42A14SEe328 2 .2766 REID 010

!";-k 'i'" l M Li

LAND3 SU

DETAILED GEOPHYSICAL COVERAGE

TULLY TOWNSHIP "B" BLOCK

TIMMINS AREA NORTHEASTERN ONTARIO

for

NORCEN ENERGY LTD.

Toronto, Ontario, Canada February, 1979

W. E. Brereton, M.Se.(A) M P H CONSULTING LIMITED

INTRODUCTION AND SUMMARY

Additional linecutting and geophysical surveys (MaxMin

II electromagnetic and magnetometer) were carried out

over the Tully "B" Block in June/ 1978. This work is

supplemental to previous surveys carried out in early

1978 which are described in a report entitled "Report

on Electromagnetic and Magnetic Surveys on Claim Groups

in MacDiarmid, Reid/ Murphy and Tully Townships/ Timmins

Area, Porcupine Mining Division" by W. E. Brereton/

dated May, 1978.

The latest surveys more accurately defined and extended

conductive zones "2" and "3" located by the previous geo

physical work.

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LOCATION AND ACCESS

The six claims straddle the Buskegau River in the

northeast quarter of the township.

.

(Easiest access is by helicopter from Timmins.

iGEOPHYSICAL SURVEYS

The surveys were carried out on cut and picketed line

grids. North-south crosslines were established at

100 metre intervals for a total of 7 km of line.

Magnetic data were recorded with a Scintrex MP - 2 pro

ton magnetometer at 25m intervals. Base stations were

established as required and the data were corrected

for duirnal magnetic variation.

A MaxMin II EM unit was used for the EM surveying at

frequencies of 444 Hz and 1777 Hz and coil separation

of 600 ft.

Technical details of the methods and instruments are

presented in Appendix I of the parent report.

GEOPHYSICAL RESULTS

Electromagnetic

Nine MaxMin conductors, EM1 to EM9/ have been interpreted based

on the results of the present and previous work.

Conductors EM1 to EMS appear to represent narrow, discreet fea

tures within a complex, steeply-dipping zone of multiple conduc

tors {previous conductive zone 2). Conductivity thickness pro

ducts decrease markedly from 1777 Hz to 444 Hz indicating a

source other than massive conductive sulphides. Previous dia

mond drill hole 65-1 by Utica Mines Ltd. in 1965 appears to have

intersected EMS. The hole cut a 7.9 m (26 ft) core length con

taining nodular pyrite in rhyodacite breccia in the area of the

present conductor. Overburden depth is 27m (90 ft).

Conductors EM4 and EMS are also weak, poorly conductive, steeply-

dipping features. These may be the eastward continuation of

EM2 and EMS across a north-south fault postulated to occur be

tween lines IE and 2E (EM9). Conductors EM6, EM7 and EM8 are

part of a weakly conductive, steeply-dipping line of multiple

conductors. Two holes by Consolidated Novell Mines in 1965

failed to intersect EMS. Overburden thickness is 65m (215 ft).

A previous interpretation of a northwest-southeast conductive

fault zone (Zone "l")in this region does not appear to be

valid.

lMagnetic

A pronounced magnetic high centred at IS on line 4W represents

the east end of an ultrabasic intrusive intersected to the west

l by diamond drilling. The intrusion appears to be truncated to

the east between lines 3W and 4W by a north-striking fault.

l* Apparent displacement of EM6, the westward continuation of EM7 ,

B indicated a right lateral movement on the order of 50m. EM6

occurs immediately north of the above ultrabasic.

lA magnetic high at the south end of line 1W probably represents

'lm another basic-ultrabasic body.

lOverall magnetic trends are east-west.

lThere is no direct magnetic correlation with any of the conduc-

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tors.

CONCLUSIONS

Additional magnetic and MaxMin II Em surveys on the Tully "B"

Block have served to more accurately define previously located

anomalies. Nine EM conductors were outlined.

Consideration should be given to re-testing conductors EM2 and/

or EMS in that the previous drilling intersected semi-massive

sulphides in felsic volcanic rocks in the immediate area of the

conductors.

EM6 is also a potential drill target for gold possibilities

as is the east end of conductors EM7 and EMS.

l

il Respectfully submitted,

, WEBrg W. E. Brereton, M.Se.(A)

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J

CERTIFICATE OF QUALIFICATIONS

I, William E. Brereton of 330 Ontario St., Toronto, Ontario do

hereby certify that:

1) I was granted a Bachelor of Science degree with Honours from

Queen's University/ Kingston, Ontario in Geology and Physics

(1971) and a Master of Science degree (Applied) from McGill

University, Montreal, Quebec in Mineral Exploration (1977).

2) I have been practising my profession in mining since gradua

tion. Conclusions and recommendations contained in this re

port are based on a knowledge of the geology and base metals

potential of and geophysical applications within the Abitibi

gained through several years' experience in the area.

