GM 12949REPORT ON ELECTROMAGNETIC AND GEOLOGIC SURVEYS

Ministère des Richesses Naturelles, Québec

SERVICE DES GITES MINERAUX

No GM- 2 (./..

REPORT OF

E Lturf-toyr. lc :IT GEC LOG IC SURVEYS

Ct;

CARPENTrER WEST TICUNDARY 'CROUP CF CLAIMS

CARMTIER aTti BARRAUTE TOW17SHIPS

FFOVINCE CF flUEBEC

by

F. J. Evelegh

and

F.. V. Stewart

Exploration Department, January 25, 1963 Canadian Johm-anville Company Limited Matheson, Ontario.

Table cf Contents

Page

Introduction . . . . . . . . . . . . . . . • . . . . 1

Property 2

Location and ;ecce sibility . . . . . . . . . . . . . • . • 2

Topography 3

Previous ,'ork 3

Line Cutting and Chaining 4

Electromagnetic Survey 4, 5, 6

General Geolo^y 6, 7, S

Geological Survey. . .. . . . . . . . . . . . . . . . . . . . 8, 9

Rock Types:

Andesites . . o . • • • 00 . • . • . . . • • • • • • • 9

Rhyolitic to Intermediate Volcanics 9

Bedded Tuffs and Aggloueratic Horizons 9, 10

Diorite 10

Feridoti`e 10., 11

Quartz-Feldspar Porphyry ''.

Structure 11, 12

Economic Geology:

Base 'Metals 12

Asbestos 12, 13

Interpretation of Electromagnetic Survey . . . . . . . . . . 13, 14

Conclusions and Recommendations. . . 14

Detailed Aseessment Report i

Certificate of Verification -- R. V. Stewart

Certificate of Verification -- F. J. Evelegh

List of Taps

Legend Sheet for Vorthwestern Quebec

Township Layout Plans •.. Barraute and Carpentier Townships

Geologic and Topographic Plans am Electromagnetic Profile Plans on a scale

of 1 inch equals 200 feet

Sheets C6 and C11 -- Carpentier Township

Sheets D5, D6, and D9 -- Barraute Township

R'r~1FCRT ON GP.( LCCIC iP:1', ELE;CTdiC;'t+iGMT IC ARir'EYs,

CARPi;PTIEII ;1E,,i: I3GtTI`•ARY GROUP CF CLAIMS,

CARF4TTtSSt~;.

T 1rt1T BAR:wtiI

7JTi~L~tLVfî+C-:i-~~,HIPS,

Fi1C~Y lYyCi~, CF ~:~~U4~s1.7L'L

Introduction:

The followin ; report describes the geologic and electromagnetic sur-

veys co ,.; leted during 1962 on seventeen mining claims located in Carpentier

and Parr t.ute Townships, Province of Cuebec.

Cutting and chaining of picicet lines were contracted to J. Alix Com-

pany Limited of Val d'0r, Quelec. Pieket lines were cut at right angles to a

northwest-southeast trending; base line and were established at 2004-foot inter-

vals. Picket: were fixed every 50 feet along these offset lines by chaining.

Electromagnetic surveying was conducted by R. Kaltwasser, senior

fieldman with Canadian Johns-Manville Company Limited. W. Scott assisted R.

Kaltwa:ser during the course of the survey. Electromagnetic readings were re-

corded at 100-foot intervals along the offset lines using a Ronka park I, hori-

zontal loop type unit. The results of this work are shown on the accompanying

Electromagnetic Profile Plans on a scale of one inch equals 200 feet.

Geological mapping was conducted by R. V. Stewart, geologist with

Canadian Johns-Manville Compary Limited; R. Kaltwasser, senior fieldman,

assisted during the course of the work. All rock exposures were tied into

the picket lines by chaining. add all topographic details were carefully noted.

The results ci this work are shown on the accompanying Geologic and Topographic

Plans on a scale of one inch equals 200 feet.

Supervision, interpretation and compilation of part of Vis report -

were the responsibility of F. J. Evelegh, senior geologist with Canadian Johns-

Manville Company Li._=itec. Pote that R. V. Stewart compiled the portion of

this report dealing with the geology of the claims group.

