\ INTRODUCTION i sAeesEeaes 63.2673 CARMAN 0^0

During the period February 3 to February 19, 1970, an

electromagnetic survey urns carried out on the property of Dome-Bnbine

Hines; Limited, 2Dw Floor, Guineas Tower, 1055 Wast HaeUnga Straat,

Vuncouvfir 1, B .C., by Shield fieophyaios limitnd,

ThB property eonaiete of 11 contiguous, unpatented mining

clalma numbered as follouia! P98561 to P9B36B inclualva, P101192,

P101193, end PinUOO. Cloima P9B561 to 98568 i nduaiva lira

recnrded in the name of A. Theriault, 150 Third AvanuB, TjLfflmina,

Ontario, claims P1Q1192 and 101193 ara rucorded in the name of

M. Lttchapelle, **39 idilaon Avanua, Timmins, Ontario, and P1Q1A08 ia

recorded in the name of E. Hard, 98-B Norman Street, timmins,

Ontario.' ' ! ' ' ' , '. i * "' . ' '. -' -' ' ' ' V :' - ' ' : i

A total of 129(J BtHtiona uiare eatabliahed on 16.9 milaa

of picket linea, A McPhat SS-15, 10pa^5000 cpa. vertical loup

electronagnotic unit UBB uaad for the survey (Sea Appendix 1 for

Inatruraflnt Data). ' '

ACCESSThe property ia located in the aouth-ctntral part of

Carroun Township, Porcupine Mining Oiviaion near the Carman*

lungmuir township boundary. Acceaa tp the property ie either via

es wintur rone! from South PorcMpine or via air from South Porcupine

Lakti to Nighthawk Lake, a diatanco of approximately tan miles.

PRLVICUS

Claim P98561 was pertly covered by a magnetic eurvey done

by Dominion Gulf. Mn Ot-her work, other than geological mappiftg

by government oganclos, haa been carried out on the property.

- 2 - -. ' - : :.:-- -.. - . . ;

'A magnBtomuter survey waa completed on the property in

December 1%'J, by Doffle-Uabine Minna Limited.

5U3LEKV. OF. THE PH

The geology of Corman Township and the Dome-Babine

property its presented an Ontario Department of Mines Preliminary

Map P. 356.

The property occurs on the nouth liMb of an eaat-north-

t'aatorly trending anticlinal etructure that crosses the central' .; ' '' ',' ' f' ' " ' "' ' -'

sector of Carman Township. The property is underlain by inter

mediate to felsic mRtnvolcanic rocks and iron Tarnation. that have"j ' ' " ' F' ' . -'i * 1 "t " . . . ." '. . 'H L '

bopn intruded by puridotite and dunite ailia. Diubaae dikes out

thu ultramafic intrusive and the meteyolpanic rock e. roat-diabaaa: ' \' - i . t - ' ' ' ' ^ . '

fnultiny occurc along two major etrika directione. Older faulti *;

having an ewt-nurthmaat Btriku direction are offeet by younger" ' '... ' h ' " '

faults tnwing a northwesterly atrike directlpn.

fJo mineralization of economic significance outcrop, on

the property. Some minor aabestoa occurs in the eerpantinized

ultramafic rocks.

RtSULTG Of . THl ..CLCCTRDHAGNtTlG.SUHl/Cy

Thn rtisultB of the coverage eurvey are presented on Map

1, attached to this report (in pocket). Four cunductora designated

A to O usre located during the survey. A discussion of each conductor

follows:

Conductor A; Conductor A uas picked up weakly from Transmitter

Location 2. T hw conductor uae picked up on high frequency only tin

linea 32ai to 3&U. Un the remainder of the linea the low and high

-. 3 -

frequency cruatjov/era ara from 1QQ to 200 faut opart. The ration

are pour ami the general correlation of the conductor axis with

e stream and auamp trend would suggest that the conductivity is

due tu ovorbunien conditions.

Conductor B t Conductor 8 wot, picked up wuakly nn linns 36U, 30U

and l+Eul. The conductor le continuous with Conductor C, however,

because Df the abrupt change in strike uuot nf line 36U it is, -- '* . ' ". .

discussed separately. The Inductor was picked up at the ende

of linea run from Transmitter LocBtions 1 .and 2. L.o to high

frequency ratios indicate poor to moderate conductivity. The source

of thR conductivity way bo biiply burled.