Dated at Toronto, Ontario this 2nd day of March, 1979.

lW. E. Brereton

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ii

VOLUME I

42AHSEe328 2.2708 REID OSO

JUN l 19/8

MINING UNDS SECT/ON

REPORT ON ELECTROMAGNETIC AND MAGNETIC SURVEYS

ON CLAIM GROUPS IN

MACDIARMID, REID, MURPHY AND TULLY TOWNSHIPS

TIMMINS AREA

PORCUPINE MINING DIVISION

for

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD,

Toronto, Ontario, Canada May, 1978

W. E. Brereton, M.Se.(A) M P H CONSULTING LIMITED

SUMMARY

Geophysical surveys {MaxMin II, magnetometer) on 5 claim

blocks totalling 44 claims north of Timmins, Ontario have

located a total of 8 conductors as follows:

Claim Block

Conductive Zone

Conductivity (inphase/ quadrature)

Conductivity- Thickness

(mhos)Comments

Reid"A"

Murphy"A" l

Low

Low

Shear and/or graphi tic tuff

3 Shear (line 8S)

Murphy"A" 2 moderate to very good to 35(444Hz At least one 120mline 3E) drill hole

Tully"A"

Tully"A"

Tully"B"

Tully"B"

Tully"B"

1

2

1

2

3

Low

Low

Low

Good (?)

Moderate

5 Shear and/or graphi tic tuff

4 Potential drill tar get

4(444Hz) Buskegau River Fault

Possibly drilled by previous workers

3 Potential drill tar get

Zone 2 on the Tully "A" block and Zone 3 on the Tully "B"

block require additional geophysical definition before dril

ling. Zone 2 on the Tully "B" block is a potential drill

target until it can be positively established whether or

not this conductor was drilled by previous workers in 1965.

iii i l . mgm

9

INTRODUCTION

During the period January 15 to April 10, 1978, magnetic and electromagnetic surveys were carried out over five properties north of Timmins, Ontario, for Great Plains Development Com pany of Canada Ltd. Field operations were carried out by Geoex Limited of Timmins under contract to M P H Consulting Limited of Toronto who were responsible for overall programme supervision, data interpretation and report preparation.

The five properties are as follows:

1) Macdiarmid Township - "A" Block

Claims P 452357 to P 452374 inclusive andClaims P 495317 to P 495322 inclusive (Total - 24 claims)2) Reid Township - "A" Block

Claims P 495323 to P 495326 inclusive (Total - 6 claims)3) Murphy Township - "A" Block

Claims P 452382 to P 452385 inclusivebeing the S 1/2 of Lot 6, Concession 3(Total - 4 claims)

4) Tully Township - "A" Block

Claims P 500514 to P 500519 inclusivebeing the N 1/2 of Lot 3, Concession 6and the NW 1/4 and SW 1/4 of the N 1/2of Lot 2, Concession 6 (Total - 6 claims)

5) Tully Township - "B" Block

Claims P 500520, P 500521 and P 500334 to P 500337 inclusive being the N 1/2 of Lot 5, Concession 4 and the NW 1/4 and SW 1/4 of the N 1/2 of Lot 4, Con cession 4 (Total '

TOTAL CLAIMS

6 claims) 44 claims

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The claims are located in the west central portion of the

Abitibi greenstone belt within a 25 mile radius north of the

city of Timmins (Location Map - pocket l at rear).

GEOPHYSICAL SURVEYS

a) Grids

All surveys were carried out on cut and picketed line

grids. Line spacing was 100m in all cases with the

exception of the Tully "B" block where crosslines were

inadvertently cut at a 125m spacing.

A total of 87.5 km of line was cut and chained with sta

tions at 25 m intervals. Two grids at right angles were

required to adequately investigate the Murphy claims.

b) Methods

Magnetic data were systematically recorded with a Scin-

trex MP-2 proton (total field) magnetometer at 25m inter

vals. Base stations were established as required and the

data were corrected for duirnal magnetic variations.

A MaxMin II electromagnetometer was used for the EM sur

veying. The horizontal loop {maximum coupled) mode was

employed throughout. A coil separation of 600 ft. (183m)

and frequencies of 444 Hz and 1777 Hz were used for rou

tine coverage.

Technical details of the methods and instruments are

presented in Appendix I.

c) Presentation of Results

The geophysical results accompany this report under se

parate cover.

The magnetic data are presented as contoured plans at a

scale of 1:2500 with a 25 gamma contour interval.

The EM data are presented in profile form at a profile

scale of l cm to 101; and a map scale of 1:2500.

DISCUSSION OF PROPERTIES

The five properties are discussed following as to location

and access, previous work, geology and geophysical results.

1) Macdiarmid Township - "A" Block

a) Location and Access - The Macdiarmid claims are lo

cated in the northeast part of the township, one

claim west of the powerline which leads south from

the Sturgeon Falls dam on the Mattagami River. The

road along the powerline was kept open by Ontario

Hydro last winter, which/ in conjunction with some

logging roads, allowed easy truck access to the pro

perty.

b) Previous Work - The most significant previous work

consists of a 1964 diamond drill programme by Silver

Men Mines Limited immediately east of the central

portion of the east claim boundary. One hole (no.11)

intersected a 125 ft. section of up to 5Q* pyrite

and pyrrhotite in brecciated rhyolite and graphitic

fragmental tuff. Sphalerite and chalcopyrite are

reported within one of the graphitic sections in the

sulphide zone. Other drilling in the immediate area

(drill hole nos. 6,7,8,9,12,13) showed bedrock to

consist of andesitic volcanics and tuffs containing

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units of massive to brecciated rhyolite. The drill

results indicate that there are two sulphide-gra

phite zones separated by approximately 500 ft. which

strike west and northwest onto the Great Plains'

ground.

l Previous and subsequent ground electromagnetic sur

veys by Consolidated Regcourt Mines (1964) and

l Belleterre Quebec Mines (1965-66) defined numerous

weak conductors in the area covered by the present

l claims. There are 2 Turair anomalies and 2 INPUT

M (Mark 5) anomalies on the ground as a result of 1970-

71 surveys by Mattagami Lake Mines and Hollinger

l Mines respectively.

