r.o.w. fowler #1 property nts 42c13 - ontario · 2017-01-17 · 42c13sw0025 2 16219 wabikoba lake...
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42C13SW0025 2 16219 WABIKOBA LAKE 010
HEMLO GOLD MINES INC.
REPORT OF WORK
FOWLER #1 PROPERTY
N.T.S. 42C13
SUPERIOR DISTRICT
Project No 429 Hemlo, Ontario March 9, 1995
Paul JohnstonGeologistHemlo Gold Mines Inc.Superior District
l
Table of C 42C13SW0025 2.16219 WABIKOBA LAKE 01OC
Page
SUMMARYI.0 INTRODUCTION..........................................................................................................12.0 LOCATION AND ACCESS.......................................................................................... 13.0 PROPERTY DESCRIPTION ........................................................................................14.0 PREVIOUS WORK......................................................................................................35.0 REGIONAL GEOLOGY ...............................................................................................46.0 LINECUTTING.............................................................................................................47.0 TRENCHING AND SAMPLING....................................................................................^8.0 PROPERTY GEOLOGY..............................................................................................^
8.1 Introduction ............................................................................................58.2 Lithologies..............................................................................................58.3 Alteration................................................................................................68.4 Metamorphism and Deformation.............................................................6
9.0 GEOPHYSICAL SURVEYS..........................................................................................69.1 Introduction ............................................................................................69.2 Instrumentation.......................................................................................?9.3 Interpretation......................................................................................... 8
10.0 CONCLUSIONS AND RECOMMENDATIONS .............................................................910.1 Geology...............................................................................................910.2 Geophysics........................................................................................ 10
II.0 Appendix lAssays, Whole Rock, Multi-Element Analyses and Sample Descriptions
12.0 Appendix MStatement of Authorship and Qualifications
List of Figures and Maps
Figure 1 Location MapMap 1 Geology Sheet 1Map 2 Geology Sheet 2Map 3 Geology Sheet 3Map 4 Trench 150 E Sample LocationsMap 5 Trench 153 E Sample LocationsMap 6 Trench 156 E Sample LocationsFigure 2 IP Dipole ArrayLine 15200E Induced PolarizationLine 15400E Induced PolarizationLine15500E Induced PolarizationLine15600E Induced PolarizationLine 15800E Induced PolarizationMap 7 Contoured Magnetic SurveyMap 8 Magnetic Profiles along linesMap 9 Induced Polarization Anomaly Map
Scale
1:50001.50001:50001:2501:2501:250
1:5000 1:5000 1:5000 1:5000 1:5000 1:5000 1:5000 1:5000
SUMMARY
During the period of June 14 through to November 29, 1994, a work program consisting of geological mapping and sampling, a magnetometer survey, an Induced Polarization/Resistivity survey, and overburden trenching l stripping was conducted on the Fowler #1 claim group. This claim group is located approximately 6 km east of Highway 614 and 15 km north of Highway 17.
The results of this work have shown that a strong alteration system is centred on a small quartz-feldspar porphyry stock referred to as the Armand Creek Quartz Feldspar Porphyry (ACQFP). Despite disappointing results of samples taken from surface exposures, the geological similarities between this property and Hemlo warrant further work. Drilling has been proposed to evaluate the alteration across the ACQFP with emphasis on its southern contact where it has not been intruded by the Musher Lake Porphyry.
1.0 INTRODUCTION
During the period of June 14 through to November 29, 1994, an exploration program consisting of geological mapping, magnetometer and IP. surveys, and overburden trenching/stripping/channelling was conducted on the Fowler #1 property. The results of this work program are contained herein.
Work focused on delineating a quartz-feldspar porphyritic unit with characteristics similar to the quartz-feldspar porphyry intrusion associated with the Hemlo gold deposit.
2.0 LOCATION AND ACCESS (Figure 1)
The Fowler #1 property extends from Musher Lake to approximately 1.0 km east of Highway 614. The centre of the property is located 18 km northeast of the Hemlo Mines.
The property is accessed from the Twist Lake timber road, which crosses Highway 614, approximately 15 km north of the Highway 17/ 614 junction.
3.0 PROPERTY DESCRIPTION (Figurel)
The mining claims on which exploration work was performed are:
CLAIM NUMBERS # of units
TB 1099990 1TB 1153692 1TB 1166521 1TB 1166522 1TB 1166523 1TB 1166524 1TB 1166525 1TB 1166526 1TB 1183291 1TB 1183292 1TB 1196846 2TB 1196847 12TB 1196848 10TB 1196849 8TB 1196850 2TB 1197158 6
16 claims 40
The above claims are held by Hemlo Gold Mines Inc. and form part of an option agreement with Fowler/Shuman.
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HKM1X) COLI) MINK SJTK
FIGURE 1 : LOCATION MAPnCATTHN MAP
4.0 PREVIOUS WORK
The following is a summary of previous work conducted on various portions of the Fowler #1 property:
Mclntyre-Porcupine Mines, Von Klien option, 1962
Discovery of a number of copper-nickel and copper-lead-zinc occurrences. Electromagnetic conductors and magnetic anomalies were tested with 28 diamond drill holes, but mineralization was weak and discontinuous with depth. There was no drilling on the Fowler #1 claim group.
Noranda Exploration Co. Ltd, 1976
Dotted Lake airborne survey completed over the area.
Pryme Energy (North), 1982
Work concentrated on the Mcintyre occurrence, located northwest of the Fowler #1 claim group.
Oued Resources, 1983
Geological mapping , trenching and drilling was completed on a claim group immediately north of the Fowler #1 property. Emphasis was on stratabound gold mineralization within iron rich interflow sedimentary sequences. Four zones were outlined but all occur north of the Fowler #1 property. Drilling returned values of up to 0.025 oz/ton over 3 metres.
Norman Resources Limited, 1983
Geological mapping, soil geochemistry, airborne magnetics and VLF-EM covering an area immediately west of the present claim block. Soil samples were all low range with one sample returning 45 ppb. No major near surface concentrations of precious metals were discovered.
Baylore Resources Limited, 1983
Airborne Magnetics and EM covering the eastern part of Fowler #1.
Kelly-Kerr Energy Corp., 1986-1988
Geological mapping, stripping, soil geochemistry covered an area in the northwest corner of the present claim group.
Noranda Exploration Co. Ltd, Newjay Property, 1987-1989
Humus geochemistry and geology filed. No anomalous Au values were found in the 23 rock samples analyzed. A weak Au humus anomaly is reported to overlie a felsic-mafic contact.
Noranda Exploration Co. Ltd, Norman Resources Property, 1989
Geological report, plans, soil/rock geochemistry and assays filed for a claim block located south of Armand Lake. Several anomalous Au values were recorded from the soil survey samples but results were not considered encouraging.
3
Fowler/Shuman, Armand Lake Property, 1991
Property report covering prospecting and stripping.
Newmont Exploration of Canada Ltd., 1992
Geological and lithogeochemical reports for a claim group adjacent to the eastern side of the present claims.
Hemlo Gold Mines Inc., 1994
Trenching and geological mapping of trenches 150E, 153E and 156E on the Fowler #1 property.
5.0 REGIONAL GEOLOGY
The Fowler #1 property is located within the Archean Schreiber-Hemlo greenstone belt which forms a part of the Abitibi-Wawa-Shebandowan Subprovince of the Superior Province. The area contains a dominantly southeast striking sequence of metavolcanic and metasedimentary rocks bounded to the south by the Musher Lake Granodiorite pluton.
Supracrustal rocks consist principally of basaltic flows and subordinate tuffs, with intercalations of epiclastic arkosic wacke and siltstone. Interbeds of felsic volcanic tuffs and/or volcaniclastic sediments occur locally. Numerous small elongate quartz-feldspar porphyry (QFP) stocks intrude the sequence. Equigranular to porphyritic dikes and sills intrude the volcanics, sediments, and small QFP stocks.
6.0 LINECUTTING
17.9 kilometres of grid was cut on the Fowler #1 property during December, 1993, May, 1994 and November 1994 by Vytyl Exploration of Thunder Bay. Grid lines were oriented north- south and spacing varied between 200 and 400 metres with stations established at 25 metre intervals.
7.0 TRENCHING AND SAMPLING (Appendix l)
Three trenches completed in an earlier program were sampled using a diamond saw to extract a channel sample across favourable rock types. A total of 103 samples were collected and submitted to Accurassay Laboratories of Thunder Bay for gold assays. Assaying was by fire assay with an atomic absorption finish. Selected samples were submitted to Chemex Labs Ltd of Thunder Bay for ICP analysis to determine whole rock and trace element composition.
An additional 37 samples were collected during prospecting of the property and were as well submitted for gold assays.
No economic gold values were encountered with the majority of the samples returning Au.
8.0 PROPERTY GEOLOGY (Maps 1 to 3)
8.1 Introduction
During the period from June 14 through October 25, 1994, geological mapping was conducted on the Fowler #1 property by Paul Johnston, under the supervision of John Londry. Mapping was performed along cut grid lines.
Geological data from previous mapping was reviewed and updated where necessary.
8.2 Lithologies
8.2.1 Mafic Metavolcanics
Mafic volcanics that underlie the northern third of the property consist primarily of massive flows with minor pillow structures and flow breccia. Pillow structures noted north of the property dip steeply to the south and indicate a southerly top direction.
The mafic volcanics are dark green, fine grained, with varying amounts of chlorite and amphibole. Minor alteration consisting of minor feldspathic fractures and minor carbonitization is present proximal to the QFP stocks.
8.2.3 Clastic Metasediments
A 100 metre wide band of clastic metasediments consisting of siltstone, fine sandstone, and minor interbeds of heterolithic pebble to cobble conglomerate extends across the northern part of the property. The metasediments are grey to dark grey with light grey-brown coloured weathered surfaces. They are typically immature quartzo-feldspathic sediments, containing minor biotite and amphibole, and rare garnet. Primary structures were not recognized in this mapping program.
8.2.5 Quartz Feldspar Porphyry Intrusion
A small elongate quartz-feldspar porphyry (QFP) intrusion flanks the northern contact of the Musher Lake Pluton. The QFP is light grey to grey and weathers white to light brown. Previous mapping identified this unit as a felsic tuff, however, delineation of the unit through grid line mapping and trenching combined with the texture of the quartz and feldspar phenocrysts and ground mass suggests this unit is an intrusive body. The unit is discordant to the sequence of mafic volcanic and sedimentary units in the area. Quartz and feldspar phenocrysts are fairly uniform in size and are intergrown with the groundmass suggesting crystallization from a melt rather than deposition from pyroclastic material.
Heterolithic clastic units occur within and along the margins of the QFP and contain mafic volcanic and QFP clasts. Lenses of green mica and up to 50Xo fine pyrite is common within the clastic unit. These clastic units appear to be related to the emplacement of the QFP and are interpreted as hydrothermal breccias.
8.2.6 Granodiorite Dikes
Narrow (10-200 cm) equigranular to moderately feldspar porphyritic dikes intrude volcanic, sedimentary and QFP units. The dikes occur across the property but appear to be more frequent near the QFP. Multiple phases of dikes are recognised but a consistent classification has yet to be established.
8.2.7 Granodiorite Pluton
The Musher Lake pluton is an arcuate granodiorite intrusion located south of the property. This pluton is weakly foliated near its contacts with the supracrustal rocks. Mafic xenoliths are common throughout the granodiorite. The pluton clearly post-dates the QFP as apophyses of granodiorite intrude the QFP. Irregular pegmatite dikes and pods are commonly observed in exposures of granodiorite.
8.3 Alteration
Intense alteration is associated with, and centred on the Armand Creek Quartz Feldspar Porphyry. Two main alteration phases have been noted. Early fracture controlled microcline alteration is overprinted by pervasive and fracture controlled muscovite (sericite). Green mica is associated with sericitic fractures and with clastic units interpreted as hydrothermal breccias. Weak alteration of the mafic volcanic country rock is present as diffuse feldspathic fractures and minor chloritization. A fine grained dike phase consisting of equigranular quartz and feldspar appears to be sericitically altered. Minor fine grained pyrite and trace sphalerite and magnetite is disseminated within the QFP. Pyrite is also within narrow veinlets that form the cores of alteration fractures.
8.4 Metamorphism and Deformation
Rocks in the area indicate amphibolite grade metamorphic conditions as indicated by amphibole in the mafic volcanic units. Garnet was the only aluminosilicate indicator mineral identified on the property. Chlorite does occur along with amphibole in the mafic volcanics and is pronounce adjacent to the Armand Creek Quartz Feldspar Porphyry.
The rocks have been strongly deformed as indicated by elongate clasts (in plan) in both the hydrothermal breccias and conglomerate units. Clasts do not appear to be elongated in the plane of foliation. Exposure was not adequate to allow mapping of geological structures such as folds or faults. Magnetic data was useful for interpreting the position of diabase dikes but the data does not indicate any major fault offsets. Magnetic contrast in rock types on the property are not sufficient to distinguish fold patterns.
