53Be9NW0018 53B89NWaai3 SKINNER LAKE 01CD

REPORT

ON

VLF EM AND MAGNETIC SURVEYS

OPAPIMISKAN LAKE AREA PROPERTIES

OF

493217 ONTARIO LTD.

FFR 2 2 1982

MINING LAND* S

(SEOCANEX R. Gillick Geophysicist January, 1982

S3B09NWe*18 53Ba9NW8813 SKINNER LAKE

TABLE OF CONTENTS

010C

SummaryIntroduction

GeologyPrevious WorkPresent ProgramFigure i - Location Map

Results and InterpretationOpapimiskan Lake GridLibert Lake Grid

Neawagank Lake Grid Conclusions and Recommendations References Appendix

*- Opapimiskan Lake Grid - Total Field

Page

12

3346

7789

10

12

Magnetic Survey Map"S2 - Opapimiskan Lake Grid - VLF Survey

Map 3 - Libert Lake Grid - Total Field Magnetic Survey

Map 4 - Libert Lake Grid - VLF Snrvey

Map 5 - Neawagank Lake Grid - Total Field Magnetic Survey

Map 6 - Neawagank Lake Grid - VLF Survey

(Back of Report)if H

it n

H n

SUMMARY

During October, November and December, 1981, linecutting,

VLF Electromagnetic and Magnetic surveys were carried out over

three properties totalling 123 unpatented mineral claims in

the Opapimiskan Lake area, approximately 75 miles north of Picjkle '

Lake, Ontario. The Opapimiskan and Libert Lake groups are located

directly north and south of the property of DOME-ESSO-INCO-i

LACANA on which a major new gold discovery was announced in 1981.i

The Neawagank Lake group is 25 miles east of the Dome discovery

adjacent to a property where previously discovered high grade

gold showings are currently being explored by INCO.

All three 'properties are underlain by volcanic and sedimeijit-

ary rocks of the Caribou Lake greenstone belt. Oxide and sulphidej

facies iron formation, similar to that hosting the DOME ET AL

deposits, are indicated to occur on all three properties.

Results of the magnetic surveys confirm the occurrence of!i i

iron formation on each of the three properties. Strong to rnocjl-

erate VLF EM conductors, possibly caused by sulphides, are as|

sociated with the iron formation.

Since the DOME ET AL gold occurrences occur in sulphides

within iron formation the zones delineated by the present suryeys

are considered to be high priority targets and further explor^-

tion, including geological mapping, prospecting, trenching anJ3

diamond drilling, is recommended.

- 2 -

INTRODUCTION

The property held by H.J. Hodge and associates under the

corporate entity 493217 Ontario Ltd. is comprised of three sepj-j

arate claim groups located approximately 120 kilometres (75 miles)

due north of Pickle Lake, Ontario (see Fig. 1). Two of the

groups (Opapimiskan Lake and Libert Lake) adjoin to the north

and south respectively, to property held by Dome Mines and partners

on \vhich a major new gold deposit was recently discovered. Thp

third group {Neawagank Lake) is located about 40 kilometres (2ji

miles) east of the two above-mentioned groups, in the same grepn-

belt, adjacent to property on which several high grade gold i

showings have been discovered.

jThe properties are accessible by rotary-wing or fixed-

wing {ski/float equipped) aircraft from Pickle Lake. There is

also an all-weather gravel road from Pickle Lake to Windigo

Lake which passes within 32 kilometres (20 miles) of the Liberb

Lake group.

- 3 -

GEOLOGY

The Opapimiskan group of claims is located in the southern

portion of a narrow., arcuate greenstone belt about 130 kilo

metres in length. Just south of Opapimiskan Lake the belt is

split by granitic intrusives into a short, narrow south-trending1

lobe passing through the Libert Lake g*roup, and an east-south-i

east trending lobe extending as far as and including the Neawa-j

gank Lake claims. The belt is composed of mafic to intermediatel

volcanics with a central synclinorium of meta-sediments. Severjal

prominent NE-SW trending faults cross-cut the belt south-east

of Opapimiskan Lake.