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c ) Geology - The data compilation map for Macdiarmid

Township (ODM map P.730) indicates the claims to be

underlain by a northwest-striking sequence of felsic

l and mafic to intermediate metavolcanics. There is

an outcrop of felsic metavolcanics in the central

l portion of claim P 495318. Our regional interpre-

M tation indicates that tops here are to the north.

m The Silver Men massive sulphide prospect is indica-

ted to be at a contact between underlying felsic

l metavolcanics to the south and mafics to the north.

This contact continues westward onto the Great

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Plains' ground.

The Montreal River Fault crosses the extreme north

east corner of the claims.

d) Geophysical Results - There are conductive indica

tions in several areas on the property characterized

by high positive inphase and, particularly, high

positive quadrature readings flanked by narrow,

slightly negative wells. The effect is best display

ed at 1777 Hz along lines 7N and 8N in the area of

tie-line 10W and in the northeast corner of the pro

perty e.g. line 3N (maps IB, 1C). Profile shapes

and conductivity-thickness calculations obtained

from detail information on lines 7N, 8N and 12N at

all four available frequencies (222 Hz, 444 Hz, 888

Hz, 1777 Hz) indicate that these "anomalies" are

conductive overburden effects related to buried

bedrock highs (map ID). The "anomaly" along tie-

line 10W coincides in part with a north-south,

linear magnetic high interpreted as a diabase dyke

which probably forms the bedrock high.

Magnetic trends are north-south over most of the

property in contrast with the indicated west to north

west strikes of the underlying metavolcanics. This

effect is probably due to diabase intrusives. A

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thick, north-striking dyle is inferred to cross the

west part of the property.

There is some indication of more east-west magnetic

trends in the northeast portion of the property.

The circular magnetic high in the southwest corner

of claim P 452364 appears to represent a small,

northeast-plunging, cylindrical body and may be a

basic plug.

The significance of the magnetic high in the extreme

northeast corner of the property (claim P 452357) can

not be determined as the anomaly extends off the exis ting ground.

Comments - No bona fide bedrock conductors have been loca ted to date.

Additional work may be warranted in an attempt to locate a continuation of the Silver Men zone onto the present claims.

10

I 2) Reid Township - "A" Block

l a ) Location and Access - The Reid claims are located

l

in the extreme northeast corner of the township.

The powerline road described for the Macdiarmid

claims passes along the west claim boundary.

b) Previous Work - There are several apparently untes

ted ground electromagnetic anomalies located in

1965-66 surveys by Terra Nova Explorations Ltd.on

the claims. Two holes by Phelps Dodge in 1975

about 3/4 miles northwest of the Great Plains'

block cut long graphitic sections (up to 156 ft),

with minor sulphides in mainly felsic flows and

pyroclastics. This geology is striking south on

to the present claims.

c) Geology - The four claims straddle about 1/2 mile

of a west-northwest striking fault contact between

felsic metavolcanics to the south and andesite-

basalt to the north according to the Reid compila

tion (Map P700).

A north-northwest magnetic trend over the west part

of the group (map 2A) is interpreted as a diabase

dyke which appears to be offset in a left lateral

fashion along a west-northwest fault. This fault

coincides with that postulated by the ODM geolo

gists.

11

There is no outcrop.

d) Geophysical Results - There are no EM or magnetic

anomalies of potential economic significance. The

major fault which cuts centrally across the claims

has a weak but definite EM expression (maps 2B,2C).

Calculated depths to conductor are on the order of

50m.

Alternatively there may be a weakly graphitic tuf

faceous unit along the felsic-mafic contact.

Comments - The Terra Nova horizontal loop anomalies are pro

bably due to conductive overburden effects. A Terra Nova

vertical loop anomaly on claim P 495324 probably reflects

the fault.

No further work is warranted at the present.

3) Murphy Township - "A" Block

a) Location and Access - The Murphy claims are loca

ted in the central part of the township less than

1/2 mile east of highway 655 which leads from

Timmins to Texasgulf's Kidd Creek Mine.

b) Previous Work - A vertical loop electromagnetic

survey by Volcanic Mines Limited in 1968 covered

the 4 Murphy claims as part of a larger programme

12

in the immediate area. Subsequent (1971) drilling

by Amax on one of the three vertical loop conduc

tors two claims west of the existing Great Plains'

ground showed a zone of massive pyrite-pyrrhotite

in felsic fragmentals.

In 1969, Amax also drilled a hole in the northeast

corner of present claim P 452382 to test an I P ano

maly.

c) Geology - The claims are probably underlain pre

dominantly by intermediate to felsic flows and pyro

clastics considering drilling on and to the west of

the ground.

There are outcrops of pillowed basalt less than

1/2 mile from the southwest corner of the group so

that part of the south claims may be underlain by

more basic volcanics.

A major north-northwest trending esker crosses the

two westerly claims. Coincident with this esker

is an increase in overburden depths as calculated

from the electromagnetic data and a disruption/

truncation of ground magnetic trends {maps 3A,3B,

3C). The esker is therefore interpreted to be oc

cupying a north-trending fault or fault zone, pos

sibly several hundred feet wide. The arcuate

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pattern and westward increasing nature of the mag

netic data reflects a serpentinite body centred

about l mile west.