Property:

The claims surveyed coprise a contiguous group in Ranges IV and V

of Carpentier and Barraute Townships, Province cf Quebec

further identified as follows:

and are numbered and

C-186489 claims 1-2-3-4 -- N/2 lot 62

Range IV, Barraute Township ✓

Range IV, Carpentier Township V/

N/2 lots 1-2-3 Mho 110.

Development Licence No. 186489

C-186486 claims 1-2 -- N/2 lots 60-61

Range IV, Barraute Township v/

Development Licence No. -- 186486

C-184785 claims 1-2-3-4 -- 3/2 lot: 3-4

N/2 lots 5-4

- -

--

Range V, Carpentier Township ✓

Range IV, Carpentier Township ✓

C-186417 claims

C-184787 claims

C-184786 claims

Development Licence No. -- 184785

3-4 -- 3/2 lots 58-59 -- Range V, Barraute Township ✓

Development Licence No. 186417

2-3-4 -- 3/2 lots 60-61-62 - Range V, Barraute Township ✓

Development Licence No. -- 184787

3-4 -- 3/2 lots 1-2 -- Range V, Carpentier Township V"

Development Licence No. -- 184786.

These seventeen claims comprise approximately 850 acres.

Location and Accessibility:

The Canadian Johns-Manville claims are loc=:ted in Ranges IV and V

of Carpentier and Barraute Townships and form a contiguous group.

Access to within one mile of the property is provided by a coloniza-

tion road branching to the east from the highway leading north from Barraute.

This road has been constructed along the line between Ranges IV and V. The

range line has been well cut out from the Barraute-Chibougamau Railway to the

property and is passable by muskeg tractor.

3

Topography:

The major portion of the claims rrouj is covered by wet spruce mus-

keg with a. thick intergrowth of tag alders. Rock exposures are sparse as the

terrain is relatively flat and; exton'ively clay covered. Cutcrops occur

along low poplar ridges in the northeast, southwest and north-central portions

of the ;rcperty.

Prainage :Ls provided by narrow streams which flow to the west and

empty into the LaFlame River.

Previous 'Fork: ....-,.-

Staking and general exploration work have been carried out or the

claims discussed in this report since the time of the "Barvue" discovery in

the late 1940.s. Barrentier Cold Mires and Chatelet Mines Limited conducted

exploration programs on tee group. This wer<-; consisted of line cutting,, re-

connaissance magnetic surveying, geological mapping aWd diamond drilling of

magnetic anomalies. As no sulphide values of interest were encountered dur-

ing the course of this worl, the claims were allowed to lapse.

The Carpentier West Boundary Group of claims was staked during Sep-

tember 1961 and same were ]ater transferred to Canadian Johns-Manville Company

Limited. Line cutting and retailed magnetic surveying were carried out during;

the early winter of 1962 anè the work was filed for assessment purposes in

September of that year.

This area has been mapped by geologists of both the Geological. Survey

of Canada and the Quebec Department of Natural Resources, the latter in consid-

erable detail. and maps have been publ i feed covering the general area (see

section entitled "General Geology" for details).

4

Line Cutting and Chainins:

Lim cutting and chaining were contracted to J. Alix Company Limited

of V11 d'Or,..,•uabec, and the work was carriel out during the period January 9

to 31, inclusive, 1962. A base line striking N. 59° W. was turned off from a

point on the line between flanges IV and V, Carpentier Township, 400 feet east

of the Post between Lot• 2 and 3. This line was cut to the southeast for a

length of 3400 feet and to the northwest for a length of 5200 feet.

Picket liner wer turned off at right angles to the bare line and

were spaced at 200-foot intervals. Every second line was cut to the boundar-

ies of the claims group, -- the intermediate lines were cut to the arumed

limits of the ultrabasic zone (see accompanying plans).

Pickets with numbered locations were fixed every 50 feet along the

offset lines by chaînage. As the zone of interest was in close proximity to

the base line, the ends of the 400-foot lines were not tied in alert the claim

boundaries.

A total. of 23.4 miles of picket and base lines was cut and chaired

during the courre of niF1 Trogram.

rote that the line cutting and chairing were filed for assessment

purposes as part of the magnetic survey.

Electromagnetic Survey:

An electromagnetic survey was conducted over the Carpentier vest

Boundary Group of claims by E. Kaltwasser, senior fieldman with Canadian Johns-

Manville Company Limited; assisted by W. bcott. This program was carried out

during the period April 6 to 18, 1962.

