Workers Rates

Person Qualifications Hourly Rate

Beverly Quist (B. Quist) M.Sc. (Geology)

B.Sc. (Geology)

$62.50

Mallory Dalsin (M. Dalsin) M.Sc. (Geology) (in Progress)

B.Sc. (Geology)

$56.25

Luke Marshall (L. Marshall) B.Sc. (Geology) $50

Avee Ya’acoby (A. Ya’acoby) B.Sc. (Geology) $50

Geoff Quist (G. Quist) B.Eng. (in progress) $37.50

Shuan Todd (S. Todd) B.Sc. (Geology) (in progress) $37.50

Dasha Gritsaenko (D. Gritsaenko) B.Sc. (Geology) (in progress) $37.50

Wes Harman (W. Harman) B.Sc. (in progress) $28.13

David Cameron (D. Cameron) B.A (in progress) $28.13

Steve Vachon (S. Vachon) High School diploma $28.13

33 J Appendices -------------------------

This report was completed on November 14, 2011

Written by:

Beverly Quist M.Sc

Mackevoy Geosciences Ltd.

Approved by:

Michael Schuss

President and CEO

Canadian International Minerals Inc.


prairie lake rare earth property · that trends north-northeast and extends for more than 600 km...

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