Bedrock strikes on the property are probably east

to northeast with moderate dips.

There is no outcrop.

d) Geophysical Results - The EM results indicate two

conductive responses, Zones l and 2 (maps 3B, 3C).

Zone l is a vertically dipping, generally very nar

row, weak conductor and is interpreted as a north-

south fault zone now occupied by the esker.

This conductor is either distinct from or superim

posed on Zone 2. Considering just the EM response,

Zone 2 is interpreted as an arcuate body about 275m

long plunging about 45 degrees to the northeast.

Conductivity is moderate to very good being the

strongest on line 3E where the high frequency in-

phase to quadrature ratio is about 2.5 to l and the

low frequency conductivity-thickness product is

about 35 mhos. Depth to current axis is in the or

der of 30 m.

The magnetics provide a somewhat different interpre

tation. There is a very definite truncation of the

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magnetic contours coincident with the conductor

immediately west of line 3E suggesting that the

east-west portion of Zone 2 may not be related to

the north-south portion. The latter may be part

of Zone l, i.e. the fault.

There is a slight magnetic low associated with the

east-west portion of Zone 2 (40 gammas on line 3E.)

Comments - The strong conductor on line 3E should be drill

tested by a hole drilled grid south at -50O from 2 7* 70S

for approximately 120 m.

Serious consideration should also be given to investigat

ing the north-south portion of Zone 2 in a hole drilled

from the same set-up as previous at -50 on a bearing of

az 230 degrees for approximately 120m.

4' Tully Township - "A" Block

a) Location and Access - The claims are located in

the extreme northeast corner of the township and

are most easily accessible by helicopter from

Timmins.

b) Previous Work - Noranda Mines Limited (1968-69)

located 3, three-channel INPUT anomalies, one

with magnetic correlation/ over the present claim

15

block. Subsequent vertical loop follow-up located

5 conductors. There is no record of any drilling.

c) Geology - The six claims straddle about 3/4 mile

of the upper (?) contact between an approximately

one mile wide felsic unit to the south and inter

mediate-basic metavolcanics to the north (ODM map

P 699).

There is no outcrop on either of the Tully blocks.

d) Geophysical Results - Two conductive zones are pre

sent. Zone "l" trends southeast across the entire

grid except for an interruption in the area of

lines 8E, 9E and 10E. The conductor is very weak

and displays low conductivity being mainly a qua

drature effect at 444 Hz. A vertical to very steep

northeast dip is indicated. A calculation on the

444 Hz data on line 4E gave a depth to current

axis of approximately 60 meters and a conductivity-

thickness of 5 mhos. Conductor "l" coincides very

closely with the major felsic-mafic contact which

is shown to cross the claims on the Tully data com

pilation map. The situation is therefore identical

to that in Reid and Conductor "l" represents a

weakly graphitic tuffaceous or sedimentary horizon

and/or a zone of shearing coincident with the contact.

P l

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Conductor "2" is a weak but definite, mainly quadra

ture feature at 444 Hz. The response is obscured by

noise at 1777 Hz. A relatively narrow, steeply dip

ping zone is indicated. Calculations on the low fre

quency data on line IDE give a depth to current axis

of approximately 45m and a conductivity-thickness of

4 mhos. Bedrock here is indicated to be basic vol

canics.

There is a positive buildup in both inphase and qua

drature at 1777 Hz and mainly in the quadrature at

444 Hz at the north ends of particularly lines 8E

and 9E. This is interpreted as an overburden effect

analagous to that in Macdiarmid.

There is no magnetic association with either conduc

tor.

Comments - There are no drill targets in Zone "l". Zone "2"

in the area of l -f 7 5N, line 10E is a potential drill target

but further definition is required. Lines HE and 12E should

be extended to the north. Lines 9E, 10E, HE and 12E should

then be re-surveyed with an 800 ft. (242m) cable using the

lower frequencies. Line 9E should be extended to the north

to make certain that the conductive indication here is an

overburden effect. Further recommendations will be contin

gent on the results of this work.

17

5) Tully Township - "B" Block

a) Location and Access - The six claims straddle the

Buskegau River in the northeast quarter of the

township. Easiest access is by helicopter from

Timmins.

b) Previous Work - In 1965, Utica Mines Limited dril

led a 489-ft. hole on an east-west striking hori-:

zontal loop anomaly in the northwest portion of the

present block (claim P 500520). The hole intersec

ted a 6 ft. section of 50% pyrite-pyrrhotite within

a sequence of rhyodacitic flows and pyroclastics

with minor tuff and greywacke. Minor chlorite-epi-

dote and graphite are mentioned. There are several

other conductors which were never tested.

Two holes by Consolidated Novell Mines Limited in

1965 on present claims P 500521 failed to reach

their intended target, a horizontal loop conductor,

due to drilling problems. The drilling showed bed

rock to consist of acid pyroclastics.

Texmount Mines defined a "very weak" vertical loop

anomaly in the north half of present claim P 500355

which was apparently never drill tested.

United Comstock Mines Ltd. in a 1965 drill hole on

an EM conductor immediately to the south of the

18

existing block intersected numerous graphitic

zones in a sequence of massive and brecciated rhyo-

lites.

c ) Geology - Interpretation of the magnetic and elec

tromagnetic data indicates that a north-northwest

trending fault (Buskegau River Fault) crosses the

east portion of the claims (maps 5A, 5B, 5C). East

of the fault, bedrock is indicated to consist of

east-west striking mafic and felsic metavolcanics

with an intercalated greywacke unit. The area west

of the fault is underlain mainly by felsic meta

volcanics. A magnetic high on lines 875W and

1000W reflects the east end of an ultrabasic body

l indicated on map P 699.

ld) Geophysical Results - There are 3 conductive zones.