Conductor C; Conductor C is the ^ueterly continuation of Conductor.

B ond was picked up un linet 2W to 36Ui. Tho lo to high frequency

ratios indicate good conductivity and the intensity of the

readings would indicate a shallow depth of burial. The conductor

axis le generally parallel to the trend of the magnetic contours

in the immediate area.

fr Conductor t) is indicated on thR amp but is indefinite

because of itB location ot tha ends of linea ra Bd from Transmitter

Locations ^ and 5 because of the possibility of lieorifintation

erroru due to the poor lints cut on the property in that area,

The conductor axis has e strike parallel to the sons of

faulting inferred on the basis of tha magnetic dHu and ia probably

due tn tha Bheariny.

fi there,

Three single line croaaovara ware located during tha

survey at the following locutiona: Line 22klXH**5nS, Line 12W/

9*252, and Una BE/15+25S.

CliNCLUS.lt :NS A

Conductnro A, B, and C are ell possible bedrock eonductora

and should be detailed. No detail ia recommended on either

Conductor D or the three aingle atotion croBBOvera.

RE.bu.LT5.rjr THL DETAILED S

The reuulta of the detailed survey work are presented on

Hup 2 ( in pocket).

CONDUCTOR A '' ' : ;,"' ; : - ,. '

The detailed survey aubatantially modified the covaraga

survey rumjltu in the areo of Conductor A. Conductor A yaa out

lined during the detail work on linwa )Qj4 to 3BW. The lo/hi

frequency ratios indicate moderate to good conductivity* The' - : ;-^ " , - . . . -' f . -. ::,; -: -' '' : ' ;v -- ' ".''

dip tmQlei] ere lou, houiever, indicating aJaubatsntial (greater

than 300 feet) depth tci tha source of the conductivity. Line 30U

WHS rood f TOP Trsnamitter Location 2 with ,a coil separation of

600 feet. The anomaly uaa picked up uepkly which aubatantiaiea/if-'' ' : . ' ' . ' " . ' -

the inference nf u cunnidarabU depth of burial ao the remainder

of tho linua mere read from Tranamitter Location 1 with coil

cepHratlon yreatar thnn 1000 faet.

The conductor axis car ra la toe in general with tha

metavolcariic-ultramBfic rock contact inferred on the baaia of tha

- 5 ~

eurv/ay. The strongest part of the conductor la the section

butuman lines 3 W am) 3&U.

CONDUCT DM S O and C

Conductoro B and C ara a 'continuous zona marked only by

en abrupt change in atrike heat of lino 3BU. That part of the

conductor west of 36^ lo deaignated Conductor O, the remainder of

the zono Conductor C,

The lo/hi frequency ratios for Conductor fl indicates

moderate to excellont conductivity and the dip ahglea indicated a

relatively shallow depth of burial. The strongest croaaover and

tha bust ratios are preeent on line **Q5. .

^hc lo/hi frequency ratios for Conductor C /indicate* poor

to rntxiurnte conductivity. The dip angles Indicate relatively

shallow depth of burial. The beat zone of conductivity along

Conductor C occurs be tuaan linea 26tj to 30U.

Dn tha hnsio of tha naQnatic data it ia concluded that

Conductor C ia caused by a sheer rone. The area between linaa

26W and 30U may ha of significance, however, bacauae of the higher

conductivity indicated in that area.

CUHOUCTOMS E. F. fi and H

Conductora t and F are single line lo frequuncy croaaovara,

The conductors ara probably of no economic aiynif icunoe.

Cunductor O IB a single line hiyh frequency croaaover

and is probably due to conductive overburden.

Conductor F ia a weak, single line qroaapvar. The ratioa

indicote poor conductivity. The conductor ia probably of no

economic significance.

* 6 -

Comiuctora A, Q, and C are budrock conductors af potential

economic significance. 'i .Conductor A occurs along e metavolctinic-ultramnf lo

intrusive rock contact and- tp probably ut a depth in exceaa of 300

feet. The contact zone should ba tented by drilling.

Conductor Q ulau occurs along an Inferred wetavolcanic-

ultrnmafic intrusive contact but la probably relatively shallow

in depth. The contact zona ahould ba teatad by drilling.