Elongated quartz phenocrysts with the ACQFP indicate that it has be flattened. The overall shape of the ACQFP is lenticular and does it does not appear to be folded.
9.0 GEOPHYSICAL SURVEYS
9.1 Introduction
Approximately 5 kilometres of induced polarization (IP) and 7.2 km of magnetic survey were performed on the Fowler 1 claims. One four man crew consisting of Noranda Exploration Company, Limited (no personal liability) personnel J. Maclsaac, D. Hancock, L. Cross and H. Palomaki performed the work during the period November 26-29, 1994.
9.2 Instrumentation
9.2.1 Magnetometer Survey
A Scintrex IGS proton precession magnetometer system was used. Total magnetic field readings are taken with a precision of 0.2 nT or Gammas, although the accuracy is generally +I- 5 nT. Readings are corrected for diurnal variations using an identical recording unit set up as a base station in a non-anomalous area. Base station readings are taken every 30 seconds unless large or rapid variations are anticipated, in which case readings are taken more frequently.
For this survey base station readings were taken at a 30 second interval. Survey readings were recorded at 12.5 meter intervals along the line.
9.2.2 Induced Polarization and Resistivity Survey
The Dipole-Dipole survey was performed using an IPT1 transmitter, a 2.5 kilowatt Honda generator and an ELREC IP-6 receiver.
Survey parameters were 50 m dipole separations ('a' spacings) with readings recorded at six receiver separations (n^ to 6). Figure 2 shows the plotting convention used to plot 'pseudo' sections which present chargeability and resistivity results.
IP chargeability represents the voltage retention capacity, or capacitance of the ground. It varies with metal, clay or graphite content of the ground, grain size, and the degree to which grains are inter-connected. It is measured as an average of ten 'windows' or time slices under the voltage decay curve of the ground being surveyed. The units are millivolts per volt (mV/V) or milliseconds (msec).
IP resistivity is a measure of the electrical resistance over a linear distance of the ground. This varies with metal, clay or graphite content, but is also sensitive to the bulk composition of overburden, bedrock and mineralization, and can be used as a lithological mapping tool. It is measured by combining the voltage measured between receiving electrodes with the current transmitted at the transmitting electrodes in a two dimensional approximation of Ohm's law (Rz vVI) that is represented by the following formula:
Resistivity = pi * Voltage * n * (n+1) * (n+2) * a Current
Where pi is a numerical constant approximately equal to 3.14159, 'n' is a multiplier (in this case 1 through 6) that represents the distance of the receiver electrode pair from the transmitter electrode pair and 'a' is the separation of the two electrode locations in the receiver and transmitter electrode pairs (please see Figure 3). The resistivity units used for plotting are Ohm-meters.
Figure 2
Dipole-Dipole Arrayna
l iH2H
Plot Point
9.3 Interpretation
Line 15200E: The anomaly at 9715N is narrow and shallow, but well defined and high amplitude. It is directly related to a resistivity low.
The anomaly at 9825N was not completely covered by the survey and remains poorly defined, but high amplitude. It exists within a moderate resistivity high background.
Line 15400E: The anomaly at 9600N is well defined, narrow and near surface. It occurs at a distinct resistivity high-low (south-north) contact.
The anomaly at 9725N is poorly defined because it is not covered by the survey, however this is a high amplitude anomaly that exists within a moderate resistivity high background.
Line 15500E: The anomaly at 9550N is probably a single dipole, narrow and near surface source as it was on lines 15400E and 15200E, however a high chargeability background has distorted its shape. The high chargeability background occurs as a sharp contact that is represented in the resistivity as a high-low (south-north) abrupt change.
The anomaly at 9725N is not completely defined by the survey but high amplitudes are present.
Line 15600E: A weak anomaly is present at 9425N. It is narrow and corresponds with an elevated resistivity high response.
At 9500N the anomalously high chargeability that was present on the north portions of the western three lines is again present. Individual narrow, shallow sources can be identified in the broad chargeability package. The anomaly is not as well defined as it was on previous lines, and the resistivity high-low (south-north) contrast is not as pronounced.
Line 15800E: The resistivity high-low (south-north) contrast present on the western 4 lines is well defined on this line at 9450 N. A corresponding increase in chargeability is present, but
8
amplitudes are not as high as they were on the western lines. A surface clay layer has distorted the chargeability data on the north half of the line.
Line 16000E: A weak, narrow, and shallow single dipole anomaly is present at 9200N. This anomaly is related to a single dipole resistivity low that plots one dipole north of the chargeability response.
A single dipole (narrow and shallow) chargeability response also occurs at 9350N . This response is related to the resistivity high-low (south-north) contrast described on the western lines. The strong chargeability background is weaker on this line and an over-all drop from west to east is recognized, however a strong and well defined chargeability anomaly is present within this zone.
The anomaly at 9575N is strong and well defined. Good depth extent is indicated and depth to top may be 50 m although this is difficult to establish because the surface clay layer that affected the north half of line 15800E is also present on this line. The anomaly is still not completely covered by our grid.
10.0 CONCLUSIONS AND RECOMMENDATIONS
10.1 Geology
Similarities between the Armand Creek Quartz-Feldspar Porphyry (ACQFP) and the Moose Lake Porphyry associated with the Hemlo deposit are listed below:
(1) Early microcline event followed by intense sericitic alteration within the core of the stock. Abundant tourmaline is associated with sericitization.
(2) Green mica associated with felsic stocks.
(3) Hydrothermal brecciation associated with felsic stocks.
(4) Small size dimensions, less than 5 km long, less than 500 metres wide. Both stocks appear strongly flattened but not folded.
(5) Evidence of multi-phase intrusive activity with intrusive events predating and post-dating alteration events.
Hydrothermal alteration related to the ACQFP intrusion positively influences the potential for mineralization in the area. Limited outcrop across the property has made interpretation of distribution of alteration phases difficult. Exposure is primarily concentrated on the northern contact of the ACQFP. Mapping and trenching concentrated on delineating the ACQFP and the results indicate that the Musher Lake Pluton has intruded along the southern contact of the ACQFP, effectively removing the potential for mineralization along this contact near the surface. Trenching was successful in exposing complete sections through the ACQFP and the potential for mineralization on the western portion of the property is small.
There has now been extensive sampling of the surface exposures of the ACQFP and the results have been disappointing. Unfortunately, these samples are strongly biased towards the northern contact of the ACQFP. There is still potential for mineralized zones existing along the southern contact of the ACQFP in the eastern part of the property where the ACQFP has not been intruded by the Musher Lake Pluton.
Mafic volcanic host rocks are an important departure from the Hemlo analogy in that they, so far, show limited effects of hydrothermal alteration. Sedimentary units found to the
south of the ACQFP may reveal aKeration patterns that aid In directing exploration towards more intense alteration and potential mineralization. ;
The strong geological similarities between Hemlo and this property require thorough Investigation of the ACQFP unit to evaluate the nature and distribution of alteration phases. One drill hole Is recommended on the eastern part of the property io provide additional geological Information and a sample medium for further geochemical analysis. Mapping and trenching has that shown that the Musher Lake Pluton has not disrupted the southam contact of ACQFP In the eastern side of the property. ;
10.2 Geophysics
It is likely that a lithologic change occurs from B300N on line 16000E through to 9700N on tine 15200E. The northern lithology Is characterized by a high (15-20 mVA/) chargeability background response and a moderate resistivity (2500 - 7000 ohm-m). The southern lithology has a background chargeability of 4-5 mV/V and a resistivity response M Ok ohm-m.
Within the southern zone there are two weak, narrow chargeability anomalies these occur on lines 15600E and 16000E.
Within the north zone there Is typically an elevated shallow and narrow chargeability response associated with the reslstlvity/chargeabllity contact, and there Is always a stronger chargeability response that occurs 100 -150 m north of the contact. The stronger chargeability response is not completely covered by our survey lines, but from a geophysical point of view it looks very interesting. : '. .
It Is recommended that both the resistivity/changeability contact and the anomaly that occurs within the northern zone be tested. The best definition of the north zone occurs on line 16000E although the anomaly may be quite good oh line 15400E If this line can be extended north. The best place to test the contact anomaly is on line 15400E or 15500E. The strongest response fs on line 15800E, but this may be due to an over-all higher background chargeability at this location.
Respectfully submitted,
Htmto Ooid Mines. Inc
2.T/v
luTJohnston Geologist Superior District
Hemlo, Ontario March 9,1995.
10
APPENDIX l
Assays, Whole Rock, Multi-Element Analyses and Sample Descriptions
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC
. 1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6Q3
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NORANDA EXPLORATION CO., LTD, Bag Service # 8 Marathon, Ontario POT 2EO
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Job #9441152*.
Project # 529
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ACCURASSAY LABORATORIES^ DIVISION OF ASSAY LABORATORY SERVICES INC.
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PHONE (807) 623-6448FAX (807) 623-6820
.Page 2
NORANDA EXPLORATION CO., LTD. Bag Service # 8 Marathon, Ontario POT 2EO
October 11, 1994
Job #9441152
Project #529
Sample # Accurassay Customer
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Certified
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820
Page 3
NORANDA EXPLORATION CO., LTD Bag Service #8 Marathon, Ontario POT 2EO
October 11, 1994
Job 89441152
Project f 529
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CERT
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551 I
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205
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226
226
226
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70 .
00
58 .
03
57 .45
75 .00
72.30
70. 10
84.20
73 .50
45.58
TiO2
?Z
0.51
0 .73
0. 66
0 .25
0.24
0.39
0.19
0.18
0.18
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^
1.67
1.06
1.01
1.91
1.06
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3.94
6.51
14 .34
TOTAL
?i
100 .50
100 .
85
101.25
100 .25
100 .35
100.80
99 .
02
99.79
92. 87
Ba ppm
280
1320
730
400
280
780
ISO
50
40
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35
40
30
40
IS
30
< 5
< S
< 5
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250
1520
870
360
390
970
3120
640
510
Nb ppm
< 10
< 10
< 10
< 10
< 10
< 10
< 10
< 10
< 10
Zr ppm
90
160
170
80
70
110
140
80
40
m
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20
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< 10
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10
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P
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NO
RA
ND
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XP
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D.
BAG
SE
RV
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#8
MA
RA
THO
N,
ON
TAR
IO
POT2
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Proj
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Com
men
ts:
533
ATT
N:
JOH
N L
ON
DR
Y
Page
NL
^^.*
' :1
-A
Tota
l Pag
is
: 1
Cer
tific
ate
Dat
e: 1
9-JU
L-94
In
voic
e N
o.
: 194
1937
8 P.
O.
Num
ber
: A
ccou
nt
:FlL
CC
: JO
HN
SU
LLIV
AN
"CO
RREC
TED
CO
PY"
CE
RT
IFIC
AT
E O
F A
NA
LY
SIS
A94
1937
8
SAM
PLE
55
5
A5
55
B
5
55
C
5
55
D
5
55
E
555
F
555
G
55
5
H
55
5
I
55
5
J
PR
EP
C
OD
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20
5
20
5
20
5
20
5
20
5
20
5
20
5
20
5
20
5
20
5
226
22
6
22
6
22
6
22
6
22
6
22
6
226
22
6
22
6
A1203
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15.5
2
15
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1
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5
17
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7
16
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16.7
2
16.9
4
15
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5
0.7
6
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CE
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OR
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D F
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Rb
RE
SU
LTS
*
Chem
ex L
abs
Ltd,
Anal
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al C
hem
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* G
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emis
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Reg
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red
Assa
yers
5175
Tim
berle
a Bl
vd.,
Mis
siss
auga
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ntar
io,
Can
ada
L4W
2S3
PH
ON
E: 9
05-6
24-2
806
NO
RAN
DA
EXPL
OR
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N C
O.,
LTD.
BAG
SER
VIC
E #8
M
ARAT
HO
N, O
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RIO
PO
T 2E
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Pro
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:53
3AT
TN: J
OH
N L
ON
DR
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Page
N
.sr
:1-B
To
tal P
ages
: 1
Cer
tific
ate
Date
: 19-
JUL-
94
Invo
ice
No.
: 194
1937
8 P.
O.
Num
ber
: Ac
coun
t :F
IL
CC: J
OH
N S
ULL
IVAN
IPIr
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REC
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A941
937
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PLE
55
5
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B
55
5
C
555
D
55
5
E
55
5
F
555
G
555
H
555
I 555
J
PREP
CO
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20
5
20
5
205
20
5
205
205
205
20
5
20
5
205
22
6
22
6
22
6
22
6
22
6
22
6
22
6
226
226
226
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2 0.2
2
0.2
8
0.2
6
0.2
5
0.2
8
0.2
4
0.4
0
0.3
2
0.4
7
0.1
5
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0.8
6
1.7
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2.5
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0
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101.2
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0.