Il Zone l occurs in the central part of the group, be

tween lines 3 J 7 5W and 5 J O OW and is interpreted

to consist of two narrow, steeply dipping conduc

tors with a depth to current axis of about 55m and

a conductivity-thickness of 20 mhos (east conductor,

1777 Hz). At 444 Hz, conductivity-thickness is 4

mhos. The conductive zone crosscuts local magnetic

trends at about right angles.

This zone is interpreted to represent the Buskegau

19

River Fault.

The grid lines over Zone "2" are at a low angle to

the conductor as reflected in the long positive

buildup to the conductor from the south. Also,

the positive shoulders are not completed on the

north side as the conductor occurs close to the

property boundary so that a meaningful interpreta

tion of depth etc. is not possible. There is an

indication, however, of good conductivity, i.e.

large inphase to quadrature ratio, at 1777 Hz on

line 5 J O OW.

The quadrature predominates at the lower frequency

and indicated conductivity decreases markedly at

444 Hz. This zone appears to be that drilled by

Utica Mines in 1965 (see Previous Work). The 6 ft.

section of 50S, pyrite-pyrrhotite in the hole would

not be inconsistent with the Zone 2 EM response.

Zone 3 appears to be the east end of the EM conduc

tor that Consolidated Novell Mines failed to inter

sect in two drill attempts in 1965. The 1777 Hz

data on line 1000W indicate a steeply south dipping

zone with a conductivity-thickness of 3 mhos. Depth

to current axis is interpreted at approximately 20m

in contrast with a known overburden thickness of 36m

in Consolidated Novell hole 2A somewhere to the west,

20

Zone 3 occurs on the east end of an elliptical mag

netic anomaly and is possibly associated with an

ultrabasic.

A broad, very weak quadrature anomaly which extends

east-west across the central portion of the proper

ty is interpreted as an overburden effect.

Comments - Zones 2 and 3 should be re-defined on 100m, north-

south lines as a prelude to possible diamond drilling. A

field check should be carried out in the area of Zone 2 in

an attempt to locate the old Utica drill hole.

Further recommendations will be contingent on the results of

the above.

21

CONCLUSIONS

Work to date on 5 claim blocks north of Timmins consist

ing of line-cutting, MaxMin II and magnetometer surveys

has outlined one definite drill target, namely Zone 2 on

the Murphy township "A" block.

Zone 2 on the Tully "A" block and Zones 2 and 3 on the

Tully "B" block are potential drill targets. Additional

geophysics and field checks are necessary before any firm

recommendations can be made.

lRespectfully submitted,

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WEB:g W. E. Brereton, M.Se.(A)

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CERTIFICATE OF QUALIFICATIONS

I, William E. Brereton of 23 Helmer Avenue, South Porcupine, Ontario do hereby certify that:

1) I was granted a Bachelor of Science degree with Honours from Queen's University, Kingston, Ontario in Geology and Physics (1971) and a Master of Science degree (Ap plied) from McGill University, Montreal, Quebec in Mineral Exploration (1977).

2) I have been practising my profession in mining since gra duation. Conclusions and recommendations contained in this report are based on a knowledge of the geology and base metals potential of and geophysical applications within the Abitibi gained through several years' exper ience in the area.

Dated at Toronto, Ontario this 10th day of May, 1978.

W. E. Brereton

23

APPENDIX l

SPECIFICATIONS

BRIEF DESCRIPTION OF THE MAXMIN II EM SYSTEM

The MaxMin II is a two-man continuously portable EM system, for

which the basic specifications were set down by Mr. Jack Betz

following an extensive test program of eleven continuoualy por

table EM systems in 1972.

The MaxMin II system is designed to measure both the vertical

and horizontal in-phase (IP) and quadrature phase (QP) compon

ents of the anomalous field from electrically conductive zones.

More accurately, the directions of the measured components are

perpendicular and parallel to the mean slope between the trans

mitting coil (Tx) -and the receiving coil (Rx) .

The plane of the Tx is kept parallel to the mean slope between

the Tx and Rx at all times. This means that the MaxMin II is in

effect a horizontal loop (HL) system, when the receiver measure

anomalous components perpendicular to the mean slope between the

coils. It is a minimum-coupled (Min C) system, when the receiver

measure anomalous components parallel to the mean slope between

the coils.

Generally the MaxMin II is run in the HL mode with the Min C mode

being used in the few instances, where it can improve on the data

of the HL mode.

The MaxMin II has the following principal features designed into

it:

1) four system frequencies -222, 444, 888, and 1777 Hz - to deal

effectively with a wide range of overburden and bedrock conductor

conductivities,

2) six Tx-Rx separations - 100, 200, 300, 400, 600 and 800 ft*-

to cope with a wide range of problems from the search for large

deep conductive zones to the resolution of shallow, parallel con

ductive zones,

4) a built-in, easy-to-operate intercom system to insure good

co-ordination of the transmitter and receiver operators at all

times.