Banded oxide and silicate (magnetite, chert), iron formation

occurs within the belt and, significantly, in the Opapimiskan

Lake area, the same iron formation which hosts the gold on the

Dome property appears to extend well into the north and south

claim groups held by Hodge and associates. Furthermore, in tht

Libert Lake group a gold bearing zone has been discovered as is

described later in this report.

PREVIOUS WORK

Prior to the present program no geophysical work had been

carried out on the Hodge properties. As yet, none of the threes

claim groups has been prospected in detail, nor have they been

surveyed geologically or geochemically.

- 4 -

PRESENT PROGRAM

During October, November and December of 1981, linecutting,

magnetics and VLF EM surveys were carried out over the three

claim groups.

The surveys were carried out to map iron formation and

delineate bedrock conductors on the properties as well as to

obtain general structural and lithological information. Gold

mineralization on the Dome property is known to be associatedj

with, sulphide mineralization within oxide facies iron formation.j

The meterage breakdown for the work on the three grids is

as follows:

GROUPS

Opapimiskan L.

Libert L.

Neawagank L.

Total

LINECUTTING

51

58

53

162

km.

km.

km.

km.

MAGNETICS

44

54

46

144

km.

km.

km.

km.

VLF-EM

44

54

46

144

km.

km.

km.

km.

Lines spaced 400 feet apart were cut to cover each of the

claim groups. On the Opapimaskan Lake and Libert Lake groups,

the lines were oriented east-west and on the Neawagank Lake

group, line orientation was north-south.

The VLF EM survey was carried out using a Geonics EM-16

unit tuned to receive signals from the transmitter at Cutler,

Maine (17.8 KHz). Readings of in-phase and quadrature were

taken at 50 foot intervals over anomalies and at 100 foot in

tervals over non-anomalous areas. The results were plotted on

- 5 -

plan maps of the grids (see Maps 2 ,4, and 6).

The magnetic survey was carried out with a Geometrics G816/

826 prot6n precession magnetometer. Readings were taken at

50 foot intervals over anomalies and 100 foot intervals in non

anomalous zon^s. The survey was performed in a looping fashion

and drift corrections applied in the standard way. The survey

results were plotted and contoured {see Maps l, 3, and 5).

Opapimiskan Lake Property

ORIGINAL DISCOVERY

OME-INCO-ESSO- LACANA

NEW DISCOVERY

LEGEND

Iron formation

Volotnloi

8 a dim* nt t

Ulgmatltt

Ooid, Bulphid* ihowlng*

v] DOME-INCO-E880-LACANA

INCO i

COMINCO - ^

[ j CANADIAN OCCIDENTAL

C ^1 493217 Ontario Ltd.

Neagawank Lake Property

493217 ONTARIO LTD.

REGIONAL QEOLOQY , MINERAL 8HOWINQ8 li PROPERTY HOLDINGS AftIA OF DOUI-INCOfltlO-lACANA tOLD DiaCOVIRY,

OPAPIMISKAN LAKE PATRICIA UININO DIV. ONTARIO From ODU U*p. f tt 1 1 Pitt*.i——p———i-.

Soil*:! 1*"4 Ulita_____Figure l__ __

- 7 -

RESULTS AND INTERPRETATION.——————-—,—-—————m———,——.——————.————-—M,. ,- ,., .— l

j

OPAPIMISKAN LAKE GRID-

Government aeromagnetic data indicates that the Opapim

iskan Lake grid is located near the northern edge of the ;ightljpj

folded region of iron formation extending southward and eastwarp

through the Dome 'discovery zone'. It is apparent from the

ground magnetic results (see Map 1) that this iron formation

penetrates into the Opapimiskan Lake grid near the south-east

corner for about 1,600 feet. It remains highly folded and dis

turbed in this area.

The relatively large magnetic anomaly amplitudes (upl

to 7,300 gammas) in this area and general lack of high amplitudei i

VLF anomalies indicate that the magnetic anomalies are almost j

certainly due to magnetite iron formation and not pyrrhotite.

