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GM 47780GEOLOGICAL AND GEOCHEMICAL REPORT, LEOPARD LAKE PROJECT
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1,6
GEOLOGICAL AND GEOCHEMICAL
REPORT
ON
THE LEOPARD LAKE PROJECT
QUEBEC
FOR
TOURNIGAN MINING EXPLORATIONS LTD.
by
G.H. Giroux, P.Eng.
Montgomery Consultants Ltd.
September 25, 1987
Ministàre de tinergle et des Ressources Service de la GéoInformation
Data l FEV 1989 No G.L.: 47780
TABLE OF CONTENTS
1.0 SUMMARY AND CONCLUSIONS 1
2.0 INTRODUCTION 2
3.0 LOCATION AND ACCESS 3 —
4.0 CLAIM INFORMATION 5
5.0 HISTORY 7
6.0 GEOLOGY 8
7.0 ROCK GEOCHEMISTRY AND MINERALIZATION 11
8.0 COST STATEMENT 17
9.0 BIBLIOGRAPHY 18
10.0 CERTIFICATE 19
FIGURES
1. Location Map 4 2. Claim Map 6 3. Regional Geology Map 9 4. Detailed Geology and Sample Location Map Pocket
APPENDICES
I. Trench Sample Locations and Geology II. Drill Logs and Sections (1956) III. Rock Geochemistry Results
20 21 22
1
1.0 SUMMARY AND CONCLUSIONS
1.1 Tournigan Mining Explorations Ltd. holds title to 20 mineral
claims between Leopard and Erikson Lakes in Northern Quebec.
-
1.2 The claims can be reached by helicopter or float plant some 40
air miles west of Kuujjuag (Fort Chimo).
1.3 The claims were explored for copper-nickel by Holannah Mines
Ltd. from 1954-56. Exploration on the property consisted of geologic —
mapping, a magnetometer survey, excavating 14 trenches and drilling 2185
feet of diamond drilling.
1.4 The property is underlain by Pre-Cambrian metavolcanics and
metasediments that have been intruded by a metagabbro grading to a quartz
diorite. These rocks form part of the Labrador Synclinal Trough.
1.5 During July 1987 a program of rock geochemical sampling was
completed to test the trenches and surrounding rocks for concentrations of,
platinum group elements.
1.6 A total of 76 rock samples were taken and analyzed for As, Co,
Cu, Ni, Zn, Cr, Au, Pt and Pd.
1.7 While the leopard rock unit is certainly anomalous in platinum-
-
palladium the concentrations are not sufficient to warrant a drill program
at this time.
1.8 The program cost $15,779.42 and was completed by August 31,
1987.
2
2.0 INTRODUCTION
This report was written for Tournigan Mining Explorations Ltd. of
Vancouver, B.C. on the Leopard Lake Prospect in Northern Quebec. The
report details the geological mapping and rock geochemistry completed on
the property from July 12 to July 20, 1987.
Tournigan holds title to 20 mineral claims straddling Longitude
69°30' in cantons 5845 and 5846. The claims cover a belt of Leopard Rock
within a gabbro unit which forms part of the Pre-cambrian Labrador Trough.
The property contains known copper-nickel mineralization
extensively mapped and sampled in 1955 by Holannah Mines Ltd. The
purpose of this exploration program was to determine if the property
-- contained economic platinum group element concentrations.
3
3.0 LOCATION AND ACCESS
The Leopard Lake claims are located about 40 air miles (64 km) west
of Kuujjuag (formerly Ft. Chimo) Quebec, between Leopard and Erikson
— Lakes (see Figure 1). The property straddles the boundary Cantons 5845
and 5846 and is bounded by the coordinates.
69°27' - 69°32' East
57°47' - 57°50' North
—
The claims can be reached by float plane or helicopter from Kuujjaug.
Kuujjaug, the Inuit name for Ft. Chimo, was established as a trading post by
-- Hudson Bay in 1842. During World War II an airstrip was built to service
Trans Atlantic flights. Canadian Airlines now provides daily jet service — from Montreal.