5) very advanced electronic (active and digital) filtering in

ll\

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in the receiver to reduce the interference effects of power line

and atmospheric noise,

6) warning lights to indicate invalid readings,

7) large scale IP and QP meters giving a fine scale reading pre

cision of 1 /2* o f the primary field strength at the receiver,

8) reference cables with teflon insulation and jacket to insure

easy pulling at all times,

9) the capability of changing the Rx from the HL to the Min C

mode with no loss of time,

10) balanced reference voltage and compensator circuitry to eli

minate stray coupling effects, and

11) two-man portability to reduce operating costs.

* 30.5, 61, 91.5, 122, 183, and 244 metres.

lFile.

tario 42AHSE0328 2.2708 REID 900

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 Survey(s)

Township or Area

Claim Holder(s)

Survey Company jhl

Author of Report U3. k. .

Address of Author \Sob - ( 4\Covering Dates of Survey

Total Miles of Line Put

IS. — Plan*[linecutting to office)*J

2Jo * 4*

i

i

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

Electromagnetic.

Magnetometer_

Radiometric

Other—————.

DAYS per claim

Geological.

Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic. .Ra

ii '

l

'

l

l

DATE:

(enter days per claim]

SIGNATURE: (jL U/LAuthor of Report or Agent

Res. Geol.. Qualifications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

/:

t

W.P..4:S3,..lfc4.!'..,..,,.....,.,......,

.a

CA

TOTAL CLAIMS .*^vri^^^TTT!^T^TSf\|5i^^^^^^5^^^^

lGEOPHYSICAL TECHNICAL DATA

i*L , GROUND SURVEYS — If more than one survey, specify data for each type of survey

l

l

P

Number of Stations —— Station interval ^, Profile scale 4. C.UA.

.Number of Readings Xine spacing.

Contour interval

C

Z9•^s

-s*- A J

Instrument fi O-'Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours)- Base Station location and value

tvy —

- n'74x^g^s;

a13 zz•s. S

l

Instrument \ (f.Coil configuration .Coil separation &OO Q+ (l&lAccuracy O - S Ip-—————Method: Frequency

Parameters measured

O Fixed transmitter "A*

D Shoot back ©In line D Parallel line

Instrument.Scale constantCorrections made.

Base station value and location.

(specify V.L.F. station)

-^:'

Elevation accuracy.

InstrumentMethod D Time Domain Parameters — On time .——

- Off time __L.— Delay time ———.— Integration time.

Power.

D Frequency Domain _ Frequency _____ Range _______'.

Electrode array-—i "tElectrode spacing . Type of electrode .

File.1; , RB| 40brio

—t

i | TECHNIC•f

ITypc of Survey(s) H^1*Jut O Township or Area l\u.f

1 Claim Holder(s) C-7ttLO.T"r kt^AA4hA

1' Survey Company (ft r H

Author of Report t A J ^

Address of Author \^oto -

•Covering Dates of Survey Ji ' ^ i- '"btal Miles of Line Cut

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (include line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

iviiiiibiiy ui i^aiurai nesuurces

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

(

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

iAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.*

^f\C. t \ t t^VC) tAAjOL^Nt-Vltj

P^Uxyi \ pUi) Vi S. U\ fe

P Vot i w-1 -j If f SLfcA^lA \M*-t\ iU^LA fin C-A^A^oLflt L-rO^^^ ^^^ * J 1 1L, ./AA ftu-L rovN* LJnw

-* /J l '*\ (j r^fi^VA-TO\Tk

•\4\ fWjLwm^tt ^Lol'(ov*AA.ro,HSti^trSJ^A^A^/LAX* IS - lr\ccu ^V IHTciJ (iJnecutting to offrot) '

,DAYS r^ L - i Per ^aWGeophysical , T l—Electromagnetic , \1aO. iw^

s ^"o \

— Radiomrtrir .... . .-Othf-r

Cpologiral

IRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

ragner,ometer T , .Flrrtrnrpagnetir Rarliomrtrir(enter days per claim) , f\j jj 1 PI xn F _•JQATR? fl iCw^U-- (Qlft sinMATiiPF- ^/A J A-lJ 4jtAJ l UA

mes. Geol.

ievious Surveys

Author of Report or Agent

Qualifications cX - 1 J l ^**r - ~

'ile No. . Type Date Claim Holder

'

.-.-4H-

s

MINING CLAIMS TRAVERSED List numerically

(prefix)

.............P.......4.S

(number)

2U^J^^2. VB3..... .........

...............^.......^s.^.^.a.^............ ,.,..fe.......4S-2,.^..s.s.:.:.......

\

TOTAL CLAIMS.4-

I

If space insufficient, attach list ,

. . ..^. . . ———————————————————————————————— ! ———————————————————————————— —

lGEOPHYSICAL TECHNICAL DATA

' " ' GROUND SURVEYS — If more than one survey, specify data for each type of survey' .

S 1 ^-Number of StationsStation interval 2.S IAA

Prnfilesrale l C^u.

.Number of Readings ^ jSHM. "

iine spacing.

l

i

Contour interval

MAGNETICArrnrary — Sralp rnnsfant -L 0

Diurnal cnrrrrtinn method \rjTiU (A^A^T MfcO\

Ra*r Statinn rherk-in interval (hours) '4 lw - l. Uv-

BSKP Station Inratinn and value fUkXA^ (A&A* .5l*-^llAA ~ ^^tTT) C . . . A1^ WD S l ^^fe^iO..lf- J' ' 1 . ' "" 7

^Instrument H U^ 1CCoil configurationCoil separation (oBO v^

Accuracy. .Method: D Fixed transmitter

- 444

D Shoot backH

©Inline

Parameters measured

Instrument,

(soldfy V.L.f. fUtion)

^ t

Scale constantCorrections made.

