KEPORT O!

SNJ-AUHl/Tih AND fcLKUTROMAGNlWlC HUliVKYS

63.1962 MUNRO 010

OF THh HAIJULH OPTIOH. KUHItO TO^HS

YhlJJDWKHIFK BEAK MIHB5 LlillYED

Yellowknife Bear Mines Limited holds an option on 27 claims

in Munro Township. During the spring of 1966, magnetometer and electro

magnetic survey e were performed over the ground under the writer's super

vision. The following is a resume of observations.

The property consists of 27 contiguoue clairaB, the Hansen

option, situated in the northwest corner of Munro Township, adjoining

to the went of the Centre Hill mine.

Claim numbers are LOOOX6 to -2A inclusive, L00034 to -43

inclusive, and 1-80052 to -59 inclusive.

Access is by road to the Centre Hill property thence overland

to the claims.

The area is one of mixed basic to acid volcanics intruded

by basic arid ultrabasic bodies, all with a general northwesst-southeast

trend. Oranite an i related intrutdves are known in the vicinity.

A wftjor northwest-trending fault the Centre Hill Fault ~

its known on the adjoining property, while several north-south, northwest

and northeast faults of limited displacement are napped in the area.

'me Hansen claime are in large part drift-covered, but with

limited outcrop of intermediate volcanics, gabbro, and one diabase dike.

- s -

On the property of Centre Hill Mine, copper ore, in the form

of chalcopyrite with associated pyrrhotite, occurs at intervals in a

Kruphitic acid tuff and agglomerate horieon in close proximity to a

lArp.9 .jabbro-peridotita mass. The neophyiiieal work on the Yellowknife

Hear ground wao done in an attempt to locate similar mineralization.

V.JKK

A north-uouth oriented 300 foot line grid vus cut and chained

with stationB at KX) foot interval on all line B. Total length of line

cut was ;,1 miles.

A magnetometer survey was performed over this line grid,

using a Sharpe MF l flux-gate jaagnetometer with accuracy of 20 gammas

pu r- BCftlo division. Heftdin^s were taken at all hundred-foot stations,

and ut intervening points where neceRsary. Uesulte, corrected for diurnal

variation, are plotted and contoured on the accompanying 200 foot to the

inch plan.

An electromagnetic survey was performed over the sn*ie grid

us 3 rv; a Sharpe 250 unit with parallel line, vertical coil configuration.

l.xcept whore otherwise noted coil separation was 600 feet, i esults in

profile form are plotted on the accompanying ROO foot to the inch plan.

details are appended*

Magnetic reuults agree well with the known geology. A diabase

dike known on the eouth-central part of the property appears as a high,

but, contrary to geological maps of the area apparently does not extend

the property under overburden.

- 3 -

Hore or loss; continuous basic intrueives OTOBB the northerly part of the ^roup, though directed and offset by faults, while amaller hir;hs in the eouthvest part of the property probably also represent baltic IntrupiveB.

The broad northwest-trending low in the eoutheajst part of theF,roup i e believed to represent an acid intrusive and/or heavy overburden,S the result of deep erosion along the Centre Hill fault.

Numerous nroes of conductivity tire indicated, the most prominent of which arc us f o) lows i

(A) A strong conductor traced for 2,AOQ feet along a gabbro- volcanio contact in the most northerly part of the property.

(B) A weak but persistent feature following a magnetic high centred at 13N on line 33. This io 600 and perhaps ovsr 2,000 feet in length, with thr central portion passing along the property boundary. A similar feature is found a3.ong the property boundary at 6W.

(C) A conductor of moderate strength coinciding with a magnetic high at ?3S on line 5/*. Thin has been traced for 1,400 feet, pausing out of tht* property to the southwest.

(D) to (G) Four moderate to strong conductors with no magnetic coincidences, one of v,'hich lies alory; the Centre Hill fault, at US on lint- li, 75 on line 60, 5N on line 75, and 2#3 on line IP.

In addition th re are a nre'''t raany weak to strong arid more or leaf) isolated conductors of limited length,

While graphite and overburden undoubtedly are the cause of many of tho corriuetore, BOMO can b*i considered good drilling targets, in

particular the first throe enumerated.

Further geophysical information would be desirable en these and the numerous ot.hor oonduotora, prior to selecting drill-Bites* A

oh*ck of th^ nora prominent features by induced poiariBfttion in reooenended. Cost should be in the ^2,000 - t3,000 range.

Hespeotfully submitted,

, M.A.Bo. f Consulting Geologist

Toronto, Ontario Juno ?3, 1966

42A89SEei62 63.1962 MUNRO

li) F 1 0 RT

ON T FI E

POLARIZATION

SURVEY

ON THE PROPERTY. OF

YPI.,] .OWKNIFE BEAR MINES LIMITED

MUNRO TOWNSHIP

ONTARIO

0S0

IN T R O DU C TIC) N

During the month of July and August, 1966

an Induced Polarization Survey was carried out over some

winter cut line detailing interesting areas on the twenty-seven

(2V) claim group of Yellowknife Bear Mines Limited in Munro

Township, District of Cochrane, Larder Lake Mining Division.