The town of Kuujjaug with an estimated population of 1,500 has
hospital, postal, banking and police service with one main motel.
Should results warrant it, a road could be constructed from Kuujjaug
along the north bank of the Koksoak river, a distance of approximately 50
(81 km) miles along sand and gravel ridges.
4
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yta'~a• 4a . \ , t H9
F LGURE 1
TJJ\ LG72,1\. V IN I\G -XP LEOPPRD LPKE PROJECT 14 87TM2
LC 2̀T I0\ V2 - 9CRLE 1: 1HHaHBDlo.
0 200. 400. 000- BOO. KM.
MONTGOMERY CONSULTANTS LIMITED SEPTEMBER 2S, 1987
--
5
4.0 CLAIM INFORMATION
Tournigan Mining Explorations Ltd. holds title to 20 mineral claims in
the Leopard Lake area (see Figure 2). The claims are recorded in the
office of the Chief Mining Recorder at Quebec City. The pertinant claim
information is reported below:
Canton (township)
Claim NumL ers Staked by
5845 459615 1-5 J.C. Turner
5845 459616 1-5 J.C. Turner
5845 & 5846 459617 1-5 J.C. Turner
5846 459618 1-5 J.C. Turner
OWN
•
69°30' -
55°00' •.
1 • rooti•:.•.
'1/42 3 ~h°'~\ '
• •4
1
2 3 4 .76
,
O 3 4
N.TS.24F/13E/14W
CANTON 5845
•
CANTON 5846
FIGURE 2
T2URNL--\ "LNLN EXP. LEUPPRD LPKE
EL ----Iv v p
PROJECT # 87TM2
SCALE 1: 30000_
0 1000. 20HH_ 9000_ 43130_ M.
MONTGOMERY CONSULTANTS LIMITED SEPTEMBER 2S. 1987
7
5.0 HISTORY
The first report on mineralization in this area is by A.P. Low of the
Geological Service of Canada. He examined the Koksoak River watershed
in 1893 (1895). The Cyril Knight Prospecting Syndicate worked on mineral
showings in the area during 1930-31. In 1945 Frobisher Ltd. prospected
--
the vicinity around Gerido Lake. During the mid 1950's numerous mining
companies had staked claims in the Thevenet-Gerido Lakes area and were
conducting exploration programs, presumably looking for massive sulphide
base metal deposits.
It was during this period that Holannah Mines Ltd. explored the
Leopard Lake claim area. During the period 1954-56, they mapped the
property geology at a scale of 1"-200', completed a magnetometer survey,
dug and sampled 14 trenches and completed several small diamond drill
contracts. In 1955 they drilled a total of 811 feet on trenches whose
total cumulative length was about 700 feet. In addition they drilled a
further 153 feet on 5 exploration holes (E.W. Elberty, 1955). In 1956
field season Holannah drilled an additional 3 holes with a total footage of
1221 feet (W.T. Elberty, 1956). All samples from trenches and drill holes
were assayed for copper and nickel. The sampling plans for the trenches
are included as Appendix I and the cross sections and logs showing 1956
drilling are included as Appendix II.
The regional geology south of the 58th parallel was mapped for the
G.S.C. by W. F. Fahrig in 1953. R. Bergeron and P. Sauve worked in the
Gerido-Thevenet-Leopard Lake areas for the Quebec department of
Natural Resources during the period 1954 to 1960. J. Dugas produced a
special paper on metallic mineral ocurrences in the Labrador Trough in
1970.
The property was examined by D.W. Tully in 1981 for Conwest
Exploration Ltd. but no work was completed.
IPMIO 8
SNOW
6.0 GEOLOGY
The Leopard Lake claims are underlain by Pre-Cambrian
metavolcanics and sediments intruded by a metagabbro grading to a quartz
diorite. These rock units are part of the Labrador Synclinal Trough (see
Figure 3). A tentative geological timetable is reproduced from Tully
(1981).