.Base station value and location .

Elevation accuracy-

Instrument

CD Parallel line

.U

Method D Time Domain Parameters — On time

— Off time— Delay time ^—— I ntegration time

D Frequency Domain Frequency —-.-—— Range ________ .

PowerElectrodeElectrode spacing Type of electrode

lll

vano

Ministry bf Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Township Claim Holder(

Survey Company Author of ReportAddress of AuthorCovering Dates of Siirvey^Uc^Mxfr*^ l S - tr\a^

VJ (lin^cutting to office) 'Total Miles of Line Cut ?**(o ———-—————

• Type of Survey(s) '(UQA(AfJ\C* . V d A ""lTownship or Area yJB^iQ l

l

l

l

l

l

l

l

1

l

i

he.

HS^JLS

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical —Electromagnetic.

DAYS per cliim

—Radiometric.-Other-————

GeorhemiralAIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)Magnetometer————Electromagnetic.

; f Ir(enter days per claim)

^ SIGNATURE:. JJ/JJtAJ feAuthor of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

..4flS...A2rla. i 1H *f

TOTAL CLAIMS-•K

RESIS

TGR

AVITY

EL

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lario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

F -1 TECHNK

I Type of Survey(s) jtU^JAf i xJ Township or Area \ yJL

( Claim Holder(s) G^r^^Vr kL^AMha

— Survey Company (ft r H1 x ^ 'J Author of Report f i J i

Address of Author ^^otrs -

1 Covering Dates of Survey^

'ti Total Miles of Line Cut

1•'" — 1 ' f SPECIAL PROVISIONS• CREDITS REQUESTED,,-.Bif.;

1" ENTER 40 days (include line cutting) for first

*' survey.f-' w

•1 ENTER 20 days for each |M additional survey using U same grid.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT 1\L REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

t'hc Glf.rjhro MAflLOV^Ud-n T^n^LLp

JHCii'v^ ([VrSuJ^UA^f

j^ Ce^A^oLflf LW\--MA, JlA-L ruv^* L-A~w

|^ fj Kfi^V^-TOV^-\4N faAjJkJ^JL ^ U^Movo^ro.HStllLSA M X

^O (linecutting to office) v '

DAYS Geophysical .S^~~^— P.lprtrorpfignpHo' 4c* / /j

S ^~-—— ::^' U y * t /^ f**. \ i\slt S— M agnptompfpr |fr*J H/ '

— Radiomrtrir. ^^r^...-OthrrGpnlngiral

Gpnrherniral1- AI RBO RNE CREDITS (Special provision credits do not apply to airborne surveys) ••Magnetometer RWtromagnetic Rarliometrir1 (enter days per claim) , si

f* , i Hi /X P — —SjVATRr (r(ctAll (Clift STr,WATTlPF. f* /A J A O XjMj fuTil ' . -

Ip^es. Geol..OVevJous Surveys

Author of Report or Agent

Qualifications -2. - ' 2 '

| File No. Type Date Claim HolderL.....................:.............'M

f .......... ......

| .......i——— ——— -;- l......................................

F '

MINING CLAIMS TRAVERSED List numerically

(prefix)Lfl (number)

/p ^00 ^^ /~^P-Swsvs •x '

( ^^ y

7 p SS)Q S vB 7*5u A x-........±.E..SJ^^ s \9 ^

TOTAL CLAIMS/fv^

w

1N.J

Eis1 |

GEOPHYSICAL TECHNICAL DATA'• : - ' ', l GROUND SURVEYS — If more than one survey, specify data for each type of survey

-Number of Stations.Station interval .JiS

l Profile

.Number of Readings JJne spacing.

Contour infprval

rJAA UAAa^vJ ri

•pIyif•bil'

1ii o

,A

p

l

Accuracy — Scale constant . . .3- v ., .PJ\irn?l c^TTti"" rprthnrl VCJ^Vp tV^-TA-^O\B?]?'' St?tinn rheck-in interval (hnnrs) '4 Uv — 4-

' L/ ', 1 .L L;Base Station location and value /l&X^uv (^^LAJl \ f^TlC

A L*Instrument , ^TW.!^- TiXVl^. MAA VfXC-S fl^'f-

t JL * l j I Y^Coil ronfjgiiration jTDY^ l ^rOV^r*v.\ \ fr-bpCoil separation (oGD rn l lB^ VM^)Armrary C3 ' ^ O ( a

.Method: D Fixed transmitter OV * j* f j * 1

IAN*. COtilAAAjf •"" ^\T^- VT^ \'

Tt \ 1 *l—Parameters measured J^H^k^L OU+ty A UU^ftLLMX

Instrument

Scale constant

Corrections made

Base station value and location

Elevation accuracy

MA- ftLoo i2-4ofce f ^ i^v^1

hu. T,

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PvAAAh0iv?vi'K *vf- L^-AduaUvu ^H 'rifelol' o

InstrumentMethod D Time Domain Parameters — On time .—-—

- Off time -——.— Delay time..——— Integration time.

Power.

FI Frequency Domain _ Frequency ______ Range _______.

Electrode .a/'ay — Electrode spacing Type of electrode .

l

l

rtano

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

l Type of Survey(s). Tovmship or Area.