Two lower amplitude magnetic ridges are evident north

of the iron formation. Both are very linear and probably re

present dikes, perhaps intruded along the volcanic-metasedimentj

contact in this area. This contact is evident as a change in

background magnetic intensity of several hundred gammas in the

north-east part of the grid. The sediments lie in the area ofi

lower magnetic intensity and the contact extends almost linearly.

from about 24+OOE on line 48N to 60+OOE on line 0+00. A partially

defined magnetic peak occurs on L 28N at about 45+OOE. There

may be some weaker iron formation within the metasediments in

this region.

. 8 -

A second system of less contorted magnetic anomalies

crosses the western portion of the grid from south to north.

This zone is not apparent in the govhrnment aeromagnetic map of

the area due to the north-south flight lines (i.e. paralleling

the geological strike). Peak magnetic anomaly amplitudes of

about 5,000 gammas are somewhat smaller than the magnetic peaks

in the eastern part of the grid. Several of the magnetic ridgesl

in the west are directly associated with large amplitude ( > 100%i

peak-to-peak) VLF anomalies suggesting the possible presence of

massive pyrrhotite (eg. conductors C,E,G and I on Map 2).

Significantly, the original discovery of gold on the

property to the south occurred at the 'No. l Quartz Vein 1 located

between Opapimiskan Lake and Thurston Lake close to the southern

boundary of Hodge's Opapimiskan-property and apparently on strike

with the western zone of conductors on the Opapimiskan grid.

LIBERT LAKE GRID

The most prominent feature of the magnetic results oveij

the Libert Lake grid is a relatively narrow (800' - 1000') zon

of increased magnetic intensity entering at the north end of

the grid and striking due south as far as line 48-fOO S (see Mafj

3). Large magnetic peaks (up to 10,000 gammas) indicate that

this zone is likely a continuation of the iron formation found

to the north on the Opapimiskan and Zeemel Lake areas. Some

localizations within the Libert Lake magnetic zone exhibit the

same tight folding however, in general, linear magnetic features

- 9 -

appear to dominate.

VLF conductor A strikes along the magnetic zone for a

strike length of ~-4,400 feet. Peak-to-peak in-phase amplitudes

associated with conductor A are as high as 84%. The conductor

itself does not appear to have a magnetic signature. Conductors

B and C have less distinct VLF signatures responding only as

secondary inflections on most of the profiles. Conductor B is

directly associated over most of its length with a 9,000 - 10,000

gamma magnetic ridge. The conductor here may be the magnetite in

the iron formation.

A gold 'bearing zone was discovered and trenched between

lines 36S and 40S at about 7+OOE {see Map 3 or 4). The zone

consisted of sericitic quartz bearing shear zones with weak magn

etite-sulphide iron formation. Samples taken over 9 feet, assayed

.19 oz. per ton gold. The trenched zone is associated with a

N-S striking magnetic ridge with an amplitude of about 3,500

gammas. There is no associated VLF response.

NEAWAGANK LAKE GRID

A zone of increased magnetic intensity crosses the south

ern third of the Neawagank Lake grid striking NE-SW. Isolated peaks

within the zone reach maximum peaks in the 9,000 gamma range. Magn

etite iron formation is the probable source.

Two parallel, well-defined VLF conductors (A and B) strike^

along the magnetized zone. Conductor A exhibits good, consistent

- 10 -

anomaly signatures along its entire length. Peak-to-peak in-

phase amplitudes range from 3(^ to 40%. Depth estimates using

several of the better defined anomalies average about 18 metres

(60 feet). Conductor A does not have a magnetic signature itself

and its relation to the magnetized zone is uncertain. The long

strike length ( 1,800 metres {6,000 feetQ ) and consistency of.

Conductor A suggest a formational conductor (possibly graphite)

or a fault. Conductor B exhibits a more variable character. It

is close to the surface on lines 28E and 32E and passes through :

several of the high magnetic peaks. A massive to semi-massive

sulphide within iron formation could be expected to give such a

response.

A second weaker magnetic linear crosses the grid from

east to west at approximately 8+OON. Peak amplitudes are -1,000

gammas. No conductors appear to be associated with this anomalyj

for most of its length, however, weak positional correlation exists

at the east end of the zone between the magnetic trend and con

ductor D.