FORMATION DESCRIPTION/EVENT
AGE
Sand; gravel y glacial debris and muskeg
unconsolidated Quaternary
Sulphide mineralization and oxides
Metagabbro grading to phases of quartz diorite
Metavolcanics and Metasediments of the Kaniapiskau group of rocks
Basement Complex
(Erosional Unconformity)
pyrite, pyrrhotite, chalcopyrite, pentlandite magnetite, minor galena & sphalerite
(Tectonic Activity-folding shearing, faulting with metamorphism)
Variety of basic PreCambrian intrusives known as "Blotchy" gabbro often metamorphosed ampholitic phases.
(Tectonic Activity)
Metamorphosed basic lavas, PreCambrian fragmental phases, conglomerate and shale.
(folding and related tetonic activity)
Granite and granitoid rocks PreCambrian
PreCambrian?
The mineralized zone consists of a belt of Leopard rock within a
metagabbro unit that stretches about two miles long and varies in width
9
Pa rogneiss
LEGEND
Gabbro ( includes sum course basalt) '
Shale,slote,orgalite,siit-stone and graywocke
E DURE 3
TCU\L LEOPPRD LAKE PROJECT tt 871M2
2Baaae_
MONTGOMERY CONSULTPNTS LIMITED SEPTEMBER 2S. 1987
10
from 30 to over 100 feet wide (see Figure 4).
Elberty (1955) completed some petrographic work on the Leopard
— rock and describes it as follows:
"There are three, or possibly four, leopard rock facies; a light greenish-white variety; a dense, gray, silicified facies; a dark-grayish-blue type; and a gabbroic type. The rock is characterized by lenticular porphyroblasts of epidote (clinozoisite) of varying abundance, which range in size from less than .5 x .5 inches to more than 7 x 8 inches. The porphyroblasts are oriented for the most part with their short axis normal to the plane of schistosity. Interstices between the porphyroblasts are filled by ferromagnesian minerals, predominantly chlorite and amphibole. The origin of the Leopard rock is not known. A chemical analysis of an eight inch piece of core from diamond drill hole 3 was made by the author. If the silica content has not changed, the analysis best compares with that of an alkali gabbro. If the leopard rock has been silicified the rock was originally an ultramafic."
Sulphide mineralization is not continuous over the entire belt, but
instead appears to be associated with the most intensely deformed parts.
The sulphides observed, in order of importance, are pyrrhotite-
pentlandite, chalcopyrite and pyrite. A study of the mineralization by
Elberty (1955) concludes:
"Mineralization has progressed along fractures and shears in leopard rock, first replacing ferromagnesium minerals and then the entire rock. Copper, nickel and pyrrhotite mineralization do not appear to have any obvious relationships with the exception that chalcopyrite is later than, and more or less independent from, pyrrhotite. Although the entire leopard rock zone contains disseminated sulphides, concentrations occur only in the more intensely deformed and altered portions of the rock."
11
7.0 ROCK GEOCHEMISTRY AND MINERALIZATION
-- The purpose of this program was to determine if the mineralized zone
contained sufficient enrichment in the platinum group elements to warrant
further exploration. With this goal in mind the existing trenches and
outcrops of the main rock types along the entire belt were representitively
sampled. The trenches were sampled as shown in Appenidix I by taking
more or less uniform chips about every 6 inches across the distances shown.
Outcrops were sampled by representative chips from several locations.
The locations of all samples were flagged and the sample numbers written on
aluminum tags. Figure 4 shows the locations of all rock samples taken
outside of the trenches.
The results for the more important elements are summarized in Table
1.