Conductor C cnrrelatea with a fault zona inferred on the

bBsie af the 'magnetic data. That part of Conductor C between

linea 26'J and 30U diepleyc batter conductivity than the remainder

of the zona and correlates with a emo l l magnetic anomaly O2UD

gammua at 3?ui on the baseline). Thia part of the conductor ahould

bv tested by drilling.

Three drill holes ere recommended to tcet Conductore

A, 8, end C.

HOI j NO. LCCA Li 'CAT I j- 'M SEAR I MG pit* UINOTH

1 ,3WX13*i*ON 195" (True) GO* 800'

Z 39*I*5UJX1*65N 200* (True) 60" **50'

3 3UuV2H5N 1BD" (True) **5* **OQ*

The locations of the proponed holes are indicated on

Map 2, ' ; '"'

Further drilling will ba dependent on the reaulta of

the recommBndad holes.

-7

If encouraging results are Encountered in tho r o corn-

men do d drill program then further fllRctromngnutic survey work

should be carried out na fullouBt

(a) Conductors E, F, G, and H should be detailed

(b) An i? ri k t-u) a f* t, 2QQ fout grid Bhould be ostfibllDhud betueen lint? 12uJ and the eoet property boundary. Coverage surv/oys ohould be cowplatad and any detailed unrk required should be carried out.

Respectfully aubraittad,

liHILLU BIOPHYSICS L lHltEO,

Timmins, Ontario, P. T. Ooorgs, P.

February 25, 1970. Consulting'QvologUt

I, Pater T, iienrye, residing at 391 John Street, Timmine, Ontario*

n coneulting geologist with office at 26 fine Straat South,

, Ontario, do hereby certify that:

I attended ijueen'a Unlveraity, Kingston, Ontario, and greduntBd

with en Honouro Q. Se. degree in Geological Sclencee in 198** and

I hove completed tuo yeore of poet greduate etudiea at Queen'e

University, KinQeton, Ontario.

I am e Hember of the Geological Association of Canada.

' * ' - ' " ' t ,

I am e Profeanionnl Cnginaer ^egiatered with the Aeaooiotion of

Profaeeional tngineera of the Province of Ontario.

I hove no interest either directly or indirectly in the ehoroB

or sticuriti^a of Domo-Bohine Hlnea Limited.

, Ontoric.', f3 . T. Qeo^e,

Fehruury 25, 1970. Goneulting

A P P E, N D l X

INSTRUMENT DATA AND SURl/EY HETHPQ

EUCTRPHAGMETIC SURVEY

Any alternating magnetic field will induce an alactrictl

eddy currant in the Medium through uhich the Magnetic field

paaaea. If a source of an alternating magnetic field ia located

near s conductive body anomaloualy atrong 0ddy currente will be

induced in the dapoait due to ita high electrical conductivity.

Electrical currents induced in the conductive body will produce

a secondary magnetic field proportional to the intanalty of currant

flow.. .' i " '. f

A reeaivar coil tuned to the frequency of the tranamit-

tlng device will pick up both the directly tranamitted algnal and

tho eddy currant aignal.

The electromagnetic unit uaed in thia survey ia a McPhar-, ' . . , ' . . ' T J/"".

unit and consiato of a vertically mounted, jnotor-generftor

powered tranamitting coil operating at fraquenciaa of 5000 and

1000 cpa. and a racalving coil, tuned to the tranamitting fre-

quanciea, an inclinometar, an amplifier and a headaa*.

Throughout the aurvay, the tronamittar and receiver ware

aaparated by diatancea of **00, 800 and 1200 feet. The plane ofj . ' : ' : j i' 1 ' -' - \ ' ;'i ' -' '''

the transmitter coil uaa oriented ao that thetrenamittor waa

verticil and painted towards the receiver. Orientation wan ob*

tained using a plnte on uhich predeterffinad redaivar poaitiona

were plotted. Gtntiona ware read at one hundred foot intervale.

'At nil time*, the receiver ;i||f*a| to\\t**Mi^^i^^^'.'\

obtained are dip unglae, meaaurad in degraoe. The dip anglea art. . - ' ", '-' ', .' t - . '. . K ^j.'; ^ . - ./-s

obtained by firat orienting tho receiver coil in the plant bf tha

" li -

magnetic field by rotating the coll about a vortical axis until a

null or minimum signal lo obtained, and then rotating the coil

about a horizontal nxia until s null or minimum aignal le obtained.