90
9
9 .
97
Ba
ppm
350
62
0
1330
94
0
1040
1130
1470
960
10
5
60
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35
65
110
10
0
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120
60
65
15
65
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370
330
90
140
10
50
33
0
12
40
570
92
0
330
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120
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17
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270
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
L070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT 2EO
July 19, 1994
Job #944698
Project #505
G
Sample ft Accurassay Customer
1 1693-A2 1693-B3 1693-C4 1693-D5 ' 1693-E6 1695-A7 1695-B8 1695-C9 1695-D
10 1695-E11 Check 1695-E12 1695-F13 1695-G14 1695-H15 1695-1 '16 1695-1(2}17 1695-J18 1695-K19 1695-M20 1695-N21 Check 1695-N22 1695-023 1696-A (1695 AA)24 1696-B25 1696-C26 1696-D27 1696-E28 1696-F
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LJSs^WJyijl \ -
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT'2EO
July 19, 1994
Job #944698
Project #505
AccuraseaySample
Customer
12 '
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1695-1(2) 1695-J1695-K1695-M1695-N1695-N1695-0
1696-A (1695 AA) 1696-B1696-C1696-D1696-E1696-F
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Certified By:
ACCURASSAY LABORATORIESJL A DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6020Page 2
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario - POT 2EO
July 19, 1994
Job #944698
Project #505
Sample # Accurassay Customer
293031 Check3233343536
1696-G1697-A 1697-A 1697-B 1697-C 1697-D 1697-F 1697-G
Gold ppb
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Certified By;
3i±rM-r DT - D/AT, emr.LADS LTD.
OUT ZOO
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
NORANDA EXPLORATION CO., LTD.
Bag Service #8 Marathon, Ontario POT 2EO
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B GG3
PHONE (807) 623-6448FAX (807) 623-6820
Page 1
August 9, 1994
Job 0944698
Project tt 505
Sample tt
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Certified By
1ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PH6NE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., Bag Service #8 Marathon, Ontario POT 2EO
LTD. July 26, 1994
Job #944710,j '
Project #505
Accurasaay
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO,, LTD. Bag Service #8 Marathon, Ontario POT 2EO
July 26, 1994
Job #944731
Project #505
Accurassay
123456789
Sample fCustomer
9957-A 9957-B 9957-C 9957-D 9957-E 9957-F 9957-G 9957-H 9957-1
Gold ppb
<5 O
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^.001 ^.001 <0,001 •iO.OOl <0,001 <0.001 <0.001 <0.001 KO.OOl
Certified By:
13 : 2'J :ACC-L.RASSAY LABS LTD.- 12381038;# 2/
ACCURASSAY LABORATORIES/l DIVISION OF AS5A Y LABORA TORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B CG3
PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. July 29, 1994 Bag Service #8Marathon, Ontario Job #944742 POT 2EO
Project #505
Sample # Gold Gold Accurassay Customer ppb Oz/t
1 9957-J 28 ^.0012 9957-K < 5 < 0.0013 9957-L <5 <0.0014 9957-M <5 <0.0015 9957-N < 5 < 0.0016 9957-0 <5 ^.0017 9957-P <5 CO.0018 9959-A 27 ([O.OOl9 Check 9959-A 28 ^
Certified By:
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY, ONTARIO P7B 6G3
v, PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT 2EO
August 4, 1994
Job #944766
Project #505
Sample # Accurassay Customer
123456789
101112
Check
9962-A 9962-B 9962-C 9962-D 9962-E 9962-F 9962-G 9962-H 9962-J 9962-K 9962-K 99.G2-L
Gold ppb
6 (5
78
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Certified By
r
O- 0-31 i l ? 'Z-'1l OOT ZOO
••'V&fe ,\i i:"-' ' ,' t i i
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT 2EO
AccurassaySample #
123456789
101112131415
Check
Customer
9962-19963-A9963-B9963-c9963-D9963-E9963-F9963-G9963-H9963-19963-19963-J9963-K9963-L9963-M
Page l
Augustus, 1994
Job #944776
Project #505
94
Gold Ppb
76
1267
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Gold Oz/t
^.001<0.001<0.001<0.001^.001o.ooi<0.001<0.001<o.oo^O. 001^.001<0.00l<0.001<0.001XO.nni
LAD3 LTD. -* l DOT ZOO
ACCURASSAY LABORATORIES"] l X A DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE, UNIT 2* THUNDER BAY. ONTARIO P7B6G3
PHONE (807) 623-6448 FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. August 4, 1994 Bag Service #8Marathon, Ontario Job #944766 POT 2EO
Project #505
Sample # Barium Accurassay Customer ppra
l 9962-L 478
e
Certified By:
APPENDIX II
Statement of Authorship and Qualifications
The author of this report is Paul Johnston, l conducted the geological survey starting June 14 and completing on October 24,1994. My mailing address is:
P.O. Box3197 Manitouwadge, Ontario POT 2CO
l hold a B.Se. (honours, (1987) from Carleton University and an a M.Se (Minex, 1990) in geology from Queen's University, l have worked in exploration and mining continuously from 1987.
Ministry ofNorthern Developmentand Mines
Ontario
Report of Work Conducted After Recording Claim
Mining Act
Transaction Number
Personal Information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.
Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for reqi
Recorder.- A separate copy of this form must bs completed- Technical reports and maps must accompany th- A sketch, showing the claims the work is assign
fi.
42C13SW0025 2 16219 WABIKOBA LAKE 900Recorded Holders)
w.Client No.
Telephone No.Address
Po itoC, Gc SU\\., La. BPV T^Vw rtv^VxX V J V\ l""Township/Area ,Mining Division M or Q Plan No.
Dates Work Performed
From: To:Work Performed (Check One Work Group Only)
Work Group
Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized WorK
Assays
Assignment from Reserve
Type
UvxecwVWt ,H^Wt i"*4*! * l^s^wMtof t cocV *P __tofftCp A fafO T^*1
UUi o 4 bib
MINING LANDS RQAMP,,
?
^ocV \ Te-A Su^-oVj
Total Assessment Work Claimed on the Attached Statement of Costs S 37.077-00Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
H.(attach a schedule If necessary)
O JlScatlon of Beneficial Interest * See Note No. 1 on reverse side1 certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.
Date Recorded flwder or Agent (Signature)
/lCertification of Work Report
1 certify that 1 have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report Is true.
Name and Address of Person Certifying
(jLkHtxi ^d cfp PoTelepone No.
, 60 lUivl^ U. .04-, faHDate Certified By (Sinature)
For Office Uso OnlyTotal Value Cr. Recorded bale Recorded Mining Recorder Received Stamp
Deemed Approval Date
Dat Amendments Sent
Date Approved
0241 (03/81)
Ontario
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des mines
Statement of Costs for Assessment Credit
Irtat des couts aux fins du credit devaluation
Mining Act/Lol sur les mines
Transaction No./N" de transaction
(A) W O- It*
- x - w
Personal information collected on this form is obtained under the authority Of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5. telephone (705) 670-7264.
Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lol sur les mines et serviront a tenir d jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministere du Developpement du Nord et des Mines. 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/Gouts directs
Type
Wages Salalres
Contractor'* and Consultant's FeeeDrafts de ('entrepreneur et de I'expert- consell
Supplies Used Fournlture* utlllsess
Equipment Rental Location d* materiel
Description
Labour Main-d'oeuvreField Supervision Supervision sur le terrain
TyDeLCfV^ie^Tn*
5W*i GnWV^
?o*f*4foj| .S-lWw/jcn
Aswm\v^Type f\wivVti'*^r^c*J '*
Typ*
Amount Montant
ii.qit-oojYgo-oi)
5(18 00
IY76-00
lyrt-fie
IT7-W)
Total Direct Costs Total des couts directs
Totals Total global
15,^-00
"ISW-oo
J^oO
53^-flO
2. Indirect Costs/Gouts Indirects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les coCts indirects ne sent pas admissibles en (ant que travaux devaluation.
Type
Transportation Transport
|Food and Lodging Nourrtture et hibergementMobilization and Demobilization Mobilisation et demobilisation
Description
Type
To/Ac v*Ki*.l*..RECEIVED
OCT 0 4 V9S5
FINING LANDS BRANCi
6*~*
Amount Montant
W6.00
-&&00
^foog-cc
Sub Total of Indirect Costs Total partlel des coOts Indirects
Amount Allowable (not greater than 20H of Direct Costa) Montant admissible (n'excedant pas 20 H des coOts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable d'evaluation Indirect coital fTotal dM coOti direct!
Totals Total global
XS*.oo
i oo 6 *oc
3(42*00
Mtfoo
37,07*00tt Indirect* admtolMtt
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulaire enregistrd sera tenu de verifier les defenses demanddes dans le present etat des couts dans les 30 jours suivant une demande d cet effet. Si la verification n'est pas ettectuee, le ministre peut rejeter tout ou une partie des travaux devaluation presentes.
Filing Discounts
1. Work filed within two years of completion is claimed at 10016 of the above Total Value of Assessment Credit.
Remises pour depot
1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 100 "At de la valeur totale susmenttonnee du credit d'evaluation.
2. Work filed three, four or five years after completion is claimed at 50*M) of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimedx 0.50 -
2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement sont rembourses a 50 "M) de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit d'evaluationx 0,50
Evaluation totale demandde
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
that as Ldr^M f i/c./tflhf(Recorded Holder, Agrfnt, Position in Company)
to make this certification
Attestation de I'etat des couts
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
l am authorized Et qu'a litre de je suis autorisd(litulaire enregistre, reprgsentant, posts occupe dans la compagnie)
a faire cotte attestation.
Signature Date
lls, fi ff
Ontario
' Ministry of Northern Development and Mines
Ministere du Developpement du Nord et des mines
Statement of Costs for Assessment Creditlitat des couts aux fins du credit devaluation
Mining Act/Loi sur les mines
Transaction No./N 0 de transaction
B 2Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.
Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lol sur les mines et serviront a tenir 4 jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/Gouts directs
Type
Wages Salalres
Contractor's and Consultant's FeesDrolts de ('entrepreneur et de I'expert- consell
Supplies Used Foumltures utlllsees
Equipment Rental Location de materiel
Description
Labour Main-d'oeuvreField Supervision Supervision sur le terrainTypeLCO/HV^'**
SW*4 Gr^WtVi^
fcfcjf^s , S-'\h?*tJfY\
ASiaV\V^
TyP* i-f\VftiVfi , JCu^V Wi tt
Type
Amount Montan!
ii,qit-ooi Yeo- otf
5/18-00
lflk-00
W 6- W
i*n-w
Total Direct Costs Total des coQts directs
Totals Total global
is,yfc-oo
18W-oo
Wuo
fc,*es-a0
2. Indirect Costs/Couts indirects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en (ant que travaux devaluation.
Type
Transportation Transport
MlFood and Lodging Nourrtture et hebergementMobilization and Demobilization Mobilisation et demobilisation
Description
Type
TfuAt vjeJrxJ
^"7 o.i
RECEIVED
OCT 0 41995
JING LANDS BRANCH
^roC^fft*
Amount Montant
WG-oa
JZ&S-flc
focS-cc
Sub Total of Indirect Costs Total partlel des couts Indirects
Amount Allowable (not greater than 20H of Direct Costa) Montant admissible (n'excedant pas 20 H des couts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and Allowable devaluationInrilrart cartel (Total da* eodt* directs
Totals Total global
;ts*-ooloc&'co
X^^OO
36^-00
fycTT-OOM Indirect* •dmlwlbtet
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulaire enregistr6 sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre pout rejeter tout ou une partie des travaux devaluation presentes.
Filing Discounts
1 . Work filed within two years of completion is claimed at 1000xb of the above Total Value of Assessment Credit.
Remises pour dep6t
1 . Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 100 "to de la valeur totale susmentionnee du credit devaluation.
2. Work filed three, four or five years after completion is claimed at SOW of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
2 . Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 'to de la valeur totale du credit devaluation susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit devaluation Evaluation totale demandee
x 0,50
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
that as Ldrds n[LACiC} f. f ^————^— (Recorded Holder, AgeVit, Position in Company)
Attestation de l'6tat des coOts
J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux devaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
am authorized Et qu'a litre de je suis autorisd(titulaire enregislre, representant, poste occupe dans la compagnie)
to make this certification a faire cette attestation.
Signature
rnttn fnrmuln lor^nu
Date
no doi nersonnes le mascu'in ost utilise au sens neutre.