-5 -

Readings were recorded unir: a Rorke ';4ark I, horizontal loop type

survey unit with a coil spacir.f. cf 200 feet. Thi wit had been zeroed on

both the "in" and "out" of p'rh:is e components over the ultrabasic sill at the

Beatty Fire of CanedIan Johns- 4anvill.e Co:1 ;any Limited in Beatty Township,

Province of Cntario, imaediately prior to the commencement of the survey.

? total of 847 stations spiced at 100-foot intervals was recor-

des during the course of the survey.

Test surveys have been coapleted with this unit over a graphitic

zone, a massive sulphide zone and a disseminated sul h da zor ,~, as aids in in-

terpreting the results obtained on unexplored claims groups. The following

data was obtained during these tests:

1. Massive sulphide zone -- a strong positive rise on the in-phase component

followed by an intense negative with a resuml tion to zero

or near-zero when the station was off the conductor. The

out-of phase component remained within 15 of zero.

2, Disseminated sulphide zone -- similar to No. 1 but with lower in-phase

peaks.

3. Graphitic zoro -- both the in-phase and out-of phase components paralleled

one another and followed the pattern of the in-phase of

T.o. 1.

It should also be rotee that coil spacing (should be exactly 200

feet) and the angle of the coils to the horizontal (each coil should be hori-

zontal) play a large part in this type of survey. Errors in one or both of

the above may cause anouF lies of sufficient magnitude to indicate the presence

of a disseminated sulphide zone. Consequently, topography is an important

factor in this work.

The results of the electromagnetic survey are shown, on the accompany-

irg Electromagnetic Profile Flans on a scale of one inch equals 200 feet.

General Geology:

The geology of the area has been mapped by L. J. Weeks for the Goo-

logical Survey of Canada during 1936-37 and the results are shown on. Map 529A

entitled "Duverny Gast Half)" on a scale of one inch equals one mile.

During 1948-49 W. tlI . Weber mapped the area for the Quebec Depart-

ment of Natural Resources and the results are shown on Map No. B484 entitled

"Geological Sketch '4ap of the Amos-Duvex T4hrraute Area" and published during

1951.

The Carpentier portion, of the map area was mapped in detail during

the 1962 field season by the Quebec Department of Natural Resources. The

results of this mapping will be published on 1000 scale sheets.

The following "Table of Formations" has been to en directly. from

Page 2 of P.L. No. 228, compiled by W. W. Weber.

Table of Formations

quaternary Pleistocene

Stream and swamp deposits

Till, sac°, gravel, and lacustrine clays

Late Precambrian Keewenawan (?) Tiabase, gabbro, and quartz gabb o dykes

Post-Alncman or

Late A1goman

Quartz veins

Faulting

Early Precambrian - 'Algo;nan (?)

AYlite, dicrite, quartz porphyry, and diorite porphyry dykes

Granite, rorphyritic granite and granodio-rite

Pwt-Ke wa.tin- type

Peridotite

Quartz and feldspar, albite porphyries

Gabbro, dicrite and quartz diorite

Faulting and folding

Keewatin-typa

Metadiorite and metadiabase

Acidic lavas, pyroclastics, and minor inter mediate volcanics

Intermediate lavas, agglomerate

Basic lavas, tuffs, flow breccia

The volcanic rocks in the map area are a complex assemblage of acid

and intermediate lava, with pyroclastic volcanic types occurring to a lesser

extent associated with these more massive lavas. The pyroclastic types are

mainly minor agglomerate bands and bedded tuffs.

Intrudirg these volcanic rocks in the central part of the claims

group is a basic sill composed of diorite and peridotite.

Also found cutting the volcanic rocks in the area were narrow dykes

of quartz and feldspar porphyry.

The general strike of all rock types in the area is S. 60° E., and

the din deduced from diamond drilling, Inform ton, is generally 70 degrees to

8C degrees to the northeast.

The map area is possibly part cf the south limb of the tuverny syn-

cline which lies approximately four miles to the northeast, and parallels the

regional strike (the axis of this syncline).

Geological Survey:

A det%iled program of geological. mapping and prospecting as carried

out on the Carpentier qest Boundary Group of claims by R. V. Stewart, geologist

with Canadian Johns-Yenville Company Limited; assisted by R. haltwasser,

senior fioldman. This work was carried out during the period August 12 to 20,

1962.