The on y H; uhich tha nugnotic fiald mukea with the horizontal la

rucordQtj au B "dip" or "tilt" angle. In tha abaanca of a con

ductor the dip angle uiill he zero aince no aacondtiry field la

present. In tha pruaftnce of a conductor, the axle qf thn receiver

c'il points townrdB the conductor and the plane of tha coil away

from thn conductor. In thu presence of D .conductor, the eeCDndary

magnetic field is usually dleplnced from the primary in-phane aa

well as direction so thot the total field le BlUpticolly polarized*

Tht; receiver cannot then be nulled completely but a minimum aignal

can be obtainod, tha width of thn mlnimurrt being an indiootion bf

the phaiiB displBComtjnt.

Tho tilt enyles ara plotted aa profilea, the zero or

"croea-nvBr" point indicating tMn focus uf the conductor axin*

Once a conductor axia haa bean eatnbliahed, tha trana-

mitter is aet up over the conductor and linea urn read on both

sidi!9 of the trflnuraitter nnd the conductor axle la triacml out by

"leap froQyinQ" from "croasj-over" to "croaB-over" .

t .JOB ra t .in .p i r raguHnc i e B t 1000 and 5000 cyclaa par second.

3ftnPJl 20"0 font separation betwoon trtmanitter tind rnceiver for B i 10 dnurcu null width.

Depth ..of. ilxplor^ion; Roughly half the diatance between trans-mitter and receivsr. *

-lil -

Tranamittpr foujur Supply; 500 watt alternator driven by o 1K M,P.gasoline angina.

Ueiflhtst PackbQHrd-mounted engine generator 48 Ibs.Transmitter coil on packboard 1*9 Iba.Coil mounting pola and apruadar bar 22 Iba.Receiver 7 Iba.

42A06SE0009 63.2673 CARMAN

INTRODUCTION

During the period December 5 to December B, a magneto

meter aurve\, wae carried ciut on tha property of Dome-Babine Mines

Limited, 2DU1 flour, Guineas Tower, 1055 UeBt Hastings Street,

Vancouver,1, B.C., by Shield Geophysics Limited.

The property consists of 11 contiguous, unpatented

mining claims numbered as follows: P9B561 to P9B56B inclusive,

P101192, P10193, and P1QUOB. Claims P9B561 to 9B56B inclusive ,

are recorded in the name of A. Theriault, 150 Third Avenue,

Timmins, Ontario, claims P101192 and 101193 ara recorded in the

name of M. Lochapelle, ^39 Wilson Avenue, Timmins, Ontario and

P10UOB is recorded in the name of E. Mord, 9B-B Norman Street,

Timmins, Ontario,

A totel of 1659 stations were established on 16.9 miles

of picket linos. A Sharpe M.F.-1 fluxgate magnetometer was used

for the survey, ,. ; .

The linecutting was dons by Ingemar Explorations Limited,

362 Seventh Avenue, Timmins, Ontario.

LtiCATI.tJN AND ACCESS

The property is located in the south-central part of

Carman Township, Porcupine Mining Division near the Carman-

Langmuir township boundary. Access to the property is either via

a winter roed from South Porcupine or via air from South Porcupine

Lake to Nighthawk Lake, a distance of approximately ten miles.

PRtVIOUS UuRK , - ,, ,

Claim f 90561 was partly covered by a magnetic survey

done by Dominion Gulf, No other work, other than geological

mapping by government agencies, hBB been carried out on the property.

- 2 -

GEOLOGY UF THE PROPERTY .

The geology of Carmen Township and of the Daroe-Sabina

property is presented on Ontario Department of Minna Preliminary

Map P.356.

The property occurs on the south limb of an Bast-northeast

erly trending anticlinal structure that crosses the central aector

of Carmen Township. The property ia underlain by intermediate to

felsic metavolcanic rocks and iron formation that have been intruded

by peridotite and dunite Bills. Diabase dikes cut the ultra*

mafic intrusive and the metavolcanic rocks. Post-diabase faulting

occurs along tuo major strike directions. Older faults having an

BBSt-northeaat strike direction are offset by younger faults

having a northwesterly atrike direction.

No mineralization of economic significance outcrops on the

property. Some minor asbestos occurs in the serpentinized ultra

mafic rocks.