Stalls for Xcrk l-eoort J AE3ST35.306*i (~? f'~,\p f^ g , \ ,''-" ^-^ ' -•t ' 1 "^
! Kork Report* jClaui Number ' for ADO i ring r'see note ^! | Reserve j
MO ' .033. 33G
! ITS 1. 153.632i i T p t 4 t f e * * : l i b ! . lOC.lt l
i t
!TS !. J BS. 523
l ITS I.J86.E24
l j
i 1 m 4 4 e e r i ri : 1C 1 . !CQ.5iSt 11 1 T p 4 4 rt ^ rt Art1 (1C 1 . 1 C J . i 3 -j l 11 i "fi 4 * i r nr 4 r f1 l Tfl 4 4 rt 1 0 rt rt: is i . icj.^r:
'
i il l Tp 4 * rt* * f T
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'Value of AssesiT:6nt1 ;j . f i. r. . ^ .i t '.'r, i/one
' I.7C2.CC1 ii 2/57. GCi w 4 r * *fll i . l ^ i . 'J Ul
1 -* 5 5?C r;Ti
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I * 2,332,00-
* C , l 5 .' ,U'.'ir n t r t nf
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Iota' Val w *ork Done
V3 iUe ADC'JCJ 1 i f'3 1 uSS ^S5ijn6 ;j i r.sSSrV'SlXork LU LS
ii ; 3 rutiiTB uatS i i i
400.00 ' ! J ' . 3u2.uL' i i i
t i r
** i* L1 1 y u ' i i i . j j ; t j i*1 t i i
t i i
4 0 0 . 0 C ' ! ' : . -; 5 1 . j 0 i i i400,00 ! l ; i . 757.00 t i i40C.OC! ! ' 3.3*6.00 i i i400.00i i i i i i
i i it ** AS, t i i 47 r; ? * *
i l l
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o u L1 . y u i - ' i - w i. ' i 'J u
ft 4 r ^ ^ ft t i iL , : ^ ,( . U U ! ; :
i i 'i i t1 i i1 T l
1 1 1
1 ' t
1 1 1
i ! RECEIVFDr i i
i j OCT 0;4 iyyji i i
i i MINING LANJDSRRai^
l 1 '
t i ii i i i i ii t i i i it i i
1 ! i i i
1 l i: : i i i ii i T
j i i t i ii t i i i : t i ii i iII
i t il 1 !r i f
7, i3 6. 00 ! ! *00.00 ' *3. 33 ; .00 i i iT.4..1 t(-1 ^ T^t-1 1....— .' T^i.l n.-*-...:ui*ai faiue tui.3 1 ftsa j yncL fuiat ^esrrvr U--J. j^^i."-w r. KM• Or.', n uut i 6u ri j!i
Credits you a r e claiming in this reoort may be cut back. In oraer to iiiiniiiiize the adverse affects of Such deletions. please indicate froif which claus you wish to Driorize the deletion of credits. Please *ark 'xi one of the following;
i. l ! Creuits are to be Cut back eauallv over all cla^nis contained in this recort of rrork.
scis as priorized on the attatcned auoendix.
.'x! Credits are to be Gut back starting with the claims that nave reserve credits.n the event that you have not specif ;ed /our choice of Dnority. ootio.n one will be isoleifented.
of aareeiiients. etc.:te I: cxano ; es of beneficial Interest are unrecorded transfers, option aayiients.with resoect to the aining clams.
ste 2: If "Ork has been oerfortied on oatented or leased land, ulease complete the following::erufy that the recorded holder had a beneficial interest in 'Signature e oatented or leased land at the tiire the work was cerforseu. l
OntarioMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines
October 05, 1995
Geoscience Approvals Office Ramsey Lake Rd 6th Floor
sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.16219 Transaction #: W9540.00118
Mining RecorderMinistry of Northern Development St Mines435 James Street SouthSuite B003Thunder Bay, OntarioP7E 6E3
Dear Mr. Weirmeir:
RE: APPROVAL OF GEOLOGY SL GEOPHYSICAL ASSESSMENT WORK SUBMITTED ON MINING CLAIMS 1099990 et al. IN WABIKOBA LAKE AREA
An administrative error resulted in this work report not being assessed prior to the 90 day deemed approval date. Accordingly, as outlined in subsection 6(5) of the Mining Act Regulations, this Report of Work is deemed approved as of July 19, 1995.
If you have any questions regarding this correspondence please contact Steven Beneteau at (705) 670-5855.
Yours sincerely
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
SBB/sb
cc: Resident GeologistThunder Bay, Ontario
Assessment Files Office Sudbury, Ontario
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PRECAMBRIANPROTEROZOICMAFIC JNTRUSIVC DIKES
13adtabase eft*
ARCHEAN
LATE FELSIC INTRUSIVE* Ue. aplite 12b pegmatite
GNCISSK COMPLEX MTRUSIONS
lib granite gneiss Ile poragnras lldnaflc gneiss
10 l FELSIC PLUTONIC ROCKS10* gronodnnt* (it Cedar Lake Pluton) lObnonionrt* (i* Gowan Lake Pluton)
MAFIC PLUTONIC ROCKS 9a gabbro
MAFIC IIKES•a c*ont* dfa* ft lamprophyre•s xenoUth-bearing lamprophyre
7 l FELSIC BIKES1 ——— ' 7a quartz-feldspar porphyry dfc*
7b feldspar porphyry dfc*7c Irregular feldspar porphyry CM* (popcorn porphyry) 7d
FELSIC INTRUSIVE STOCKSta quartz-fvldcptr porphyry ftock•b ftw graMrd quartt-fvldspar porphyry itockftd hydrothtrml br*caa rtlattd to QfP stock
9 CLASTIC SEDDCNTARY ROCKS 1 ——— ' 5* cebM* congUMwrat*
9b pvbbt* conglorwrat*Se pvbblv-bmring, (andctonc and pebble conglontrat* 5d pvfaolc-bmrtne (andcton* 5* p*bbl*-b*aring landcton* and cttstont Sf sandstoiwSg fm* landston* and iHtcton* 3h fiM lanctoton* and ironstont 3n fUtcton* and gray siltston* 3p pelitic sltftone and pelitic sandstone
OCMKM. K0MNTARY NOCKS
ch*rt vulphMto ran formtnn 4* bar rt*-rich
INTERMEDIATE VOLCANIC ROCKS 3a massive 3b pyroclastic ash 3c pyroclastic lapilli 3d pyroclastic bombs
FELSIC VOLCANIC ROCKS Ea massive Eb pyroclastic ash EC pyroclastic lapilli 2c pyroclastic bombs
MAFIC NETA-VOLCANIC ROCKSla massive flocle amygdaloidal flo*If tuffIp pillowed flo*Is ultramafic rio*It tuff breccia
caoTM grow* or Men*
5409000 N 5409000 N
Peutopir erystai knmg u^Xum ne-i* clift reMtane clast
540805408000 N
Geologist
Hemlo Gold Mines Inc.
eutcnp
(^ clan poet
SULPHUR. CTC
4X Mhytrft*au (OWb* karitecpO* sol*"* o*
py•pM telluride*
Fowler lHenlo North East
Sheet lFeb. 6, 1 995
P.Johnston
#.16219
42C13SW0025 2 16219 WABIKOBA LAKE 210
PRECAMBRIANPROTEROZOIC
NAFIC INTRUSIVE HIKES
LATE rCLStC INTRUSIVE* Uta aplite Ifibpeomtite
11 l GNEISSIC COMPLEX INTRUSIONS Ue. uneubdlvMee) lib granite gnrln llcparagnetss lid naf le
10 l FELSIC PLUTONIC DOCKS10* granodiorite O* Odor Lato Pluton) 1MB nanzanrte Of Gowan Lake Pluton)
MAFIC PLUTONIC MOCKS 9o gab* g
FELSIC DIKES7a quarts-feldspar porphyry dike7b feldspar porphyry dfce7c IrrvQUar fdetepar porphyry Mum (popcorn porphyry)7d
FELSIC INTMJSIVC STOCKSi* quarti-fHd*por porphyry itocUM fm* grained quartz-ftldcpar porphyry itockCd hydpothvrfial breccia related to OFP (tack
CLASTIC SEDIMENTARY ROCKS Sa cobbl* conQlan*ra~tv 5b
p**0*t fceoi M( wuMlrtone M
gray Mtrtoneend pelfttc sondeton*
4 l CHEMICAL SCDIMENTAKY ROCKS 4a chert4to cherty wltitone 4c chert-nagnetlte Iron f or ra-t ion 4d chert eulphMe iron fornation 4e barite-rich icdinent
INTERMEDIATE VOLCANIC ROCKS 3o nanuvt 3D pyroclastic ash 3c pyroclastic lapilli 3d pyroclastic bonbs5W09000 N
FELSIC VOLCANIC ROCKSna*Mve
2b pyroclastic ash 2c pyroclastic lapilli 2c pyroclastic toonbl
11968
Fowler lHenlo North rast5408000 N5408000 N
SheetDatei
Geologist
Feb. 6, 1995
P,Johnston
.16219
Hemlo Gold Mines Inc
42C13SW0025 2 16219 WABIKOBA LAKE
PRECAMBRIAN mOTCROZOIC
l* l MAFIC
tt l LAIC FCLSIC MTMISIVCS Hoop*** Ukpognattto
ONCBSK COMPLEX MnUSIONS IUUkgroMto UcptrogMttf
FELSIC PLUTONIC MCKSM* gr**Mttrit* Ot Codw Lok. Pluton)
(it GOMII Ukt Pluton)
MAFIC PLUTONIC MCKS K
7k fWtatw porphyry *k*7c Irpvgutor fcM^Mr porphyry *k* (popcorn porphyry)
MTMJSIVt STOCKS qu*rte-f*l*a*r porphyry itach
•b fko froMd ^uw*i-* tWvpw porphyry siaeh M hyJroihti "nol hrocaa rtt*-tod to OTr ctock
CLASTIC SODCNTAtV ROCKS So eokkto confltOMrat* 9k ppkM* conglOMratv Se M9o pikkli NaU^ •andstan* and dtctam 9f ,...
landrtoM and Mtctont 3h fit* landrtow and ronctont
Mtvtont and gray Mltci.ont Sp pvlrtic sttston* and pelitic sandfton*
MTOMtMATC VOUCMRC ROCKS3*3k pyroctarttcle pyrocUrtac UpMiM pyroctostic bc***
rCLSIC VOLCANIC ROCKS C*
pyrocUtttc avh •c pyroclactic le pyroclastic koNu
l l MAFIC WTA-VOLCAMC ROCKSla naiMv* flowle •nygdaloiitel ria*If tuffIp pMoxd flo*t* ultranafic flo*It tuff hr.caa
5407000 N 5407000 N
FowlerHenlo North East
c
Sheet 3\ \^.Datei
Geologist
Feb. 6, 1995
P,Johnston
Hemlo Gold Mines Inc
42C13SW0025 2 16219 WABIKOBA UAKE 230
RES 0.
IP
12.
oj n.
r- t - T— r - T T - i - T i - T ~'T ' i ' i " T - i -1 - r t i r ~ \ ~ r" T - T ' i - i ~r ~ rIP
.-25RES
.0
CHARGEABILITY mV/V
81+00 N 82+00 N 8,5+00 N 84+flO N^,. ^ , ( ,- f * t * -f--,, —f — .---t--*-55 55 62 51 71 75 II l
85+00 N 86+00 N-*- f- * -*- - 1 t— *II 10 12 II
87+00 N -*--t *M li
88+00 N 89+00 N 90+00 N 91+00 N 9^+00 N 9J+00 N 94+00 N* -i -* - -f- - * —f * t * - 1-- *— — f- *- f * - t— *- f * — f — -*. -f -,- -j. — r - t - ,,18 21 22 tl 17 15 14 M 13 i 51 4 32 2!
11=10=2
0 = 1 n=4
0=5
n-6
5, 5 57
58 55 I.S 71 79 t 7 l 4 , ^-
6 t 7 ^ 12 X 7 5 l6? 54, 71 55\
2,^ . 3 J ( ,. \ H f .1^ , l j 1^-. l l 1-^ *J
" "^ J? X" " l 3 \ " \ V ' 3 ^ 5 ' V ' * \\ ' W ^ 5,' 2 J( f? \X 11 |3 \ 4 l x x 7 i \\ -2 3 '"-52\ \ x ' \\\'^x \x
15 \ 17 \ N 10 13 A\ 2 7 \ \ 7 4 ^ , -6 i
37
APPARENTRESISISTIVITY
ohm-m
81+OON—— -t-* 82+00 N- t--.