All rock exposures and topographic features were tied into the picket

line grid by the chain and compass method. Cutcrops were partially stripped

for detailed examination for chrysotile fibre and sulphide mineralization.

The results of the detailed magnetic survey, (previously Mee for

assessment purposes) wore used extensively during the course of this work as

wore aerial photographs of the area. The geologic interpretation of the map

ara is based to a moderate extent on the results of the magnetic survey.

These results wore especially useful in tutlining the ultrabasic intrusive

and the cross structures offsetting same.

Geological survey results are shown on the accompanying five Geologic

and Topographic Plans on a scale of one inch equals 200 feet.

It should be noted that R. V. Stewart compiled the portion of tais

report dealing with the geology of the claims group, while F. J. Evelegh in-

terpreted the naps and co-:piled the remainder of the report,

Rock Types:

Andesite:

This rock is very fine-grained to apharitic and is greyish-green in

colour. Occasional variations in composition to a more basic volcanic rock

occur locally, but the intermediate ande itic type predominates. Cnly four

scattered andesitic outcrop areas exist on the claims group, so that only

limited information was gleaned. Using the limited amount of outcrops and

generalizing, the •andesite is liessive with no pillows or flow structure evi-

denced. Locally the rock is sheared and moderately schistose, eg., south half

of Lot 57, Range IV, Barraute Township.

Rhyolitic to Intermediate Volcanics:

This is a very fine-grained to aphanitic, massive, greyish-buff to

white coloured rock, with minor evidence of flow banding locally. Local car-

bonatization of the rhyolite adjacent to fault shear zones was noted to a

minor extort. The buff colour of the rhyolite appears to be caused locally

by fine oxidized pyrite disseminations throughout the rhyolite.

Minor variations to a more intermediate type occur locally within and

adjacent to the massive rhyolite type.

Bedded Tuffs and Aggloneratic Horizons:

Surface mapping has outlined only two small tuff outcrops in the map

area. However, it ie suspected that jart of the volcanic outcro p area north

of the peridotite outcrop in Lot 62, Range V, Barraute Township, is composed

of interbedded tuffs. The remaining evidence of tuff-agglomeratic existence

i:: that taken fro% original diamond drilling in the area. It appears from

- 10 -

drilling adjacent to the basic sill intrusion that a complex assemblige of inter-

bedded tuffs, apçlomerate and rhyolitic bands, approximately 400 feet wide,

parallels, and is in contact with the peridotite intrusion on the north or

hanging wall side of tho sill. Logging of holes in this horizon indicates acid

and intermediate tuffs with tedding and schistosity of the tuffs steeply dip-

ping to the north. Agglomerate horizons have acidic bombs of approximately

one inch average size.

Diorite:

Only three small outcrops of diorite occur on the claims group, and

these are found in the south part of Lot 57, Range V of Barraute Township; and

are not part of the main diorite-peridotite sill complex.

From diamond drill examination of the main sill, the diorite appears

to be a fine- to medium-grained, greenish-grey coloured rock, with an apparent

differential metamorphism locally, to give a "meta-diorite' with the true dio-

ritic texture obscured. Pue to the lack of outcrop, no valid explanation can

be given for this secondary alteration of the diorite. The three diorite out-

crops in the area have essentially the same texture as that described above,

and this separate intrusion is most likely the same age as the larger diorite

body some 700 feet due north.

Peridotite:

The three small existing peridotite outcrops on the claims group in

Lot 62 of Barraute Township can be termed a pyroxene rich peridotite. It is a

medium to coarse-grained, greenish-black rock, with very distinct large pyrex-

one cleavages noted. Serpentinization of the peridotite appears to be only

slight to moderate here.

-11 -

Examination cf the diamond drill core cutting the peridotite reveeled

a finer graines:, more highly rarpentinized peridotite, v, te a definite decrease

ir, the number of pyroxenes. Cerbonatization of the peridotite has also been

noted to a moderate degree near the central portion of the peridotite, but the

contacts of the feridotite •- with the volcani.cs ana the gabbro -- are note-

ably fresh and unaltered. Absence of serpentine-picrolite veins within the

peridotite is distinctive. ti few white carbonate veins cut the mass locally.