12
TABLE 1:
SAMPLE
RESULTS OF ROCK
TRENCH ROCK TYPE
GEOCHEMISTRY
WIDTH Cu (%)
IN TRENCHES
Ni Au
(X) (ppb) Pt
(ppb) Pd
(ppb)
18459 1 Leopard 10 ft. .159 .10 48 57 124 18460 1 Leopard 21 ft. .694 .123 34 45 166 18461 2 Leopard 25 ft. .285 .070 31 71 119 18462 2 Leopard 21 ft. .196 .053 3 53 92 18463 2 Leopard 12 ft. .131 .051 2 7 79 18464 3 Leopard 25 ft. .302 .079 8 31 96 18465 3 Leopard 13 ft. .285 .093 33 19 78 18466 3 Gabbro 5 ft. .039 .014 2 14 8 18467 3 Leopard 20 ft. .184 .157 2 1 83 18468 3A Leopard 32 ft. .431 .145 1 12 101 18469 3B Leopard 23 ft. .135 .044 3 9 40 18470 3B Leopard 21 ft. .268 .079 6 15 72 18471 3B Leopard 20 ft. .448 .093 2 1 46 18472 4 Leopard 16 ft. .069 .021 1 6 1 18473 4 Leopard 16 ft. .215 .052 57 1 49 18474 4 Leopard 17 ft. .810 .094 27 31 169 18475 4 Leopard 18 ft. .436 .136 30 47 139 18476 5 Leopard 29 ft. .065 .026 1 1 1 18477 6 Leopard 28 ft. .508 .082 28 56 105 18478 6 Leopard 14 ft. .430 .070 8 11 60 18479 6 Gabbro 23 ft. .154 .039 2 3 14 18482 7 Leopard 15 ft. .220 .059 7 7 20 18483 7 Leopard 17 ft. .419 .094 10 28 53 18484 7 Leopard 9 ft. .480 .109 48 52 138 18485 8 Leopard 21 ft. .134 .061 2 2 37 18486 8 Leopard 14 ft. .176 .049 2 30 18 18490 9 Leopard 19 ft. .383 .027 14 22 35 18491 9 Leopard 22 ft. .412 .080 2 5 51 18492 9 Leopard 21 ft. .067 .024 7 10 16 18493 10 Leopard 21 ft. .254 .056 25 12 18 18494 10 Leopard 31 ft. .349 .142 9 19 89 18495 11 Leopard 21 ft. .482 .070 23 24 129 18496 11 Leopard 14 ft. .292 .107 10 1 51 18497 12 Leopard 21 ft. .081 .026 9 1 10 18498 12 Leopard 8 ft. .040 .020 24 1 11
Simple statistics were compiled on the 51 samples from leopard rock
and the 21 samples from the adjoining gabbro. The results are summarized
in Tables 2-5. Clearly the copper cobalt, nickel, chromium, gold, platinum
and palladium are enriched in the leopard rock with mean values for each
far exceeding background in the gabbro. There is also an excellent
correlation between copper, cobalt, nickel, chromium and palladium in the
Leopard Rock. In addition platinum and palladium are well correlated.
13 TABLE 2
LEOPARD RECK
I S RL-E BT t r I B1 I GB
LEOPARD LAKE
B
- 1 Element Unit n Mean Median Standard Lowest Highest Coef. 1 Deviation Value Value of Var. 1