83+00 Nt-.-*
i*89+00 N
rt90+00 N
rt91+OON84+00 N 85+00 N 86+00 N 87+00 N 88+00 N 89+00 N 90+00 N 91+OON 92+00 N 9J+00 N 94+00 N
-*- .-l-*--f t -l- *-f-* t * t . * - * - t - t - i t i . t ^ j- . t , i *- j . (-*--t *-^-, t * -i- *
15K 14K 15K 14K 14K UK 14K 14X l SK 14X IK 4411 1121 1022 137 (tt 1375 7744 15K UK 20K 20K 22K UK Itt UK UK I22J
0=1 I2K 1922 — 1677 9412 — 7101 -^ I2K 9167 16K 17K 15K\ ? "N "\ //"^
0=2 IIK UK I4K 1550 ( IIK MSS V. 14K __ |4K ( 24K \ 15K
l SK —— I5K ~ " 15K M02 I5K 7947 . l 19K __. UK X-- 21K0=3
0=4
0=5
0=6
(23 . — . . — — 214 - ^ 126 - - - (U ^ v v 15K 19K -9277 IK 14K -^ UK- I4X - 2JK - 1701 _ . 10K"—^1U —— 154 120* l ( 209
22K -\ 17K 17K\ IIK 15K N 9)19\ N \^24K \ 17K 20K \ 10K \ 1IK IIK
X /' \A \25K ^ 20K ~" m ^ 1 2K
15K
UK
M///1U —— 154 120*//y//// y - i11K /S 1 502 — . m' 1 525 l"// ~~ S
1507 — 1201
2JK UK 20K ^ I6K l 2 IK \ UK
2IK\
3IK 12K ' 24K 21KN ' \
\- 1W l OK , __ UK\\ ^ r^\\20Kj s 7747v. .
. V UK ' UK \ 3JK \ 1IK ~ - IOK 6420 ^ 16Kl,' N \|/ x^ V i \\ VNX . \ Xx \ v '. ~2403 ~- 1152 l 2422 J 49S --. 700 x 171 V, 100 x^ 1111 V 5615 \ 18K 35K - 16K N " 10K^^\ ~ l Jll((r,\ \\\] \ \\V\\ N\v\ v \\ v -.
22K - IU7 ^ IIK * 1615 2111 ~ 205J " 1079 s 2SO "- 731 x 1 11 — - 114 x 2105 S212 x 19K v V5K - - 14K ~ - 22K ~~- UK I8K
r-12K N1 N \ 25K ^ 4151
Lo
CHARGEABILITY mV/V
APPARENT RESISISTIVITY
ohm-mn-1
0 = 4
niter*
* ** * *
* * * * * * * * *
Dipole-Dipole Arrayna
J±L
Vplot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS : n = 6 WINDOW :CHARGEABILITYInterval 27., 1 05SRESISTIVITYLogarithmic 1, 1.5, 2, 3, 5, 7.5, 10,
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMITTER : PHOENIX IPH-B
Scale 1:500050 O 50 1 00 150•ass
(maters)
FOWLER 2INDUCED POLARISATION
LINE 17 40 O EDate : DEC. 1994 Property : 530 NTS : 42 D/9 Survey by : NOREX
hemlo oldMines Inc. -*J
7 l 6 2 l 9
42C13SW0025 2 1B218 Vw5lKOBALAKE240
RES 0.
IP23.
OJ II.
0.
r- t - r - T - r - i - r ' l ' i i T - t i ' l T i i i i - l - i - i -T— i - i - i - i i -
CHARGEABILITY mV/V
APPARENTRESISISTIVITY
ohm-m
42C13SW002S 2 16210 WABIKOBA LAKE 250
91+OON 92+00 N,--T -i T- -. - . ( .- - t - *-
(4 4.t 44 it 5
II, 3.5 ^ M J J- .7
X
.L--J ,-4-—l———l— l -J -i —L- J- . l . j _l L-O--l ..i ,0-, 4... I.. J., l . j . t . 4 . j.
IP .2J
KES.0
-11
.o Lo
9J+00 Nt
94+00 N^ ( i 95+00 N , 'S* 0?!*.^ i 97+00 N 10 75 li 10 21 II 11 l 5
98+00 N '9+00 N t J02+OON ^ JOJ+OON ^ . 104+00 N 105+00 N
'5 M ( * i'l ' 5*1 ' i'l ^ s'l ' 5^7 * S*7 t 3CHARGEABILITY
mV/V
0=2 0=3
41 57 7?
SI 5? ((- 4? --J Jn
4i M' 4 J 4 1 J
27 J 7 31 31 H 4 4 k 3 l ^ - 4 l l 4 41
.- -l 1 '"'
p
M iS l l - l t I 75 (5J i l -l J
- — \ -i ' f \ , f — ~-\ \ x \ '4 J 3 * J 9 J.7 33 \^ 47 ^ 3^7 5J- '51 43/71 || p }| f i i J\ | jN -, 4 ^74 j j ^57 5 j
51 ^ 3 7 4 I 31 "4 1 3 * l 41 ' '4 l 3 9 r "Tl 3 34 " 3 9 ^ 4 9 5 3 S l '' ~ 1 7 I.I |0 11/1 \ Vs \ l 5 " - J l vx ~ i 3 (( v 53
n -l
^ .
2 * 31 4 l V~- 4' 43 31 51 39 4 l /3 3 23 21 ' 5 l 4 ! ' -' 10 ^ II 17 I.J l l ' '" l l \ 7 l'' 57^ 19- ) l ^ "n 17
91+OON t— ~t- .—4421 (710
H^^ 92+00 N^ - ^ 93+00 1^
H35 (107 Till 1291
94*00 N—t -iO 51*4
95+00 N, —— 4- — t- .
SI34 WOI
96+00 N-^ ^ ——
417} 5151
97+00 N 98+00 N ^ ^99+00 N 100+00 N 10HOON
(til 7191 744(
U4i 7113
11=2
5110
4417 /^\tLv 7 v, \H)0 . HiS WU
Ml? OH
5IJJ ^\
^
^ U5J
1533 JII5 - l(i; ^- M10 2U4^ J511 __ 4041 x UU
UH ^- U01 tllJ J2I4 "~ 3511 3(75/^(441 ^ 4j.ll - 5180
4017 30H 4IU 4104 HIS ^' Mil l
J570
DU
10K UK 1)07
-^ 3511
7BS" ^ 1 3K .
n=6
Sill 70IJ 52W
5oi M]]5057 7(17
\M20 - TIM
\NX , - ^. ' S V m ~^C- 4 741 4435 . 4711 (110 5515 (007 5J05 ,' )170
NX\ S" l Nil 1010 . I4K \ U,M DU 1(10 lil l 7001 5513 7511 MM
15K J 57(1
nn
5111
(514
41(1
}55*
102+00 N* 4 *-
3554 3934
lOJ+00 N ^ 104+00 N Ml) 7116 1340 1343
au
^105+00 N TKI mi 7114
5MI
APPARENTRESISISTIVITY
ohm~m
(731
53M (4(1
\ \1154 IKO |W MU N (130 ' 1400 ' 1113 ^
r/I0)| ' 1IK
i*
17K
l^/}
5113
5105 4107
(343 5111
7UI S345 UU
^ 1H4 1511 -- Z5I7 ^ 411) . 5133X ) l M l \ \ S ~~^
3I3( ' 10(4 \ 41(7 2441 v 4310 7750 tU7 i \ \ \ ^ \\ V. -v, \ ///--N \ i l H7I IMI \ 1729 1740 "i 5570 f m \ 1042
^ " -^ -\ v-^ 7'l l J \ x,4144 4113 \ 1490 37M J741 l 1 2K ~~ - I4K I53(
1011 [ 7142^ 3915 \ 1500 \ 4741' . 1511 till, |5K Mil
sin "-^ inn \ iiu '
.\
Ul((110 Ull ilk7013 7015
IMS
5777 5115 "^ 4014 ^ (715 till \4K
0=2 n-3 n-4 n^-5 0=6
2 . i 6 2 1 9 .
Dipole-Dipole Array
* * * * * * *
* * * * * * * * * * \
na
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :CHARGEABILITYInterval 27., 10 J!RESISTIVITYLogarithmic 1. 1.5, 2, 3. 5, 7.5, 10...
INSTRUMENTSRECEIVER : BRGM ELREC-6 TRANSMITTER : PHOENIX IPT-1B
Scale 1:500050 O 50 _ 100 150
(meters)
NORTH LIMBINDUCED POLARISATION
LINE 14200EDate : NOVEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo oldMints Inc. *
RES 0.
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
IP 18.
\
l 0.) 9 l
l
l
oj o.
-T i'1'T i t i i i i i '"i t ~ i i ' r f i i i r - i i i ~ i - T ' r * r r ~ i ' r ' i i i ' r' i - T
L. i. i.. i. i i i- i i-i * - J t J-i.i i
IF 1r-18
l J - l . t . J , l J i l . i-.-l-.-t .-J . i l . l J . J . J .J - 1-- i - l l l . i . J l ]
Rt S n
-a Lo
42C13SWQQ26 2 16218 WABIKOBA LAKE 260
o Lo
91*OONr- f — * -* - -*
71 21 31
W+00 N t ^ 94*00 ^
41 47 t l M
95*00 N
J l
. 96*fO(l N l i t 4 7
97*00 N 98*00 N ( ^ a*flfl N
2 4 31 j 2 j l
0=2
r= Ii
0=6
., v - - -v- - -~~" " "— "— -55 ' M Z l - ~~ 2 4 ^^ J 7 J I 27
5 ! \ l 5
3 l
4 'l 24 J J 33 37 27 2 C
41 51 f J K 11
41 41 43 41
14 II
102*00 N f 1 ! 4 * J 9
44 53 4 l - - 4 S l X /li 81 ty' U \// U - " l* ) \ i l 41 i J l
3 l
J 7
CHARGEABILITY mV/V
Jl ' 47
/' P--*!
*'/ l' t l'/sn/'rt^M I I \ 11 ! }l ir
, ^ ~/ //\-' /, \ \ ^ ~ \ 'S 4 - , t l 45 \ 3 l 71 35 J 9 21 21 3 X \ \ ,. 7 \\ J' 4 ( f l 4 II - r/ j'l s \\ 1 5 ^\ ' l l It N 4 t f? t 4/ f/// L~ X' \ x x y \ \ i
i l 43 45 3 S 32 4 34 2 l 2 J 31 35 l i ' \1 , il t l ' f 70 /. 1 4 15 14 x I l ^ i l M v - to
j 4 J*- 41 4 5 -- J 5 J 7 l? 71 34 J H M -" 7 l l i 14 )4 H 14 ' 7 t 51 41
9I*OON 92*00 N* - * * - * t 4 *7151 1034 7111 MO]
HN 14*00 N 15*00 N 96*00 N 17*00 N 98*00 N 98*00 N
. t - t 4 ' t r t-t-l t t * l * - t *-l * f-* f tt t
4717 4'70 4773 4001 4477 4113 5147 (71k 1237 1371 }77i 7l7fc *OOI) 4211 3310 7521 150J
100*00 N JOUOON *00 N
!447 1105
n=lr i
tOK 7215
W35 1W x 433J 7071 -, IH7 1115 17/3 1141 - 1375 - 250* 3491 4713 ^ M47 — (113 7lM (Ml , 2lH 2171 U4| , l?2( , 535* 1140 2(17 Uti V \ \ s s~ - - - --' - ' ' , ^~~-^ ^ . ~ . r ~ / /; ' \ v.r ^ \l Ilk 11K l IMS, 7730 — 2M3 \ 1441 ^ JJOi 2444 -- 3514 4541,,. 5033 7MI ^ U K x Ml JI23 -.5510 - 37J5 1S*4 " 14(* M t, , 5717 ! 100 T - J2H
S527 J1I7 -' 55J5 1 -- 4ISC _ 471! 304* , !I72 211?' 5433 5JI* 5511 fill ' IW , I2K\ ' 5WI 3161' IW ^ JJI4 (^Wl t, 3IM 4315 , 2271 ^ H3 s 4*i
APPARENT
RESISISTIVITY ohm-m
I53t S527 1117
*77J 7537 / 3 705 l 7152 ~ I5J7 4111 .. 4711 - J403 5705 7501 (004 1114
7MS' s 'au 5010 j lOK " 1447 (411 ' 4773 ,, 4413 7i7l) M l . 7055
n=G
14K MM (521 - 55J7 . 4122 ,' 1704 -; 7104 J1H y !029 21*9 '/l ' ^ \ s ~
/ Mti 50IU l ID* IM7 Mil f in , . 44IJ W/D fli/ . 7055 / ' 3d IIK ___ IOK (541 (491 3317 ' U52 - ' 3 4(3 l 2314 , 1105 ' 7500 4721f ,'' \ *O ^ -. . -^ ~ . " ' V ^ f - , l ,' - - '' ,---. \ /, -. ' ,'
3147 4911 7054 H 27 D M 1111 (111 547* 7437 MJ ' 14K IOK 7351 - 71M ' IM5 ' 4001 ' 1 5(2 ' S411 - 3414 1109 2103 ' 44f7
llfll ^ 571
- 2I2"0
2271 ^ M3 s ' 4*71
15I\ n-4
niterDipole-Dipole Arroy
* * ** * * *
* * * * t* * * c * *
plot point
DIPOLE LENGTH : a^50 DIPOLE SPACINGS 10 = 6 WINDOW :
CHARGEABILITYInterval 2 7., 1 0/ZRESISTIVITYLogarithmic 1. 1.5. 2 , 3 . 5, 7.5. 10,
INSTRUMENTSRECEIVER : BRGM ELREC-6 TRANSMITTER : PHOENIX IPT-1B
Scale 1:500050 O 50 100 150
SSSSiiii(maters)
NORTH LIMBINDUCED POLARISATION
LINE 14400EDate : NOVEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo goldMinal Inc. v*J
RES0.,
IP
11.