The survey was designed to explore certain

electromagnetic anomalies of a previous survey, occurlng on

a possible contact between spherulitic lava to the north and

SCOP

reddish weathering black peridotite to the south. The

property may lie on or quite close to the major control

st i-uetiire of !.ho Potter Doal fault.

pRorF.K'Ty LOCATION AMD ACCBSS

'l 'he property comprises twenty-seven (2?)

contiguous uri pa tented mining claims known as follows:

l ^C'GJ 6 - 80024 inclusive ( 9 claims)I., 80034 - 80043 " (10 claims)I., BCO:;2 - 8001)9 " ( 8 claims)

TOTAL 2? claims

The claims are located In the northwest

corner of Munro Township, Concessions V and VI, Lots 9*

10, M , and 12.

Access is by motor vehicle from Matheson on

Kwy, #101 14 miles to the Munro Mine turnoff (formerly

Centre Iiill Mines Limited) then by a private gravel road to

the shaft of the operating Munro Copper Mine located in

Claim No. l-''-.t ;39 r)5 (6 miles from the turnoff).

A base line from the Munro shaft running west

connect o the a out*, h east corner post of the Yellowkriife

property. The distance from the shaft to property corner

was chained at 6,475 feet as shown on the plan.

scat- 3 .

CEP]' HVSTCAL. SURVEY

The survey lines were cut in the winter In

a north-Bcut.h direction. Location of tho lines was hampered

by dense tflg alder under brush. An effort was made to

locate as many as possible of the old chaining pickets. If a

more dot all od survey Is desired, re-cutting and re-chalnlng

will be necessary.

P R nES EN T AT ION OF R ESU LTS

The Induced polarization and resistivity results

are shown on the enclosed profiles. The results are plotted

In the manner described in the preceding notes and bount in

the following order with this report!

LINE

9 -* 00 E h 5 * 00 W 6 4 00 W 57 4 00 W

35 -f 00 W 60 4 00 W 27 4 00 W 69 4 00 W 33 4 00 W 81 ^ 00 W 36 4 00 W

Enclosed with the report also is a plan of the

property showing the lines laid out for the Induced Polarization

Survey.

The definite, probable and possible anomalies

aro marked with solid, broken bars and hatched lines respectively

SCOP!on the profiles and plan map. These bare represent the

surface projection of the anomalous zones as interpreted

from the location of the transmitter and receiver to electrode*

when anomalous values are measured.

Blnce the Induced polarization measurement

is essentially an averaging process, ae are all potential methods,

it is frequently difficult to exactly pinpoint the source of an

anomaly. Certainly, no anomaly can be located with more

accuracy than the spread length, I.e. when using 200' epreada,

the positions of a narrow body can only be determined to Ile

between two stations 200' apart. In this case, where the

target may Ile at a depth of 50' to 300', the anomalies appear

on all -three separations; therefore, while the centre of the

indicated anomaly probably corresponds fairly well with the

source, the length of the indicated anomaly along the line

should not be taken to represent the exact edges of the

anomalous material.

DISCUS^J.ON. OF RESULTS AND CONCLUSIONS

The area has generally very low resistivities

which increase to the west of the property.

Anomalous zones were detected on the following

lines and are listed in order of their priority:

L,lne 69 Wl An -j G 1.'; WI,Ine 33 W

-24 DON to 5 4 OON- 7 4 O OS find l -i OON

12 4 OON to 14 * O ONi.,lne l;j W - ;j? -^ OOS and 11 -f OON 1,1 no 9 l 'J - S -f 008

li should bo kept in mind tha.t a careful

comparison should be made between the electromagnetic,

ii.agnotic and induced polarization survey in their relation to

the geology, before drilling Is planned.

Respectfully submitted,

SCOPE MINING 6- EXPLORATION CONSULTANTS LIMITED

D. W . Sullivan, P. Eng.

Septornbor, I960 r]' o r C)U to, C )n t. a i' i o.

Warden T w

10

L (L

80054

Boost BOOS 5

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\ 8 0040

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,c L ALM.^LOG A.IJ.ON. ....MARLYELLOWKNIFE BEAR MINES LIMITED

MUNRO TOWNSHIP

LARDER LAKE MINING DIVISION

ONTARIO

Scale Sept. (966

Scope Consultants

Use flkone type of survey only4aA89SE816a 63.1962 MUNRO

900

Assessment Work Breakdown

1. Typeof Survey.................I!l)UC:tI)...POI.AHIZAT^

2. Township or Area ...................................J-fUMRQ..............................................................^

3. Mining claim numbers......L,.8QOl6,...~17.,....~19.,..e20.,...~23-,---.~24,.--34,- r^y...^ t--^B ) ..^..,...^J40.t .

..........................................................^^

,......................................... ............,,...p..........'./.'..........j...t.........................,....................,............. ........,................................................................................