_ 1 1 AS ppril 51 24.5 27.0 12.3 1.0 52.0 .50 1 CO ppm 51 44.2 44.0 26.8 10.0 137.0 .61 1 CU % 51 .201 .140 .198 .003 .810 .99
- 1 NI I 51 .052 .052 .045 . 00 1 .157 . 88 I ZN ppm 51 92.6 63.0 66.5 27.0 408.0 .72 I CR ppm 51 212.4 181.0 145.8 32.0 575.0 .69
- 1 AU ppb 51 12.4 7.0 14.0 1.0 57.0 1.14 I PT ppb 51 18.0 11.0 19.3 1.0 71.0 1.07 1 PD ppb 51 48.6 20.0 48.9 1.0 169.0 1.01
-I
NOTE - Coefficient of Variation = Standard Deviation / Mean
NIMMI
LEOPARD LAKE LEOPARD ROCK
BIEriRLE B
L._ B C 1 RZI)
rI9-r-
-Fr.r--rinhc3
- 1 Element Unit n Mean Median Standard Lowest Highest Coef. I Deviation Value Value of Var. 1
-I I AS ppm 51 1.2542 1.4314 .4644 .0000 1.7160 -.37 1 CO ppm 51 1.5561 1.6435 .2983 1.0000 2.1367 .19 1 -CU % 51 -1.0792 -.8542 .7330 -2.4949 -.0918 -.68
- 1 -NI Z- 51 -1.6101 -1.2857 .6745 -3.2218 -.8041 -.42 I ZN ppm 51 1.8937 1.7993 .2360 1.4314 2.6107 .12 1 CR ppm 51 2.2048 2.2577 .3496 1.5052 2.7597 .16
-1 -AU ppb 51 .8033 .8451 .5266 .0000 1.7559 .66 I -PT ppb 51 .9152 1.0414 .6262 .0000 1.8513 .68 I -PD ppb 51 1.3424 1.3010 .6631 .0000 2.2279 .49
-I
NOTE - Coefficient of Variation = Standard Deviation / Mean
14
TABLE 3
LEOPARD LAYE LEOPARD ROCK
CQRRL-AT I CIN! t'+iATR I X
AS CO CU NI ZN CR AU PT PD
AS 1.0000 -. 120E -.2017 -.2412 -.3139 -. 1139 -. 1578 CO 1.0000 CU .7479 1.0000 NI .8901 .812E 1.0000 ZN .1526 .3849 .3900 .2270 1.0000 -.0026 -.0561 CR .5609 .7626 .6970 1.0000 AU .0574 .2E44 .4022 .3231 .2776 . 221 1 1.0000 PT .1382 .3561 .2978 .3101 .4842 1.0000 PD .6248 .6828 .7667 .1868 .6074 .6158 .5331 1.0000
51 SAMPLE PAIRS ARE COMPLETE
TABLE 4 LEONARD LAKE GABBRO
Element
GINIPt_E 9 -T-c TI9TICB
Unit n Mean Median Standard Lowest Deviation Value
Highest Value
Coef. of Var.
I AS ppm 21 20.3 22.0 12.7 1.0 41.0 .63 I CO ppm 21 23.0 22.0 5.0 17.0 40.0 .22 i CU ppm 21 172.0 91.0 322.9 39.0 1542.0 1.88
- I NI ppm 21 73.0 50.0 81.1 8.0 390.0 1.11 I ZN ppm 21 80.2 72.0 25.7 51.0 160.0 .32 I CR ppm 21 91.0 70.0 51.1 26.0 200.0 .56 i AU ppb 21 3.4 2.0 3.2 1.0 12.0 .96 i PT ppb 21 8.8 8.0 8.0 1.0 28.0 .91 i PD ppb 21 6.0 2.0 5.2 1.0 18.0 .87
NOTE - Coefficient of Variation = Standard Deviation / Mean
MOON
LEOPARD LAKE GABBRO
I M I L_ r( T I ST I GB
MONA
Element
L_ C) C 18 1 el? Trari•• -F rrn
Unit n Mean Median Standard Lowest Deviation Value
d
Highest Value
Coef. of Var.