OJ Oj
- i - i - i - v -i - t - i - t ~ i ' i ~ T" T
/
"\
\
_\—-
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
42C13SW0025 2 16219 WABIKOBA LAKE 270
0=111=2 0=3 0=4 0=5 0=6
89+OOJI. ^ 90+00 N ( ^JI+00 N ( , 92+00 N ^ ^ 9J+00 N5 53 i 5 51 5 ( 53 51 31 5
4 C v^ 41 (1-31 4 1 4^5 5 2 4 l 41
51 43 57 31 54
7 5 3 , - 5 5 61
4 t
55
x - 5 j 6 1 l 5 l 53
73 l 3 -51 5 t
5 3 fi e '13
89+00 N ( 90+00 N ( ^91 tOO N
IS* 22K 70K 17K 11k '5k
92+00 N 9.1+00 N4 * t r f- - -t
k 1311 U5I
0=1
0=4
UK Ilk . - 5514 ^ 154 ^ 4412 -- 7247
I4K ~/ m )]l, 1IU -^'lUI —"l
UK '.S. 6014 - I lk ~~17K
V - - 13R s I?K ;, ' A \ l II 1
. 5412
2411
\ 3002 ~ 57U \\ \ \4971 ' f 40K "^ 27K ZOK I3K ' V H7
1 7 /- - x. l x //i32K f 60K Ilk ' UK 7 4 102
\ V \ l ,' /'(4K UK - 13K ' ' 4(13
IP RESi - T -i -1—1~ r" T—r -T —r T - r - t - i - i—i —r— r ~ r - i -i -
94+00 N 95+00 N
94+00 N 95+00 N
Lo LO
96+00 N ^ .J7 *00 N ( ,98+OON 41 4 5 5 l 71 II
44 J 3 i 41 1 J i
4 - '[4 ' J l 55
45' J
99+00 N 100+00 N 101+00 N 102+00 N 103+00 NU II 10 17 li 63 43 J 2 21 11 32
10 13 ,,.,. 2*
10 , li/// U .,- 20 \ "li V
II 11it / i3' , i3 ,y j ii f . ////, f
10 21 2 t j 11 32
-10 l 5 x i 7 2 * 3 t
- 10 13 14^ 4 J\ x r\\31 s 4 7 ,' /S |J V/ 20 - x'li ^ l' II ^ 14 N\- 21 -10 l 2 l 37' , y 7 XX V / . \ \ \ \\x\\\\ (
73' 13 f . I I s , I I J |7 X li li 13 ^\^ 2 l . 17 -27
17 ' 11 ' ' 17 " - U ^ 17 li ^ II * 17 NI ' "l3 \ - - 3 ' O
0 = 2
0=1
0 = 4
0=5
0=6
H*96*00 N 97tOON 98+00 N 99+00 N 100+00 N lOUOON 102+00 N 10J+00 N
73lt UK 14K UK I1K 0(7 J)JJ J5IO 2S4b 3525 4114 4594 5041 5410 5101
21K i I4U . 2711 14014117 i 1 143 , ' OK — 1451' , s - ' n ' ~ v iM45 , Ilk )tk - 10K l(k J 4 310 4114 l
l , ,- \ - ^ - \ l iMOl l W ' Z K UK 5111 \ 4205 HIO/x -X x x \ , i ' j\-
12k (UK I5K 7 5SI7 S104 2144 IH4 . 2141v ' /ir' f - - 'ITK 14k ^ 7717 4727 27)7
1101
2141 1165i" S.
1442 441J v '
1125 UI7
-^ 1617 / '
M4I
121
6*08
- 21)4
3712
5J07
4134 2!|7\ v -
~ 500J M2J
7015 , ll'l 1104 b004 6401' -^, ,' l ,' ; \f\\\till 7M5 J413 ' 24t4 7141 4313 2565 1174 ^ 7204 f20S
)U2^ -, 11(1
5419 '-f 1 5k- -__s
1IK - 14K
UK
n-1
r-5
ri-6
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
Dipole-Dipole Array
* ** *
* * *
no
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :CHARGEABILITYInterval 27., 107.RESISTIVITYLogarithmic 1, 1.5, 2, 3, 5, 7.5. 10
INSTRUMENTSRECEIVER : BRGM ELREC-6 TRANSMITTER : PHOENIX IPT-1B
Scale 1:5000SO O 50 1 00 150
assHfiiii(maters)
NORTH LIMBINDUCED POLARISATION
LINE 14600EDate : DECEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo ooidInc. ^J
RF.S O,
CHARGEABILITY
APPARENT
RESISISTIVITY ohm-m
IP 40
oj nj
l' 1 l ~ T - i r i ' i - i r - r ' r ' i - r ~ t ' i T ~ t i r - i - T t - t - r - r i - T
9J+00 N 94+00 N* i * t -* J. l
Dipole-Dipole Array
20 [.O
l t l
i Lo
n-10 = 2 0=3
0 = 4 n--5 0=6
v^f.f] EiIN ( ^ 96+00 N t f 97+00 N f ^ 18+00 N
' ' l * 24 li 15 2i 2 1
5 2
4 7
13 J' M n " " 56 99 K 24 l! 15 2, 2*
i d~~ * 7 ^^--^ 4 ^ 52 41 51 -41^89" |^r^,\,V.: /, j , )\|\V\ 'M ,l ^ \ S '/'I \ Stl'-r^ f -'x -X V 7 n *i? "/r 5 J - 5 —'/' V/-'ffi}M " 55 j j "--*- *- ^' i. '{/4fa)'fv'//''*".-y " '"/'v //' ytfWw'W -
J ' X *' J* -41' M /l J 6 5^5 '-^V//^///^ n^
HlUOON *-~ t t
psi
n-2
n-3
0=4
(1=5
0=6
7291
57/2
l IK92+00 N 9J+OON 94+00 N 95+00 N
^ . -f . i-^-i-. t ^ ^ ^ -t12K UK UK m 1(K Hk 17K
96tOO N
1517 — 67JI^ \\
I\K\ 7MI 1 V \ ^m "^ i n — - -
5354, - III! 7514 MJ4
ITIi J^Xti'O ^X UK
--. "K
1175 -''241^ ^ 12K
m iwI* f ZJK
I5K ^ 1JK
m ,15K
'V y/'iw y
15k
IJK-
97tOON
1597j 98+00 N
StCI 3716
/'^7x' '/wy//
iixx/ X - IOK4457
UK
J1K
/VX /^/'rf' &S S s*~ \K'fe^ r 5MJ
' 1161 -^ IOK 77M
6502
n^^
0=4
n-S
0=6
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
DIPOLE LENGTH . M- -u DIPOLE SPACINGS : n * 6 WINDOW :
CHARGEABILITYInterval 2 7., 107.RESISTIVITYLogarithmic l, 1.5. 2. 3, 5, 7.5. 10...
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMIHER : PHOENIX IPT1-B
Scale 1:500050 O 50 100 150
(maters)
FOWLER GRIDINDUCED POLARISATION
LINE 1520 OEDate : NOVEMBER 1994 Property : FOWLER NTS : 42-D/9 Survey by : NOREX
hemlo goldMln*t Inc. *J
RES IP
OJ 1G.
OJ 0.
-r - r T i
y-. A . a --L - i .-i- —j. _i .-a-. 4-4.. j.j.i.. j-i-i-j. --J—
IP RES- 12 n
-1G LO
-0 l.n
CHARGEABILITY mVA
APPARENTRESISISTIVITY
ohm-m
0=1
0 = 2
r-1
0 = 4 0=5
p-6
n^2
0=1
0=6
9J+00 N 94tOO N J l 45 54 t 5 II
95+00 N 96+00 N 97+00 H *^t.i*(**.t-*U li M l* 21 29
CHARGEABILITY mV/V
l 17 45 41 5 5 x ' l? - v H x- - 2? -x x H -x / /i )///1 ;i(^-4 '^43 41 4 7 J 1 ,1!, 7 2l X/' " -<~\ .. .. ' l ^ ''''//i k '' x X"'.'.
J 41 41 l ' id , ,x (, /'/41 41 7 t ~ 15 s////v'
4 1 ' 71 1 . ,/ 11x ///'/L.74 7 4 ' x H - '-
-. li, - - -,
28 'x 3o'-' x
' 23 ^^- 10;14 /, 2: V ' M//'/7;
13 v 21 V ID)///'" ' ,; ' 20 ' ' !l n-G
9JtOO N
1554 1140
94t()0 N* * *ilk UK
9"itOO N 96+00 N "7,on N K D5H iSf 2927 Jt2t 2141
APPARENTRESISISTIVITY
ohm-mr nk UK
MIS \ 1104 ^ Uk 14K IOK __ Ilk IJK ' /' !4IO ZIOJ 1MI\ ! /' -155J ( I5K I7K Uk IJ 1* X W *' j
~ S .'' i'Mi ' J OK 15K Ilk UK 2177 52)1 249?
\ ' ! , x x ! i '13,11 N UK L Uk Itk X Z527 - *5IJ 40J2 X l ; J,', !ilOb - Ilk PK ' JOI5 -- *MI 3701
r- 4
n-6
Rlter*
f *Dipole-Dipole Array
no
* * * ** * * * *
* * * * * *
4 9 A
^plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :CHARGEABILITYInterval 27., 105JRESISTIVITYLogarithmic 1, 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMIHER : PHOENIX IPT1-B
Scale 1:500050 O SO 100 150ssssss,
(meters)
0219
FOWLERINDUCED POLARISATION
LINE 1540 OEDate : NOVEMBER 1994 Property : 529 NTS : 42 D/9 Survey by : NOREX
h em l o goldMlnci Inc. ^J
42C13SW0025 2 1 6219 WABIKOBA LAKE
11R1?
HI
1swoo
RES IP
1 J .
\
oj 14.
1
J .
oj o.
fNII A Q f^C A Q| I IT^l'w^l^^^u^^^DILI 1 T
mv/v Jn-1 2 0=2
0=0
0=4
0=5
0=6
APPARENT
ohm-m0=1 1
ri— A
iiiiuuiiHnnniiiIIIIIIIIIIIIIIll2fi 2 1821(1 WABIKOBA l AKP
X'
/ /
^ — -^
93+00 N^
1 41 51 7
7 3.1 34 ^5
n j /^v41 / l
II ''
i __ ^ 93+00 N
J2I I4JI 1341 10
721 i till 4215 IJ
5114 f'llOI V. (ji7
UN Cui^ — H
(201 1 1iK \\ V "IUJ \ li VN
.^-^ S
V — - — ^*^^
^ v^^~-- ———
94tOQ N ^ 95+00 N ^ 96tOO N ^ ^ 97*00 N
1 1 l f l li I -."' S J^ ~ — | ' 'III V — /" -^ -"- ~ ~ ~
3 x/ (5 is 1 5 My/ 1' _ - 29V 15 ^12 — U x^ li /"'"li
U v
94tOO N 95+00 N 96+00 N 97+00 N
K Ilk 110} 571! 1114 J7b1 7-JJI 271
0 13K 12K i '265 1124 x 4^" KOH "'J t ' i \ l \\\c-1* I1K till / 3U! U02 l i304 \ bOf
1 / / y \ ^ . x K UK lilt x 3111 1145 1IC4 4CUy 7 7 x , - \
11K 11K// 3HI — 27M J1I7 2250
li \ 11K " 4211 3727 3012 " ' 2541
15K 1 'ttll 4421 J72? ' 2474
IP RES29 0
. l
1
.14 Lo
. i
.0 Lo
z:CHARGEABILITY
mV/V
o-3
0=4
0=6
APPARENT , RESISISTMTY
ohrn-m0=1
P3 ^
0=6
niter n . ,* Dipole-Dipole Array
* * .a no a* t * i ——— i ——————— i ——— ,
* * * * r~®~i r~®~~i ***** i l l l
plot point
DIPOLE LENGTH : 0=50DIPOLE SPACINGS : n - 6 ^^ - u/iMnnw ' ^BF lWIINUUVV . F* A M
CHARGEABILITY Interval 27., 10% RESISTIVITY Logarithmic 1, 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMIHER : PHOENIX IPT1-B
Scale 1:5000SO O SO 100 150
(meters)
FOWLER 1INDUCED POLARISATION
LINE 15500EDate : NOVEMBER 1994 Property : 529 NTS : 42 D/9 Survey by : NOREX
hemlo aold1 1 ^B^ 1 i i 1 ^Mk7 ^B^J *^ m ^*FV
Ulnei Inc. **S
.6219
RES IP 0.. 29-.