Nowhere could any chrysotile fibre veine be seen.

Quartz-Felds r PorEhyrz:

Only two small occurrences of quartz-porphyry dyke were located on

the map area. Examination showed these to be coarse-grained dyke rocks -- the

width of dykes noted being about ten feet, and the strike parallel to the

regional strike, e} , S. 60° E. Examination of these dykes from core drilling

indicates finer grained feldspar porphyry dykes also cutting the volcanics.

Thus these porphyry dykes may be quite common within the map area. No mineral-

ization was noted in these dykes.

Structures

The main •structural feature of the area appears to be the constant

persistent strike of all rock types in a direction S. 60° E. Diamond drilling

has indicated a quite consistent dip of rock types at approximately 60 to 80

degrees to the northeast. The projection of the''Duvern .r Syncline" axis to the

southeast from the "Geological Sketch Map of the Amos-Duverny-F3arraute Area"

onto the herein described claims group, appears to coincide with h the thesis that

the map area is part of the south limb of this syncline.

Due to the lack of outcrop in the area, it was almost impossible to

deduce much about the existence of strong faulting in the area. However, shear-

ing noted in outcrop and diamond drill core indicates the shearing parallels the

- 12 •

regional strike. L;hearirg to a minor extent was evidenced - in almost all out-

crop areas, so that t'ele structural trait appears quite cor_sictent throughout

the area.

It is important to rote from previous .work completed by the Quebec

Department of !`atural Resources in the area that a major fault break called

the "Barvue Break" apparently is contained in the band of tuff and agglomerate

immediately north of the main basic intrusive in the map area. This is the

same fault zone on which the Barvue Mines ore zone is located some six wiles

along the strike to the northwest. Evidence of faulting in this zone is only

moderately indicated from the recent mapping mainly due to the lack of outcrop.

However, a major shear of this intensity would probably acount for the sheared

nature of the rocks it the man area.

A distinct contact between the diorite and peridotite was evidenced

in diamond drill core, which indicates separate age intrusions for these two

rock types. Due to their close association and conformable nature, it is

suggested that the time between intrusions is not very great, and they may have

been separate injections from a parent magma.

Although no dykes of porphyry were noted cutting the peridotite, it

is assumed from the more general geology of the tcwnshiee that these dykes

belong to the Early Precambrian possibly of Algernon age, and are therefore the

youngest rocks in the area.

Economic Geology:

Bane Metals:

No sulphide m.ineralizati. n to any extent has been noted on the out-

crops or in the Grill core examined on the claims group.

Asbestos:

No trace of chrysotile asbestos fibre was noted either in outcrops or

-13 -

diamond drill core examined. Due to the complete diamond drill intersection

of the peridotite in Lot 60, Sarraute Township and Lot 3, Carpentier Township

without a trace of fibre, it is felt that due to the narrowing of the perido--

tite resepectively west and east of these two locations, no further work need

be done here. A strong magnetic cross fault in Lot 2, Carpentier Township

appears to offset the peridotite by approximately 100 feet.

A limited amount of drilling adjacent this fault, and possibly in

magnetically favourable areas east and west of this zone, would prove or dis-

prove the economic fibre pos. ibilities for the map area.

Interpretation of Electromagnetic Survey:

A study of the electromagnetic profile plans indicates little varia-

tion over the claims group. Several weak, isolated "in-phase" peaks occur on

Map Sheet D-6. However, as these peaks range only from 15 to 20 units, the

conductors are probably due to disseminated pyrite and/or pyrrhotite mineral-

ization in the diorite and intermediate volcanic rocks. The zone over the

ultrabasic intrusive on line 2400 West, immediately north of the base line

is probably caused by this type of mineralization. A similar weak conducting

zone occurs in the north part of Map Sheet D-9, conforming with. the regional

strike of the formations, and extending over a length of 1500 feet. Due to

the weak parallelism of the "in-phase" and "out-of phase" curves, this zone

is assumed to represent a tuffaceous horizon contas.ning minor graphite and sul-

phide mineralization. Another, extremely weak, irregular zone occurs in the

north part of Map Sheet C-6. However, as the "in-phase" peaks do not exceed

10 units, this zone has not been outlined on the maps.