AS ppm 21 1.1486 1.3424 .4710 .0000 1.6128 .41 CO ppm 21 1.3534 1.3424 .0837 1.2304 1.6021 .06 CU ppm 21 2.0007 1.9590 .3592 1.5911 3. 1881 .18 NI ppm 21 1.7001 1.6990 .3783 .9031 2. 5911 :22 ZN ppm 21 1.8865 1.8573 .1218 1.7076 2.2041 .06 CR ppm 21 1.8957 1.8451 .2435 1.4150 2.3010 .13 AU p o b 21 .3645 .3010 .3744 .0000 1.0792 1.03 PT ppb 21 .6793 .9031 .5529 .0000 1.4472 .81 PD ppb 21 .5817 .3010 .4416 .0000 1.2553 .76
NOTE - Coefficient of Variation = Standard Deviation / Mean
TABLE 5
LEOPARD LAKE GP.BBRD
CCl R RE LA é i Cns4 MET R I X
AS CO CU NI ZN CR AU PT PD
AS 1.000e -.0875 CO .3396 1. 0000 -. 0018 CU .1969 .7929 1.0000 -. 1066 NI .4941 .5280 1.0000 -.1664 -.2499 -.0796 ZN .0799 .0941 .0418 1.0000 -.1531 CR .0148 .1951 . 4756 .6570 .1596 1.0000 -. 0305 AU .3040 .0325 .036E .1824 1.0000 PT .0661 .1288 .0721 .1083 .3769 1.0000 PD .4036 .2964 .27E7 .33153 .8351 .341C 1 . C-t •
21 SAMPLE PAIRS ARE COMPLETE
16
17
8.0 COST STATEMENT
GEOLOGIST 14.25 days @ $330/day 4,702.50
ASSISTANT 11.50 days @ $160/day 1,840.00
TRANSPORTATION
Airfares 1,982.60
Float plane 1,068.74
Shipping 1,032.67
FOOD/ACCOMMODATIONS 894.07
EQUIPMENT/SUPPLIES 571.57
GEOCHEM ANALYSIS 1,709.99
EQUIPMENT RENTAL 250.00
DRAFTING 373.75
TELEPHONE 48.01
TYPING, REPRODUCTION, BOOKKEEPING, ETC. 245.52
REPORT PREPARATION, ENGINEERING 860.00
COMPUTER COSTS 200.00
TOTAL: $15,779.42
G̀GGcccc~c
~~F E.SS /0%
n
G. H. GIROUX Â BRITISH ~̂
C 0~P
J~J77~%
OEMS
18
9.0 BIBLIOGRAPHY
Bergeron, R. (1954), Preliminary Report on Gerido Lake Area, New Quebec; Quebec Dept. of Natural Resources P.R. No. 291.
Bergeron, R. (1955), Preliminary Report on the Venet Lake Area, West Half, New Quebec, Quebec Dept. of Natural Resources P.R. No. 311.
Dugas, J. (1970), Metalic Mineralization in Part of the Labrador Trough, North Part, Quebec Dept. of Natural Resources Special Paper No. 5.
Elberty, W.T. (1955), Holannah Mines Ltd. Final Report on Erickson No. 3 claim group. Assessment Report GM-5909-A.
Blberty, W.T. (1956), Erickson No. 3 Claim Group Record of Drilling, 1956 Assessment Report GM3909-C.
Grant, J.M. (1955), Magnetometer Survey of Erickson No. 3., Assessment Report GM-3909-B.
Sauve, P., Bergeron. (1956),-- Gerido-Lake-Thevenet Lake, New Quebec, Quebec Dept. of Natural Resources Geological Report 104.
Tully, D.W. (1981), Report on the Leopard Lake Claim Group for Conquest Exploration Ltd. (Private Report).
19
10.0 CERTIFICATE
I G. H. Giroux, of 982 Broadview Drive, North Vancouver, British
Columbia, do hereby certify that:
1. I am a consulting geological engineer with an office at #701 - 675 West
Hastings Street, Vancouver, British Columbia.
2. I am a graduate of the University of British Columbia in 1970 with a
B.A. Sc. and in 1984 with a M.A.Sc. both in Geological Engineering.
3. I have practiced my profession continuously since 1970.
4. I am a member in good standing of the Association of Professional
Engineers of the Province of British Columbia.
5. I have no interest, either direct or indirect in the properties or
securities of Tournigan Mining Explorations Ltd., nor do I expect to
receive any such interest.