Of several high grade gold showings discovered in 1943,

one is reported to occur on the Hodge property. The approximate

location of this showing is shown on Maps 5 and 6.

CONCLUSIONS AND RECOMMENDATIONS

Folded iron formation and associated conductive zones are

found on each of the Hodge properties. In view of the known

- 11 -

association of major gold mineralization in this area (Dome

property) with disturbed iron formation and sulphide mineralization,

the geophysical results over the Hodge properties are extremely)

promising.

It is recommended that the three properties be prospected in

detail and mapped geologically. Furthermore, it is recommended

that selective drilling or trenching be carried out on the

labelled conductors on Maps 2,4 and 6, based on the results of

the prospecting and mapping.

Respectfully submitted,

R. Gillick Geophysicist

- 12 -

REFERENCES

.

Hodge H.J., 1981 - Report on (told Properties Adjacent to Dom^-Inco-Esso-Lacana Discovery, Opapimiskan Lake Area, Ontario - P..ivate Report.

Andrews, A.J., Sharpe, D.R. and Janes, D.A., 1981 - PreliminaryReconnaissance of the Weagamow - North Caribou Lake Metavolcanic Belt, Including the Opapimiskan Lake (Musselwhite) Gold Occur rence, in Ontario Geological Survey Mise, Paper 100, Summary of Field Work 1981.

Thurston, P.C., Sager, R.P., and Siragusa, G.M., 1979 - Geologyof the Winisk Lake Area, listrict of Kenora, Patricia Portion, Ontario Geological Survey Report 193.

Robertson, C.P. 1945, Report on the Forester Lake Area in Asses sment Tiles, Ontario Geological Survey, Sioux Lookout, Ontario.

Ayres, L.D., Bennett, G., and Riley, R.A., - 1970 - Geology imdMineral Possibilities in Northern Patricip District, Ontario, Ontario Department of Mines, Miscellaneous Paper 28.

53Be9NWeai8 53B09NW0ei13 SKINNER LAKE

!'' '''V. .1, Gv-lr^ical,

C. ' '.ii .' il . ,'l Gxpciidiluics)

,.. ,.. .The Mining Act

900

m -;1i in liOmr - F'!*-v,(; typt O i I irml.

If nijinbttf ot mining c! ; ' nii ir 1*.o. j J txcbL't.s space* on Ihii form, oUuch o \ M,

Note: — Only dnyk credits cfllcvJ'ftlfrd in J he "E xpi.'nditutet" ipclion jniy be eni^*'! in i he "t xpend. Di* y i Of/' rnlunirtj

— Do dot uu- jhdfVd iirr-ai ht-'ow.

Totel Day* Cftdili may be a pportioneo At the claim holdvr't cnoic*. Enie' numbe' of days crediu p*r cloln^ *clect*d in colyrnnt *t right. " -

- ... , VLF,. Magnetometer s Linecuttingv.la.,n HolOor(s) * .... ---

- ........... .--..Jj9321Z.Ontario. .td

1 C - .vMi 1 . p O' Ai fi A

Skinner Lake M2707'''otpJtciO' fc Ln.eru.ft •••o.

T1165

s^9irj....^O...Univer.sity-.J\Yenue J ..JorontoJ Ontario M5J 1T1.................. H, J, Hodge..NtiTt* and Adrlre** of Author (o) Goo-Tt cr.r.ica

Credits Requested per E^ch Claim in ColuSpecial Provisions

For first survey:

Enter 40 days. (This includes line culling)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

PATRICIA MINING C[S E(8i8 WE

FEB 1 f 1982A.M. P''-'7i8|9iIO|llil2i 1 12|3|^

Airborne Credits

i

Note: Special provisions credits do not apply to Airborne Surveys.

Inc.... ..lepon)

3fi Avenu&j..nns at right

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. Mapnttom.,., ^^

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)IV. ' N ''n' to n,.,,. i

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L^C her

fioo'o c*l

tJllfi !•rjfjy.f miCBi

1 Days per

t Jccir o mtl pn e t ic 'i i

Radiomeu i c

Expenditures (excludes power stripping!