Two isolated moderate to strong conducting zones occur on line 20}00

West, to the south of the base line and are shown on Map Sheets D-6 and D-9.

- 14 -

The most northerly zone has an "in-phase" peak of 51 but due to the similar

"out-of phase" peak of 42, this conductor is probably due to graphite. The

conductor to the south has a marked crossover with reverse "in-phase" peaks

of 28 and 15. The "out-of phase" component shows a slight parallel effect.

This tone is probably due to a graphitic zone with moderate sulphide mineral-

ization.

Conclusions and Recommendations:

The results of axploraticn work completed to date on the Carpentier

'test. Boundary Croup of claims indicate little potential for either chrysotile

or sulphic w mirera ization of ecoroa:ic importance. However, prior to allowinE

the claims to lapse, limited diamond drilling is recommended to test the

ultrabasic intrusive in the vicinity of the crocs structure shown on the

accompanying plans. Further work would. depend upon the results obtained from

this. program.

R. V. Stewart, Geologist

Jar:,ary 25, 1963.

F. J. E'vel gh, Senior Geologist

August 12 - 30, 1962 and January 7 - 8, 1963 -- 17 x 8

August 12 - 30, 1962 •- 15 x 8

September 3 - 13, 1962 - 9 x 8 January 25, 1963 -- 1 x 8

September 9 - 11, 1962 and January 7 9, 1963 -- 4 x 8

•-

R. Stewart -- geologist

R. Kaltwasser

J. Lytle B. Kallunki

F. J. Lvelegh

assistant

draughtsman

typist

geologist

40.

NO 40

--

01.410

4000

41006

a-

i DET.? ILk.L Aa.3LSS`ZENT REPORT

CARPENTIER WEST BOUNDARY CROUP CF CLAM,

CARFEFTIE`- and BARRAUTç TOWNSHIPS,

PROVINCE CF QUEBEC

Geological Surva:

This work was carried out by R. V. Stewart, assisted by R. r:'. Yalt-wasser. All personnel connected with this work are employees with Canadian Johns-Manville Company Limited and reside at Matheson, Ontario.

136 hours

120 hours

72 hours

8 hours

32 hours

Total 368 hours

Total number of man days worked -- X68 x 7 -- 322 days -- "B" 8

Electromagnetic Survey:

This work was conducted by R. Kaltwasser with the assistance of J. Scott. All personnel connected with this work are employees with Canadian Johns-Manville Company Limited and reside at Matheson, Ontario.

R. Kaltwasser -- operator -- April 6 - 18, 1962 -- 12 x 8

W. Scott -- assistant -- April 6 - 18, 1962 -- 12 x 8

J. Lytle -- draughtsman -- June 2 - 10, 1962 -- 8 x 8

F. J. Evelegh-- geologist -- January 10 11, 1963 -- 2 x 8

Total

01/011,

000

4040

96 hours

96 hours

64 hours

16 hours

272 hours

Total number of man days worked -- 272 x 7 -- 238 days -- "B" s

Total number of man days to be applied against mining claims 0-186489-1-2-3-4;

C-186486-1-2; C-184785-1-2-3-4; C-186417-3-4; C-184787-2-3-4 and C-184786-3-4 --

322 t 238 s 5Q days

F. J. Evel.egh, Senior Geologist

January 25, 1963

Certificate Verifying Geologic and Electromagnetic

Report and Maps Cc\verine the Mining Claims of the

Carpentier West Boundary Group of Claires ac Listed

in this report and located in Carpentier and

Sarraute Townships,. Province of Quebec.

I, R. Ti. Stewart, general Delivery, Matheson, Ontario

hereby- certify

1. That I have a personal ar_c intimate knowledge of the facts and data set

forth in the report and maps covering the surveys on the mining claims

of the Carzentier fleet Boundary Group.

2. That the grounds of my knowledge are geological mapping of the claims

group and ccyipilation of the geological section of the report.

3. That the attached report and maps are correct on the basis cf work come

pletBd to data.

R. V. Stewart, Geologist

Sworn before me at Matheson,

in the Province of Ontario.

This 25t1 dey of Jeruary, 1963.

/ f1 ro-.;~ N.,

S aria u-: of Ccerciissioner

• S`a?Cr'., _ ~ ~ ,

f.:::' .