J .
0. 15.
oj n.
CHARGEABILITY mV/V
0=1
0=3
0=4
0=5
APPARENTRESISISTIVITY i
ohm-m
0=2
0=4
0=5
0=6
. . . . ———— . ———— . ———————————— ———————————————————
r- -i -p i - i - T i i - i - r i - i i i ft T ' i " i i i i ' T ^ T - i
__ 1
91+OON 92+00 N 9J+OON 94+00 N 95+00 N 96+00 N 97+00 N5 I t 1 5 41 15 15 10 14 22 26 23 21 li 11
6 ^ -28 jy. 56 JJT" 6*W"I " Ty * 5 ' -~ , 7 JX-","//! \2/'/ 20 -^\"x v v-9 ' "
4 3 ^ 1 l' 26 51 75/54 y ,'f 1 4 'l j V 26 ~-— 25~ j * 11 - ,: 21
1 2 ^ x 5 2 S 7 1 l 4 4 //f (SyY/'u ~7 22^ ~^ l* -~ " x"^ M
47' 12 ' 4 - ' 12 ' ' - U 24 ''•iP^'^l '''16
————————————— ——————— ——— ———————
IP RtN-29 .0
1
1
-15 Lo
. l
.o In
CHARGEABILITY mV/V
0=2
0=3
0=4
0=5
0=6
APPARENTJM+OON ^ j 92+00 N t , 93+00 N ^ . 94+00 N ^ 95+OC IN ^ ^ 96+M N ( ^ 97+00 N
117 UK 1617 1421 1041 141.3 6311 4114 1126 1711 1711 1141 1110 4011 RESISISTIVITY
ohm-m471 - ItK 6124 5)l( 1191 - 6025 4260 X - 7075 3121 , / 642 f 771 ' ,. 2055 - 7611 6717 o= 1
1242 —— 10K 6311 ( 444S -"1052 7764 ^4516^ 5207 J 1 102 - — W / '2320 1 123 N\ 3611 1^ = 2
SIM llOK \ 5744 S W. ~~~ IM1 6723 \ 1220 ^ 1 613 ~" lUO — 2013 ^ 1071 ~ 1241 0=3\ ——— \ \ \ l /V-X /V^-N \ l'^^ 6323 \ 9004 -"" UK 1IK 1761 4771 144J 7 2205 ' 3515 l i 754 1439 0=4
^ 7 ^-. / li \^/ / / //Y /5161 , 17K \v 13K Ml! , 6013 2745 ^ 2001 1 4041 f 1 116 — 1011 0=5
\ \ \ J / / / - __ y //X9187 ItK \ UK 6117 ' 2123 ' 3691 1911 " 1210 1560 0=6
niter * Dipole-Dipole Array
* * a na at * t t * - -i — — i
***** 1 1 1 1
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS : n - 6 WINDOW :
CHARGEABILITY X * l ft 2 1 G Interval 2%, 1 CT^ w "^ * v RESISTIVITY Logarithmic 1, 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMITTER : PHOENIX IPT1-B
Scale 1:500050 0 50 100 ISO
FOWLER 1INDUCED POLARISATION
LINE 15600EDate : NOVEMBER 1994 Property : 529 NTS : 42 D/9 Survey by : NOREX
hemlo goldMints Inc. ^
l
42C13SW0025 2 16219 WABIKOBA LAKE 310
1HII
- ————————————
RES IP
0 1 "l
l
1
nJ 38.
l 1oj oj
CHARGEABILITYmV/V
n-^1 i
0 = 2 0=1
0=4
o--5
n-6
APPARENTRESISISTIVITY ,
ohm-m0 = 1 5
0=2
0=3
0 = 4 0=5
0=6 .
•li Hill i nw mn mn inn nw inn mi nw m inn mi iniinniiiiiin
- - i - T - i - i - i i i T r - r - i i - i - r - i ' i
/ ~~~-~ ^^
/ "^
\X
^X
\ __ L __ I——I — 1 __ 1 — i -J _ J. __ l __ 1 _ J _ J _ 1 - -J —— J. —— t
CIZ9H-OON 92M10 N 9J+00 It 94+00 N
f 41 J 5 49 i 'j t 11 It l
1,, 10- -1 -30 J 1 - -J.7 lV *-ll —— 19 i - a\ , , ~ - .- ~ ~~~ ' | \V ^--—-^sg
J 9 ,-' 7- , S J 41 55 7i x H 13 - -xV, \ f ) ,
3.1 - ^ t 5 V 5 1 M ' II X , P ' ' 15 ,- 1 )
s \ - f s ' /' , j C37 \ 6 3j * 7 i 4 X 10 x , 7 15 H J- ' 7 s/ ' ' /A45 si - -i? X*' /7 " ; " ,'V/ " ; -X' x ' , /^ x//
J 3 '71-^11 '15 - ^ ^ - - l\
VV *^. . ..1w ^ 1
9UOON 9/t-OON IJt-OON 94+00 Nb!5 Ilk 12K UK )I2^ 1171 7325 Slfl ?7
144 v 14K - — UK 1IK 10K UOi . I7J2 1307 - il.
^ ;' \ S " ^ /' -1251 ' Uk I?K . H(3 J12! lj*0 1134 -1 ?5U .\ f —— '//,'
UK - ISK 9501 1411 10K UK /' 3013 15!
V ^ //^' v-J472 I3K \ (lil IOK l*/ ' 454i . 1340 \ ^^^ /, ,' ^ ( , 7IJ* x Uk Ilk 13k /, 4il3 3710 | 14\ y// 1 1 1
7197 INC — |3K S 4630 53it ?IOJ
' 1 ' T - 1 ' T I ' T 1 T'r - -
f
-^^ ^-^^
__ L _ J _ -l- _ L^4-, J-- l-, i —l -j
95tOO N 96fOO N 9 7 tOO N
M 4i V) 4i (1
O 2 } 55^ " ^^ 'l ^5 Z3~^i 32Vn - — ' i' ,' 14 24 23 , - 25
/' 2? 2! - ""li ) , H
L - 2 ' ( 21 ,. 'X24
21 " li ;s
95+00 N 96+00 N 17+On N
10 1(21 1705 1116 3507 457
1 , 1541 v U94 , 1317 4247 -- 4{5/' ,' ~ " - - ' x : i r197B 1 J?2 — ~ IH2 J574 J7i3
s l , \ l l l 1C - 1147 MO ) ?041 ^ 45*2^ ^-' J l \ 1
S5I 119 ^^ 1400 r 11711 , ^ f ^ l
C v (7t f 1 H2 - 2232\ ^ J 1 ( JJ7 — 1347 ' 2504
IP kESr 75 r 0 lr
-38 Lo
1rLo Ln
CHARGEABILITYmV/V
n-i
0 = 2
0-^
0 = 4
r^
n-6
APPARENT, RESISISTIVITY
ohm-mi n -l
0=2
0=3
0=4
0 = 5
0=6
Rter* Dipole Dipole Array
* * a na a* * * i ——— i ——————— i ——— ,
.V.V. 1^1 r*l
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS : n * 6WINDOW : t r* O r CHARGEABILITY .ft A 1 fi M 1 IInterval 27.. 1 0*^ -^^e^^^ft-J-RESISTIVITYLogarithmic 1, 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMITTER : PHOENIX IPT1-B
Scale 1:500050 0- SO 100 150
(meters)
FOWLER 1INDUCED POLARISATION
LINE 15 800 EDate : NOVEMBER 1994 Property : 529 NTS : 42 D/9 Survey by : NOREX
hemlo ooidMines Inc. ^S
42C13SWQ025 2 16219 WABIKOBA LAKE 320
RES IP O, 74^
37.
nj OJ
T - T ~ r~ T— i ~ r - i— T T ' r - T - T T " T - r-- ^l— 1— T
CHARGEABILITY
APPARENTRESISISTIVITY
ohm-m
5 5
4 i
89*00 N-* * * * *-
S.I i 1 i J i J S
90+00 N—— * -t - *- - -l
S 7 S 7
55.
t 9W)OI^t l i
^ 93+00 N ( ^ 94+00 N H li 14 15
95+00 N-t*
W 2*
-l——l——l— U,
96*00 N——^ , ^ .
a i ?
IP RES -^74 n
l-"
l l lLo
n* 3
n-6
\
42 i l 57 l 58 51
i 4 7 51 54
f l 11 x 4 J J ' 55
7 4 v 42 SI 47 5 .' 79 -i 7tSI 41 5
7 -—l I \ ' l
* 7
44/71 57 14
4 i J l - 4 S --' 7 2 -51-^15
11 -IB/15 ' '' 2J
90+00 N 91+nON 92+00 N 93*00 N 94+00 N 95+00 N 96rf)0 N*-'t * t * t *-t-. t r -*-. 1 . *-.-** t * ^ *-t . 1 . t . 4 * t . t * t *
UK 12K UK IK 15* I4K l* IJK UK 117* UK 7JC] 51(2 JII5 1H3 2411 JD|2 J170 U77
, J004 4|J7 - M5J - 5SJII - (166 4HI
4B4I - 4M5 l 1 44! x - ^Wll WTI 1971
l tJlS 2JN~ - ,-1\ ~ y\4088 , )I)(U i 15U 1878 ^ 12*5
I4K 14K U7J ' *JI8 7JO* ' '|BM "~ 1910 ^ 1744 , 112'*, . . ^ .' / , //r \ r" . \14K x UK ' 7IK IlK S tM ' I 4K 1JK JflOI ' t'Jl UJB JJ85 ^ 1177 J251 1'7k
HJ7 1506 IJK - IJK IlK UK IlK I5K
42C13SW0025 2 16218 WABIKOBA L^tE
CHARGEABILITY mV/v
" n-2
r--fi
APPARENTRESISISTIVITY
ohm-m
n=J
ri^4
n-5
330
niter t
* ** * *
* * * ** * * *
Dipole-Dipole Arraynq
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS : n = 6 WINDOW ;
CHARGEABILITYInterval 2K, W7.RESISTIVITYLogarithmic 1, 1.5, 2. 3, 5, 7.5. 10.