L/—1 A

Type o) Work Perlormed

RpODhvsirnlPirlo'rntO on C**'rn(i}

-BCL55S8Q2Lr..558853 ( I ne 1 uswej^

Calculenon o* Expenditure Dayi OeOiU

Toifcl Expendhuret

|S H- 15

Total Days Credits

L.. JInitruciiont

Js

PjJt.0) Su/.'fy.l'rom f, LO) IToia! Miles c* lil

20,10,81 0111 81 , n Qj Day j Mo. j Yr.' Day j Mo. J Yr. j j3(J , y

Q.n±i-BQVJ...Dntar ofining Ciaims Traversed (List in numerical sequence)

Mininp Claim

Pa ! 558807i

09101112

i 14L 15*— 1 6

171819

i- - 20 l21

L-.—22..2324 1

i 25' ! 26

272829

Expand. Deyi Cf.

— -—

- ——

30

* Cut

3 .

Mining Claim Prefix f Number

Pa 558831^ __ 3.2

34~-—

35363738394041424344

: 45

47—

48 ^

4950

^ 51,——-^.-

Totil numbe' of mining c'amis cowed by inis report o* work.

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— ....

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——

47

———————————————k————.———————————————————————————— ,————————fv———————————————————————* ^—————"—————————'————————' heieby certify that l have a personal and intimate knowledge of the facu set lortfv in the Report of Work annexed hereto, having performed the wor,.

or witnessed time during tnj/or alter its complelion and the annexed report is true.

K*mf and Poitll Address O( Pirson Ctrlilying

H..-.Ja-.}iQte^-J^Jl.(L-^JJnlyej^li^.AyfiDiifiv. Toronto, Ontario N5J-a'TlDate Certified

12 Feb. 1982uM)

^^^^^^^^^^^^^^^MBe^^^^^^^^^^^e^^^^e^fc^ei^^i^i^^^e^i^^^^^e^i^^^e^^ne^^n^^^e^eiB^i^^^e^e^e^^^^B^B^B^B^e^B^^BB^B^^^p^B^^e^^^^^e^B^^B^^B^B^i^B^^^B^B^^^^^^e^^^i^^^^w^^^^^^^I^H in the "Expend. Dfiyi Cr." Cllumni, I^H^^^^^HK Tho Mining Art — Do not use shaded areal below.

P

^1 ,. ^93217-^ddfsii

iurvey Company

--^^.^......H^J,.Name and Addre** of Author (of C

R. HI! 11 rk. W

agneiometer.&Ainecutting . ........... iSkinne,

I-ty. Avenue.,. Jorontc Hodge-lnc........ ............. ...,.. ..... ........ ........ ..

'LoJf;.eJ12ZQZ—5roipector'i uTcffncB No.

T1165

^-Ontario ....... .. ......M5.J...1T1^\^\o * 5 L^v*^Vom 5k V5Day ! Mo. j Yr. Day

3eo-T*chntcel report)

19 . ludop. Avenue. North Rnv. Ontario

———— —

.. —

-, -- |Tot*l M:M of line Cut

iii- 8J- ! 30 98

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)

j

i

ii \

Special Proviiioru

For (irtt survey:

Enter 40 days. IThu includes line cutting)

i

For each additional survey: , using the same gnd:

Enter 20 days dor each)

Man Days

Complete reverse stele snd enter totallsl here

A^hotne C'OOHi

Note: SjH'C'iii p'ovsions credits do not apply to Airborne Surveys

Geophy.ic.l j D'^. P*H i Cllim l

•Electromagnetic 1 ..p. l

- Magnetometer ; Of^

. Ra.iom.tr.c J

- Other

GooiOQicftl

Geoch*n\ical ijl Davt pe-

Gftophystca! ' r (a j m

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Geological

Geochemical .