RESULTS DF THL MAGNETIC SURl/LY, f. i, ' ' -.

The survey was carried out using a Sharpe M,F ( 1 fluxgate

magnetometer (6ec Appendix 1 for 1 instrument data). The results

of the survey are presented on thjB attached map (in pocket).

The magnetic background on the property is 1500 tp 20130

gammas. The magnetic relief is approximately ^0,000 gammas

(155 to ^0,000 gammas).

The interpretation of the results is difficult in that

there ia no definite correlation of magnetic highs with areas

known to be underlain by ultramafic rocks and magnetic loys with

areas known to be underlain by intermediate to felsic matovoloanic

- 3 -

rocks. Fnr example the magnetic low in the southwest corner of the

property is underlain by outcrops of felsic metavolcanic rocks

whereas the magnetic low south of the baseline in the line 2kU to

28U area ia underlain by ultramafic rocks.

The interpretation of the magnetic results has been based

on known geological data from D.D,M. Preliminary Hap P.356. Where

no geological data ia available, magnetic highs are assumed to

reflect underlying ultramafic rocka and magnetic lDUB are assumed

to reflect underlying felsic to intermediate metavolcanlc racks.

The central part of the property ie underlain by ultra

mafic rocks that hove intruded the metavolcanic rocke. The local

magnetic highs within the area inferred to be underlain by ultra

mafic rocks are believed to be due to concentrations of magnetite

formed during the process of serpentinization of the ultramafic

rocks. The cause of .the magnetic louis in the central part of the

'.li 1 . . .

area is not known. - ,

A zona of faulting having a northwesterly strike direction

has been inferred in the east part of the property. Strike Slip

movement would appear to be approximately 600 feet In a left-hand

direction. The magnetic high that parallels the fault zone along

the northeast boundary of the fault zone is believed to be due to

concentrations of magnetite formed during shear-imposed serpen*

tinization.

A parallel fault has been inferred to cross the southwest

part of the property due to the abrupt termination of the iron

formation inferred in that area.

An older fault having an easterly strike has been inferred

to cross the central part of the property.

- f* - '.:; ; .-

This fault IB baaed on offsetting of the magnetic highs end the

presence of an electromagnetic conductor parallel to the baseline

between linsa 6W to 36UI.

CONCLUSIONS AND REGDMMENDflTIDNS

The property l a underlain by intermediate to feleic weta-

volcanic rocks that have been intruded by ultramafic rocks. A zone

of iron formation has been inferred in the southwest sector of

the property. i , ;

The magnetic aurvay has aided in the interpretation of

the knouin geological data, has outlined the local extent of the

ultramafic rocks and has indicated the presence of a number of feult

zones.

It is rBcamrnnndnd that a vertical loop electromagnetic

survey be carried out with the objective of testing the property!

particularly those areae underlain by metsvDlcanic-ultremafic

intrusive rock contacts, for the possible presence of sulphide ;

mineralization* :" ;

It IB recommended that additional lines be cut in the east

part of the property. The lines should be cut in an east-ueet ,

direction and ahould run fron line 12U to the east property boundary*

Respectfully submitted, V

SHIELD GEOPHYSICS LIMITtD,

Timmins, Ontario,

December, 1969.

P. T. Gaorjje, j'.Enjj.,

Consulting Geologist.

A P P L N D I. X

INSTRUMENT DATA AND SURVEY METHOD

MAGNETOMETER SURVEY

A Sharpe M.F,-1 fluxgate magnetometer uaa used in the

magnetic survey. This instrument measurae the vertical component

of the earth's magnetic field in gammaa. Base stations for de

termining the magnetic diurnal variations mere eatabliahed along

the main base line at 100 foot intervals. Magnetic readings were

taken at 50 foot intervale, along the cross lines.

l

SHIELD ' 26 f ine

sQ 0)

LIMITED th

ST CLASS RE CI ASSE

NT. F. ki. Matthews, Supervisor, Kining Lands Branch, Cnturiw. wEp^rtiT.snt ef Mines,Parliament Buildings, TDHGNTC, 'CWT.^RIC.

SHIELD^tCPHYSICS LIMITED 26 Pine Street South

, Ontsric

Mr. F. '.J. Matthews, Supervisor, Mining Lands Branch, Ontcric Dspartmart of Mines, Parliarrent Buildings, TORONTO 1 82, ONTARIO.

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