INSTRUMENTS RECEIVER : BRGM IP-6 TRANSMITTER : PHOENIX IPTl-B
Scale 1:500050 O 50 100 150—————~
(meters)
9
FOWLER 1INDUCED POLARISATION
LINE 16000EDate : NOVEMBER 1994 Property : 529 NTS : 42 D/9 Survey by : NOREX
hemlo goldUlnci Inc. ^S
RES O,
oJ
oJ
IP28 r -T- T~ T i ' T -r- i —r- i" T - t" T— -i ~- r - T T-|— r--r-i t --i "r —f- i— i — |— T - r ~i — r r -r -T — r- T- T - T--I
IP28
RES ..O
Lo
CHARGEABILITY
APPARENTRESISISTIVITY
ohm-m
0=4 0=5 0=6
0=2 0=3 0=4 0=5 0=6
81+00 N 82+00 N 83+00 Ni — -f--*— -f—*- ^ -* — 4 ~ *- 4 - --*-
45 M J 4 J l tt 4.4
7 S x I.I
I
84+00 N* -H- -t- -4— *-
S 4 7 b 4
85+00 N 86+00 N^ *- - 4 * — -4- *~
87+00 N- 4 - -*
88+00 N-4- - — 89+00 N
--- 4- -* 4
4 l 44 44 49 41 51 7 J 12
90+00 N.-f-* t
13 II II li II
91+OON 92+00 N 93+00 N-l--. t- - t — 4- *- 4- —— *- 4 -,
21 21
94+00 N* 4--*-
23 21
95+00 Nt j ,
24 21
96+00 N 97+00 N 98+00 N- ,.. -, ^ 4 - *- 4---* 4 *- t -*
li U 12 74 7 J 11
I.I i 12 ,- — J 9 43 43 41 4 5 s^x |0 ^^- 4 l _ -^2 l 45 4 1 , J ( J.) li 4 ! 5,! i , 12 - — ) 1 -^ H x f ^' L 1 - v, " V " U-^ \ ' - ~~ " ) 2I l l \ M V 2J Li0 ' " \\\M 5 ' " - 6 V 1 7
I --23 41 41 47 51 i) 41 4 4 ' (iH ) 42 S! 4 27 l 1 . --" 4 7 5 l ' , i ] ,' 15 //IT' J j 13 Z— |5 \ II \^ 2? ^\ 7.7" x II l l 2( V 10 \\\ 27 2I\ \ lYv\ s l f 'Tt 4 3 KV - vny ; 7 ^^ ..y l i /,'///// -^~- O\ \ ^ v x, ' V\ — J\\ x s \\\\\V ^ l
3.1 J.* \j(7'- Jl 47 57 52 4? 41 41 47 4.3/ J2 li/ M 1.2 73 ' ^\J ! f V -^ \i ^- 1\ ^ l i 11 \ X ^23 J 2 1 /' 2 4 X 21 2 ? y \" P \\U\V* 7 54 XI4
33 j l 27 l * 7 5 55 41 4 l --. 4 7 5 i f J l 32^,1 77 74 /^ X|1 ' ( ( 17 ^ ' "|5 '//'to ) 20 V. |7 J 20 2? ^ .x 25 24 25 25 \ \ 2" H l \ I2X ^\"* 3 5 4~ " ~—
3 4 * 47 53 J l 47 31 31 15 11 3 4 ' - 7 4 71 ' l l- -
H " 10 ' ' - 1 1 21 ' 74 ~~ 24
0=2
0=3 0=4
0-5
0=6
81+00 N 82+00 N 83+00 Nf ——— 4 - -* —f— — t- -t —— -r 4 -- * * —4- -*- 4
2I2J 174f 4421 1441 1417 UK Ilk
^ \ /2114 M23 4111 \ HOO H24, \
53S1 ~~ W7I 1131 \ 7215 11K\
SIOI \ 4241 H40\ i5141 4310 s 1515 \ IIK^ \\
4MI 1737 1011 - IIK
,\ fIOK fl i v
515 \ IIK\
h——— W ^ ——————— l l ————— *
84+00 N 85+00 N 86+00 N 87+00 N 88+00 N 89+00 N 90+00 N 91+OON 92+00 N 93+00 N 94+00 N 95+00 N 96+00 N 97+00 N 98+00 N*- 4 - -^- -4- .--4-*--4 — *-* *~ — 4 -*- I-* 4--^-*- —— * - + - --*- 4 *- - 4 — -*- — 4 -* -4-*---4---*- t * t -* H---*--! -.--4 * * *--4---* 4 * 4- * 4- *-4---. * * 4— *---4 * 4- -*
K Ilk t SK 1SK 1W 15K 15K I5K 1172 14K 11K I3K II ID 1411 4.151 1114 Illl l III 1134 4141 1121 1251 Ilil UK l Hi I7K 7JK 1IK 1W 71K 17
31 ^- l OK I3K 17*3 1151 — NI4 IOK ^ I W / . 3M4 3754 v . 401 ^ - 1115 2073 x 1572 1011 . 1471 .- 2271 , 171 141 ,v - 5727 i 12K 10K \ Illl v . 13K 17K — liK , 12K , 1 5K 14K ,- 21K x Ill* ~ ^~^//^ }1"S ——— ^ ' '-* N \\ / li ~ (: f v ^ l YU \ l l -- \ \ l i l ,/ f. J M 7/ -
1* ^ 1 5K 12K I1K l* W y IK J l 4742 1171 4251 ^ W4I ' 3121 ^^2115 \ 1772 - 2711 2514 ' J M7 711 J 1 114 \ 1117 I5K Illl - 7111 \ IIK IW IK 25K l l I2K l l 2IK 2*s i /— v, -^ 'v/ L ^ /^±r^ ^\ K- —--x //x J^mVx\ v ; - , \ -' v- '1K ' 1 7K l 1 1K I4K ' IIK IIK '^ 25K s - ' 1071 5127 3143 ' M *JM M97 1117 ~ 2111 3M5 . 152 1010 1351 2175 - 1121 . I2K N 1151 -S 1 2K 14K , - 1W V 21K ' 17K - 2IK 27K
Rt ^ 1 121 - 2751 v 745J 71JI 1131 ^- l OK I3K 17*3 1151 — NI4 IOK ^ I W / . 3M4 3754 v . 401^^ ' \ /' * ~ ^~^^ "S
17K 14K 14K ' I7K-"-
///
1SK ^^ IWiIW IW
^K / / Ot /, SII2/ (s A// J
17K 17K -' IOK S, 7421 5110 "y ///y )15K ' IOK - 7lll 7111 ' H5I
1411 ^ 3177 ^ MK-
32K 30K
4JK V III! r~ U\ \\-\\\ .si r -",.
2IK v JIK , Y MM 1304 140v. .) U \v\\\ ^ f22K 23K sXs 1143 1101
--x2111 3M5 /. 152 1010 1351
\ l if L. S / - 'lM97 ) 1117 ~
\1071 1375
IM?-. 'fIlll ^ 1215 ' 1152-
. --' \ X~ .^\ s^
2101 27M - 7)41 ^ IIK 1* f 1221^~, \ x \ \ o J~
^^1221 ( l 3W ^ IIK' -
14K l 2 7K 1IK~, ~1114 2114 1414 . l* l IOK 1W ~ - 17K -' IIK ' 20K 24K\ ^ ', . ^
2045 -- |M2 |7JI 1155 2111 2151 ' 1521 12K - 17K 12K IIK -" IW 17K
0 = 2
0=3
0=4
0=5
0=6
CHARGEABILITY mV/V
APPARENTRESISISTIVITY
ohm-m
niter*
* ** * *
* * * * * * * * *
Dipole-Dipole Arrayna
J±L
Vplot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :
8.162:LCHARGEABILITYInterval 27., 1 05!RESISTIVITYLogarithmic 1, 1.5, 2. 3, 5. 7.5. 10...
INSTRUMENTSRECEIVER : BRGM 1P-6 TRANSMITTER : PHOENIX IPT1-B
Scale 1:500050 O SO 100 150
FOWLER ZINDUCED POLARISATION
LINE 16600EDate : DEC. 1994 Property : 530 NTS : 42-D/9 Survey by : NOREX
hemlo goldiji - i^ ^ mMlntt Inc. ^f
42C13SW002S 2 16219 WABIKOBA LAKE 340
OO (Oo
z o oNt-
o
o oCM O
o o o o
o o00m
o oIDen
o o "*O)
o o(NJCD
Oo oO)
o o oo00
o8oo
o o"t00
ooCM 00
o o o00
14200E 14400E 14600E 14800E 15000E 15200E 15400E 15600E 15800E 16000E 16200E 16400E 16600E 16800E 17000E 17200E 17400E
H
H
H
H
H
H
H
lH
H
TB1196847
a
o
TB1166525
a
H
TB1196846
TB1183292H
TB1166521
TB1163592
TB1166523
TB1183291
TB1196845
TB1166526
TB1166524
H
H .
Resistivity Low'
H
H
H
'
1 l L
14600E 14800E 15000E 1f5200E 15400E 15600E 1 5800E 16000E 16200E 16400E 16600E 1 6800E 17000E 17200E 17400E
00 OOo z
NORTH LIMB/ FOWLER 1 fc2INDUCED POLARIZATION SURVEY
InterpretationProject |: 505, 529, 530; NTS: 42-D/9
Instrument: BRGM IP-6 Rx , Phoenix IPTt 2 . 5 kW Tx Operators: Noranda Exploration
Date: 7 February, 1995
HEMLO GOLD MINES, INC,——————— - ———————————————————————————————————————— - — - ———————— —r? ——— — —— : —— -J
o en o o
o ^ o o
oM Oo i!
o o o o •z.
CO 00oo
'DmC )o
00-f* o o
00 N) O O
N
High Chargeability ——t-Mod. Chargeability -XL--..J]—
100Scale 1:5000100 200 300 400
^.16219
42C138W0025 2 18219 WABIKOBA LAKE 350
LJ O O 00 CNI
LJ O O Om
LJo oCM
LJ O O
LJ O O CD
LJ O O 00
o oo
LJ CoCN
LJ O O
LJ O O CD
LJ O O OC3
LJ O OoLO
LJ O'O CM LO
LJ O O
LO
LJ O O CDLO
LJ O O 00LO
LJ O OoCD
O Oo 1CL
LJ O O
CD
LJ OO CD' CD
OouCD
LJ O Oo
\
1200N
11000N
N
-i r \ pi T; \ i' '^uu,\
10800
10600N
\
<
10400N-)
10200N
10000N
9800N-
9600N-
9400N-
9200N
9000N-
8800N-
8600N-
8400N-
8200N-
- 10800N
- 10600N
- 10400N
-10200N
-10000N
TBl166521 TB1166526
9800N
9600N
-9400N
r; TBl166523
TBl166524
--9200N
-9000N
LJ O O 00 CN
LU O O O
LJ O O C\In
LJo o
LJ O O CD
LJ O O O
LJ O O CM
LJ O O
LJ O O CO
LJ O O 00
LJ O O OLO
8800N
8600N
8400N 1621 9
8200N
OO
LJ O O
in
LJo oCD LO
LJ O O 00 LO
LJ O O O CD
LJ O O CM CD
LJ O O
CD
oCD CD
LJ O O 00 CD
LJ O O O
mmm"C13SW0025 2.1621
360
Instrument : SCINTREX MP-3Profile Scale SOOnT/cm
Reduced Profile Scale SOOOnT/cmProfile Base Value 400
Datum : 58000
Scale 1:500050 O 50 100 150 200^ -w
(meters)
NORTH LIMB/FOWLER 1&2MAGNETIC SURVEY
TOTALPROJECT : N UMB.FOW1&2 NUMBER : 505,529,530
BASELINE AZIMUTH : 90 deg
DATE : NOVEMBER/1994 NTS : 42-D-9 SURVEY BY : NOREX
FILE : M529FOWM
hemlo ooidMines Inc. - S
UJoO 03 OJ
1 1200N-
11 DOON- ; :
10800N
10600N- :;
10400N- -
10200N- - i
10000N- *
9800N-
9600N-
9400N-
9200N-
9000N
8800N-
8600N
8400N-
8200N-
4-
LU O O 00 (N
42C13SWQ025 Z16219 WABIKOBA LAKE
LJ O O O
Ld O O CN rO
LJ O O
ro
LJo oCOro
LJ OoCOro
LJ O O O
UJooC\J
LJ O O
LJ O O CO
LJ O O 00
LJ O OoLO
CN LO
LJ O O
LO
LJ O OCO LO
LJ O O 00LO
LJ O O O CO
LJ O O CN CO
LJ O O
CO
LJ O O CO CO
LJ O O00 CO
LJ O O O
M- 1 1200N
- 1 1000N
-10800N
10600N
-10400N
-10200N
-10000N
-9800NTB1166526
-9600N
-9400N
TBll66524
-9200N
-9000N
!: -8800N
8600N
-8400N
: -8200N
LU O O O
LJLJ O O CM
LJ O O
LJ O O CO ro
370
Instrument : SCINTREX MP-3Contour Intervals : 50 nT
Datum : 58000
Scale 1:500050 O 50 100 150 200
9^5S! (meters)
NORTH LIMB/FOWLER 1&2MAGNETIC SURVEY
TOTALPROJECT : N LIMB, FOW142 NUMBER : 505,529,530
BASELINE AZIMUTH : 90 deg
DATE : NOVEMBER/1994 NTS : 42-D-9 SURVEY BY : NOREX
RLE : M529FOWM
hemlo aoldIfineslnc. *
5408650 N
00 CO OJ01 om
RENCH 156E4-16219
U
vi) ID
03 CO•^ o om
5408650 N
5408600 N
f
9400 N
Clalh Post 3114 m at 100 degrees
elm 1166522
oo
Oom
cln 1183292 i 5408550 h
Trench 156 E
LEGEND
SAMPLE LDCATIDN
FT-4-14 SAMPLE NUMBER
DUTCRDP
-- - CUT GRID LINE
42C13SW002S 2.16219 WABIKOBA LAKE
cln 11642411164420Clain Post 2170 n at 87 degree
cln 1166525 .162195409000 N 5409000 N
FT-3-9FT-3-10
FT-3-11FT-3-12FT-3-13
FT-3-14 T-3-15 T-3-16 T-3-17
LEGEND
SAMPLE LDCATIDN
SAMPLE NUMBERBL9800 FT-4-14
DUTCRDP
CUT GRID LINES
5408950 N CLAIM POST
metres
FT-3-52 FT-3-53 FT-3-545408900 N 5408900 NFT-3-55 FT-3-56 FT-3-57
Trench 150 E
42C13SW0025 2.16219 WABIKOBA LAKE
LEGEND elm 1166522Claim Post l194m at 337 degrees
SAMPLE LDCATIDN
SAMPLE NUMBER
DUTCRDP
CUT GRID LINES
metres
f F T-4-f 5 FT-4-Z6
FT-4-27 FT-4-TRENC
2*162199600 N
Trench 153 EPI* k* K KuM* (M* Mw K/IO DM.
42C13SW002S 2.16219 WABIKOBA LAKE 400