Days P*"

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Mflgn*3Ton^eler i

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Expenditures (excludes power stripping)

fifiophvsirnlPtif to"iioci on C'a'mlsl

As per attached

OIK u'diion o* E * penoitu t e Oov*

Total E xpe^iJtUi'ei

liGf ltd .is

Total Day* C'Cd'i*

-r 1 5 ^

1 nil r uci tO"J

Totdt Day* C'*dns may DO apportioned at the claim holder's choice. Cute' number of oayt credit* per claim selected •n coluntns ai right, S

Dare Ree

M Fph. 1QR?

/f^rdeqHo/der OfJXytXt (Signature^M^

Mining ClaimPrefix Number

Pa 5588074Jfe 08•1..&. 09

,:; 10. ^' - 11. ...,..,r 12-^ .........i3...' . 1 15;; '-j 16

,^..,,,.,... j ••-- -— -— — --' : 18''•"'• ; "i . 19. .

20' ' ......21......

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27 28 29

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y*?2?y^.t-"i^'

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For Office Use Only

M r n i n g ClaimP^e^ix H Number

Pa - 5588313233

' 35 U......36..i.... 37. L. ...J.8.."~. TWL."

—

....

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: Sl. ......48.

; 50 51 52 53

TotO' nunitjer O( rninnig cUi."!i cuve'oti by thu

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Total Days Cr. Date Recorded Mining Rocorcle' Recor.Jed

Date Approvud as Ancorctecl iBrancn Director

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S

^

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Certification Verifying Report c/i^/brk ZJ

\

i

1 hereby certify that 1 have a persona) ond intmviie knowledge of the lads set forth m the Report of Work annexed hereto, having performed the v\ or witnessed same during and/or after its completion and i he annexed report is true.

Name and Potia) Audrots or Person Certifying

...H, J. Hodge,... #91.0... .^0 .University Avenue, Toronto, Ontario fEJxLTlDite Cerlilmcl -fyftt

ork

^ Ministry^ Geotechnical *"* ^i ?J P?™ Re Port ~P ^jr 6 if

Onisrio ^ Approval

Mining Lands Comments

3

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To: Geophysics " T^Y^ f"^* fiCommintl

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To: Geology- Expenditures

ComiT)*ntt

^

n.t( Signilur*

To: Geochemistry

Comminlt

'^vv

\ \^^^ ^^^ ••••M*^^

OIK Signitur* Q] Approved | 1 With lo tat tgain wilh cotocliont

To: Mining Lands Section, Room 6462, tthitnt;y Block. (Tel: 5-1360) i

It/IJ iUI/10/

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

j*

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

Type of Survcy(s) Electromagnetic (VLF) St MagneticTownship or Area Skinner Lake (M-2707)——————————— MINJNG ^^ TRAVER^D

Claim Holder^) 493217 Ontario Ltd_____________ List numerically j1910 40 University Ave, Toronto, Ont -' j

Survey Company H. J. Hodge Inc ___________________ ..oi?.?.S...?.Sfe?sSAlAfi..A\ft.\\...........i".'(prefix) (number)

Author of Report R. Gillick, GQOcary&K_____________ 'Address of Author #3 12 Judge Ave. North Bay. Ont •"•••—".—"..."....•............."..•".""l—

Covering Dates of SiirvryQct 20 - Nov l f 1 981_________ .........j.,p.-,.....|.yj..f*.w*y........f...(linecutting to office) |\ C ^-- ' ' '~

Total Miles of Line Cut 30.98______________________ ......................................................f...FFR V 2 1982

—————————————————————————————.—— -i .....................................................4...SPECIAL PROVISIONS DAYS MINING LANDS Stv.JONCREDITS REQUESTED Geophysical p" cUim .....................................................I""""" f

--Electromagnetic———±2—— ....................................,.................;.ENTER 40 days (includes on l line cutting) for first -Magnetometersurvey. —Radiometric—

.................................................,............... jENTER 20 days for each -Other. * additional survey using same grid.