6. I consent to the use of this report by Tournigan Mining Explorations
Ltd. in submissions to the B.C. Superintendent of Brokers and the
Vancouver Stock Exchange and to distribute all or parts of the report to
shareholders or other parties, provided that the meaning is not altered by
partial quotes. G~s‘ F E S 5 /(j
~+ es
GQQ-O Q `oINcF " n OF
f/4 G. R GIROUX VVE+-ITI5H
G. H. Giro 982 Broadvie North Vancouv?,, September 25, 198
•
NIP
4 PLAN OF TRENCH No.1
Oct ,1455 ERLCKSON NQ3
ÇH ANNEL 41c4 4YS1 • 4254 42G3 4256 42.57 4258
COPPER tO4 .44 Ig • 2Z .11 •41 .73
NIChEL K.1 . 13 .11 -10 • 22 .20 .70
rMIP 4:61 4252 t
4-20 4251 4262 4263 4264 4265
COPPPik .04 .32 .4Z .76 _ 94 .53 .s1 .32
NICKEL Nil .11 .12 -14 .'4 .17 , f* ,22
N
Mil ASSdY >EiS 7. 38 13 CRT$ 1 8O5 Is2L4)3844 =03 2)360Z t)380i
C.OPPgR .c2 30 .24 .1/ .Z8 •51 .55 . .44 .37
NIGISEL. T. I.SO , IS .2i .18 .2z .16 .17 .24 .3i l
PUBLIC
rl5EPTr
1
2 1 • 4• 1
DR/FT - COVERED
LEGEND
LtiOPARD ROCK
GAS SRO
DISSEMINATED Su.Pl t0E5
iME.2
• ,7o INT ▪ _owracr
18 459
rii ictère des Richesses tr'i`g: C~j~a Q.Aec
SERVICE DES GITES MINE-:RAUX
No GM-. 3'
LEGEND
• LE 0 PA RD POCK
GABBRO
DISSEMINATED SULPHIDES.
SRGAR
.roiNT
CONTACT
4278
.40
PUBLIC Ministere d;s riicLAes blurt:Ns, &bee
SERVICE DES GirES MINÉRAUX
No G M . ..
Œt., I955 ERICKSON No.3
PLAN OF TRENCH Na 2
18466 _ u• 811 467
t:;aa:±re dss Fie.ta.scs Liurcri:S, 2
SERVICE DES GITES M1NERAUX )2j01 4300 CHANNEL,
Cu .08 ~1.53 42 91 421e 4297
NO GM- ....SCR) ..9 .44 .39 .30
.22 .24 •14 .!4 .17
CHIP
C+} Ni PUBLiC
1-,
,oq l 22 .56 .27 .22 .41 .4-T .08 .33 .68
4316 4313 4312 4311 4310
LEGEND
Œ0A*D ROCK
"A'sRo
MSS. PRINATCD $ULPS1 DES
`S,„„ ZOJNT
SMEAR
URN No.
PLAN OF TRENCH N.3
"= 10'
18464 1+3 "
18463
It 3
DOH Cu Ni
URN. No.
3839 .18 .18
38+0 .15 .10
3841 16 0S 11. 9. 10.
3
w4-ON
00+6N
LEGEND I• ~ .1 r.v:~•i: d~S IlÎzfiz:sc5 !i •,tuar:.5, G.cJwc
SERVICE DES GI T ES 1111N F AUX
NO GM— qQ9-R
LGoPARD AOLK
z
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?O I NT Oct,,1956 ERICKSON No..3
PUBLIC I PLAN OF TRENCH Nv371 T
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PUBLIC
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LEGEND
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'1 PUBHC ►ina;ère d:s f.ic'.,::~sa Y,'~r~C~s, Qu6bec
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10 PLAN OF TRENCH No.5
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SERVICE DES GÎTES MINÉRAUX
NO GM- 3109
ERICKSON NŒ3 0-,1955
a• PLAN OF TRENCH 1413.8 13
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1
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PUBLIC
Oct., 1955 ER IL 14,50 N No.3 10'
PLAN OF TRENCH No.10 IS
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PLAN OF TRENCH Noll ►6
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QUEBEC DEPARTMENT OF MINES
AP L (.) 1957
MINERAL DEPOSITS BRANCH
DECS6 ERICKSON No3
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