Certificate Verifying Geologic and Electromagnetic

Report and ''a.ps Covering the Mining Claims of the

Carpentier t4est Boundary Croup of Claims as listed

in this Report and Located in Carpentier and

13arraute Township, Province of Quebec.

I, F. J. 3velegh, 3ox 276, Math+eson, Ontario

hereby certify

1. That I have a personal and intimate knowledge of the facts and data set

forth in the report and maps covcrin ! the surveys on the mining claims

of the Carpentier 1;est Boundary. Group.

2. That the ground's of my knowledge are supervision, interpretation and

compilation of part of the report.

3. That the •atta< ied report and maps are correct on the basis of work

completed to date.

F. J. Evtlegh., Senior Geologist

Sworn before me at Matheson,

in the Province of Ontario.

This 25th .ay of January, 1963.

S gnat e of Commissioner

s

S I

S2

S3

S4

S5

S6

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1 2 R 1

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Iron Forr„ation.

Granite .

Granoâiorite

Aphte.

Pe9nriati te.

Ma9netie Bose Control stmt; a.

Geolo9ieal Contact .

f G- •Geo/ ^9 rc .

FQ..It Zone . M-r/a~ prit• T- Tpc9 raPh:c-

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Scale 40 units ./inch.

East s po.rit,ve.

West it ne4utive.

N.P.C.S.- Not p r-r er Coil 4-pacing .

.L -L 1

o

00

TOPO. SYM$OL$ outcrop.

Higher G roan a.

Scarp .

Muskeg or Swamp.

Creek.

Drill Hole.

Busl, Road.

Trench,

Rail recd -

Power Line .

Buildin1S.

Main Road.

/Geo/o5ica l Syrr► boIs.

Strike and dip.

Strike and top.

Strike, dip and top.

Sc histosity.

CANADIAN JOHNS-MANVILLE CO. LTD, MATHESON MUNRO MINE ONTARIO

LEGEND SHEET ~ PROVINCE OF QUE.

scats . ;;A /b1 aLyt_ /î f62

nhk4,'r;~J: K. L. PRQ1/ TRAM ~ 4. ef . APoR vrD F. û: E .~ e s ~

u E.

A

OA•

4e

• • 76• 7A- 7L- o.

rOF ..(. .

M...,....

I

.,

°w

,-,

'Rp~ ,

"â:o,

L.1,....,. ~ T ..r n~.,,~„

~ r~„ti

gpyprtlie I

c.R

~.

.ti

e^ •

M rww

•~`

Vdda L. c.:,.

a

4

Y L. 7.iv

Ld . r,:~

d RSRRVor

oourv

R . ► SL

-F i_

lia .

11

~,..

....: • L,•R(slR

) CA6yM ..

t l

...r . •

lQ U E L O....:., ,t

P

°

vo1R5: ..d ...

T 1..

-11,4T+ssM"

CA L.

B 1.\'''. Ô (t V

/ P'

Bar a., ~

}} Kew* p,

r

- ,

Alit

Ak~~t Lo Tuy,.r

`. i ~ Q

~N.rwyJc.

~ /..

(.1R r:

»!! I

DO- ~~ 6

Diorite,

Lan,prophyre.

Dia base .

Peridotite.

Pyroxenite

Gabbro.

Tni.lc - Ça.rbonate Rock.

=NM

~ _

= Q

CEO /WAG SYMBOLS_ .:=,. at 4.1.1 °

44.4... Z. ~ ca to 2 ~ s...~.

CT) tr- Contour- Mier-Val : 500 9a r, ,r.raS, ~

7•1 >, !v CC ~

^+

~ g a CD iv ~ ~ i; • U-4p

47

v~ :a

ca'U

,ry, >•c~ Od

ELECTRO-MAG, SYMBIN_,Z la ,.--.4

GEOL. .• L EGEND - Acidic to Intermediate Volcanics.

R hyoNte.

Dacite

Intermediate to Basic Volcaics.

A ndesite .

Basa It.

Tuff.

Agglomerate.

Undiff'erentiatecl Sedimentaries.

Con9 lorr,ero.te.

Arkose .

G ro.y wac ke.

S late.

Quartzite,

LOCATION SKE

% '♦

In phase curve.

Out phase Curve.

Conducting Zone M. Medial,.,.

W. weak .

V2

V4