AIRBORNE CREDITS (Special provision credit! do not apply to airborne lurvcyi)

Magnetometer_____Electromagnetic ————— Radiome^ic(enter dayi per claim)

HATK- 5 Feb 1982 SIGNATURE: V/7 '/^?/yAitihoi o f Report or Agent

• " ii 'i iiftin niaum 'i i nil' f \ . 1 i . 111.1 i irnnii

Res. Geol.._____.____Qualifications _

j. Previous SurveysO File No. Type Date Claim Holder ~1C/5

O

TOTAL CLAIMS

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS. - If more than one survey, specify data for each type of survey

rnWrNurnWr of Stations 1 1 6 3.2 .Number of Readings 1,720Station intrrval 100 Feet, some 50 Feet Profile sralf VLF EM lcm = 20%______.

.Line spacing..., 4QQ...Eeet.

Contour intrrval. Magnetic g 250 gammas

(J•—H

HW 2;C •r;5!

Instrument Geometrics G816 Proton Precession MagnetometerAccuracy - Scale constant 10 gammas

correction lOOplncf IntO baSG Station

Base Station check-in interval (hours) l HourBase Station location and value See magnetic maps

UCX,o*-N

w

Instrument Geonics EM-16r.njl configuration Vertical Loop

Coil separation Infinite

AccuracyMethod: X^Q3 Fixed transmitter Frfqurnry 17.8 kHz - Cutter Maine

D Shoot back O In line O Paralic NAA

(specify V.L.F. nation)

line

Parameters Dip Angle (In Phase) S. Quadrature (Out of Phase)

Instrument

Scale constant

Corrections made.

Base station value and location

Elevation accuracy.

Instrument ____————— Method D Time Domain

Parameters — On time ———

- Off time ——-— Delay time ———

— Integration time .

Power.

D Frequency Domain

_ Frccjucncy —————

Range ——-——————

Electrode array —

Electrode spacing .

Type of electrode

Mie) 366-39-17

14IB) 247-2360

RES' U16) 242.2791

H. J. HODGE, INC.EXPLORATION AND MINING GEOLOGIST

25 HOBDEN PLACE

WELTON. ONTARIO MBR 3R6

12 February 1982

Ministry of Natural Resources Room 6450, Whitney Block 99 Wellesley Street East TORONTO, Ontario M7A 1W3

ATTENTION: Mr. J. C. SmithSupervisorMining Lands Section

RECEIVEDFEB 2 2 1982

MINING LANDS SECTION

Dear Mr. Smith,

Please find enclosed two (2) copies of reports on Geophysical Surveys on three groups of claims in the Kenora Mining Division, Patricia Portion, along with supporting documents applying for assessment credits.

I have forwarded completed Reports of Work forms to Mr. A. Hanson in Sioux Lookout.

I trust everything is in order.

Yours very truly

493217 ONTARIO LTD.

H. J. Hodge

HJH/is

Enclosed

c.c. - Mr. A. Hanson

1982.03. 01 2.4568

Mining RecorderMinistry of Natural Resource*P.O. Box 669Sioux Lookout, OntarioPOV 2TO

Dear Sir:

Ve have received reports and naps for a Geophysical (Electro magnetic and Magnetometer) Survey submitted under Special Provision* (credit for Performance and Coverage) on Mining Claims Pa 558807 et al in the Area of Skinner -Lake.

This material vill be examined and assessed and a statement of assessment work credits vill be issued.

Yours very truly,

E.?. AndersonDirectorLnnd Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phonet 416/965-1316

J. Skura/amc

ccs 493217 Ontario Ltd. Toronto, Ontario

cc: B.J. Bodge, Inc. Weston, Ontario

1982 12 31 2.4568

H.J. Hodge Incorporated 25 Hobden Place Western, Ontario K8R 3R6

Dear Sirs:

Enclosed are geophysical (magnetometer* electromagnetic) survey maps covering Mining Claims fK 558807 et al 1n the area of Skinner Lake.

Please have Mr. R. 61ll1ck date and sign these maps and return them to this office. Also* please request Mr. GllHck to provide a resume of his qualifications stating his educational history and work background.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

For further Information, If required, please contact Mr. F.W. Matthews at 416/965-1380.

F.H. Matthews:se

Encls:

cc: 493217 Ontario Limited Toronto, Ontario

cc: Mining RecorderSioux Lookout, Ontario

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