4. Number of mi les of line cut ,.............,.............,.....,.........................^

* 5. Type of instrument used ....,,,,,!!?.9.!^aL^

* 6. Scale constant or sensitivity ...................................................,................................,,.....................,..,...,............................................................

* 7. Number of stations established ............................................,................................................................................. 1 ......................,....................

8. Summary of days worked ( details on reverse side )

Total technical ( include consultants, draughting etc. ................3.?K.*.25....X..7...~...22.5.*.75.........

Total line-cutting ( maximum 5 man doys-p^f-c-ig-w)-). l ... l ....................,.,,..................,..,...........,..,..........................................................

Total man-days ( technical plus line-cutting J...........................................................................................................................................

Assessment days credit per claim ................................22.5-75.,.t...20...-...10..1...days/claim..............................................

(Totol mon-doys multiplied .by ossossrriont foctor 4 divided by totol number of-cloims trover G od-)

9. Dot.d........^...^r?.!?..f.M7............... S i gn ed .......^'L/^- - " ^ L . G. PHKLAN

* Complete only if applicable Complete list of names, addresses and dates on reverse side

Use for one type of survey only

1. Technicol

Type of Work

Assessment Work Breakdown

Name o\ Address Dates Worked

rJeie.r...r...,S..cpp.e.J;jrn^

J.....Lyons,..TT,.S.cope...Mining.,,372 Bay.St,.^

..

Hours

.......so.....

........go---

........go.....

Totals

Consultants

Nome 8. Address Dotes Worked (specify in field or office) Hours Days

,..P.......Sul.Uyftn...-...^

Totals

Draughtsman, Typing, others (specify)

Name 8. Address Type of Work Dates Worked Hours Days

.Mninf,.,.J7;L,B.ax..S.t.*,.^^^

,MninRr.372,te,St.,.Ioro^

Totals ...25.8..M^..M. dayi

2. Line-Cutting

Nqme Address Dates Worked Hours Days

l

Totals

YE LLOWKNIFE BEAR MINES LIMITED

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GUIBORD TWP M-352

42A09SEei62 63.1962 MUNRO 200

THE TOWNSHIP OF

MUNRODISTRICT OFCOCHRANE

LARDER LAKE MINING DIVISION

SCALE: 1-INCH 40 CHAINS

LEGEND

PATENTED LANDCROWN LAND SALE

LEASES

LOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLY

ROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES

CANCELLED

Kc.

NOTES4Ob' Surface rights reservation around all lakes and rivers.

For status of summer resort locations and other subdivisions please contact Dept. of Lands and Forests.

DATE OF ISSUE

NOV 1 6 \i

ONTARIO OEPI. OF MINES

ONT. DEPT, OF M INES MINING LANDS BR.

THIS MAP FOR CHECKING PURPOSES ONLY - MUST NOT BE SOLO.

PLAN NO. M-376DEPARTMENT OF MINES

— ONTARIO —

WARDEN TWP M-397

l r l Mf, b j '-1654 7465!

L l L 40721 153321 80 V4980/348

52514 '58:866i© i E

M R0 i MRO

73450 6 I267

L jL 53953 5i948

9|6 A re ]52f 63

GUIBORD TWP M-352

63.1962 MUNRO

TRIM LJNL

THF TOWNSHIP OF

MUNRODISTRICT OFCOCHRANE

LARDER LAKEMINING DIVISION

SCALE: 1-INCH 40 CHAINS

LEGEND

PATENTED LANDCROWN LAND SAL F

LEASESLOCATED LANDLICENSE OF O CCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

C.S

S3?tt

NOTES400 Surface rights reservation around all lakes and rivers.

For status of summer resort locations and other subdivisions please contact Dept. of Lands and Forests.

ONT. DEPT. OF MINK MINING LANDS BRl t f A - .

MAP FOR PURPOSES ONLY NOT BE SOLD.

PLAN NO. M-376DEPARTMENT OF MINES

— ONTARIO —

l|IO ^s-iro

oz oi-cr

Q)^01

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YELLOWKNIFE BEAR MINES LIMITED.

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————————————————————————— . .———————————————————————

SCOPE MINING AND EXPLORATION CONSULTANTS LIMITED

INDUCED POLARIZATION AND RESISTIVITY SURVEY

ELECTRODECONFIGURATION

i i l \

FREQUENCY S ~*fi. 3

\ T* V — ^ /1/Yv X * f**Uy*vPLOTTING

POINT

Anomolous Zones

PROBABLE B B B B B B

POSSIBLE / / f / / //

DATE

APPFOvED

DATE

\

YELLOWKNIFE

ONTARIO

PROPERTY LOCATION MAP.

O LJOD

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Scote : l -- 2 5 m.

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—————

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S . P SURVEY-ANOMALY LOCATION

1

SCALE; r* 500

Sept. 1 966 SC OPE CONSUL T A N TS

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