, \ ' r( i i- -(Ji/AV H ( . ( ~~ V c w o c-v-rt f IK; \ \ t.A.——

( r\* Siu \ (r^,,-.

O ri: \^ Vn yv .Address of Author Cpc-C- - CA iCovering Dates of Survey. - (ila-.J

• Claim Holder(s) U'-'^f PU , V. -, H; ,:; l,-JV\ iv^^.-i^/w,hr^^ A Cr-^, - l-!--

B Survey Company- ™ Author of Report,

l

i ii

D vt-vx (7t , -fri *^ 1. 1 S. gr, - 3 7 ( 1 *^^ (IJnecutting to office)

H Total Miles of Line 'fiiif 11? - 7- f .Sf C kr ( : ^ (- (rv l/. ;- A \

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using

fwl same

Geophysical—Electromagnetic—Magnetometer.—Radiometric——Other——.—-

DAYS per claim

2-C?

i Geological.Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne f urvcyi)•Magnetometer.

r )it-tVATE- ( I(U( l

Electromagnetic Radiometric(enter days per claim)

SinNATIIRF. ; l XAtifhor of Report or Agent

Res. Geol.. . Qualifications ^ ' l S l I^Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

tt tT*^ *^ ''J ^f *^• •••••••••••(•••••^•••••••••^••••••••A*\* rv* t * * * * * V* •^•••••••t

A V r- - - - -

TOTAL CLAIMS.

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of surveyG 7 *r-

Number of Stations Station interval __

j

Profile scale__

Lm. .Number of Readings JLine spacing

(W

CX*A ^

Contour interval 2^^ 4Instrument O n " L .. hP-?\ P x^vAWu R Mf 6-Accuracy — Scale constant, Diurnal correction method.

Q

flrt^Base Station check-in interval (hours).

W Base Station location and value ( \0

i^ 1 Lv

1 \A \ rT ~

.b N

^. (S?V^1

Q

Instrument

Coil configuration Coil separation Accuracy Method: Frequency.

h^ FC-^D r-( l (i?

^ - S,

CD Fixed transmitter D Shoot back D In liner^.L'A^p ~ 444 (K i^i (h-

D Parallel line

Parameters measured. -v(specify V.L.?. station)

Instrument

Scale constant

Corrections made

Base station value and location,

Elevation accuracy.

w

InstrumentMethod D Time Domain Parameters — On time ™-

- Off time —.—— Delay time.— Integration time.

Electrode array -— Electrode spacing Type of electrode

D Frequency Domain— Frequency.———-—.—- Range _______

1978-06-01

Mr. J. R. McGinnDirectorLands Administration BranchWhitney Block, Room 6404Queen's ParkToronto, OntarioM7A 1W3

11978

Dear Mr. McGinn:

Please find enclosed two copies of reports on Geophysical surveys in Macdiarmid, Tully, Reid and Murphy Townships in Timmins area, Porcupine Mining Division.

The recorded holder of the claims is Great Plains Development Company Limited, 715, 5th Avenue - Calgary, Alberta T2P 2X7

Yours truly,

W. E. Brereton MPH Consulting Ltd.

/cba

V*

Consulting Limited141 Adelaide Street W., Toronto, Canada M5H 3L5 (416) 363-6375

May 29, 1978

NOTE:

These figures take into account additional line-cutting and

geophysics which have recently been completed over claims

P 500520, 500521, 500334 as per grid sketch attached. The

report for this work will be completed shortly and the results

forwarded at that time.

W. E. BRERETON

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l P ,P

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,

t P IP , P

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l l . *.0*0l 4*90*4) 4090*8 4*0707

i i lM.

MACDIARMID TWR - M. 294

4SA14SE0326 2.2708 REID 200

l

CL

UJO UJZ(T < O

THE TOWNSHIP OF

REIDDISTRICT OF

COCHRANE

PORCUPINEMINING DIVISION

SCALE: 1-INCH - 40 CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLEDPATENTED FOR S.R. O.

c.e

NOTES

400 surface rights reservation along the shores of all lakes and rivers .

Subdivision of this twp. into lots and concessions annulled Aug. 19, 1953.

Flooding rights for areas along Mattagami River are reserved to Ontario Hydro. L.0.7085

PUN NO. MONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

REID TWR - M.575

roCM

*

^ i

o:

Qz <—lUJ

o

499432 .499433 '499434J320848 J3Z084•P" IP"'

320849 320646 499496 499494 -499435515877 615878

[500344 500342 500339

5O0353 1500334 300355 1500386

320842 j 3 25952 | 325953 l 325954-- ——----I——----———

3TI l 452370 1452365

P

320841 l 325957 l 3 29956 l 325955 p ip .p IP

1 196925 /498924499420 j 499398 494772 [494767~-~--"~-- J- ___

'498922 '496917199419 499399 494771 494768

P IP IP

499402 499401 494770

^ ,1 V .aa o ton l ^

1508117 l 508118 l 508119

P P508123 508122 1508121 l 508120

-/LI 5' 5688 --4- — — -4— — -t- — -f- — l—

' bozT-i'' lI38I2 6. 1^276^ l ^ \UOW4J 50B ,25 1506)261808^7tp ' -^j__-J.--'" J f l i \ ! 515687- L_|__ — — - j—— —— ^--J-^^ -

508130 [5081291 508(28 i

TP i372337 372362 372363 372364 372363

CM

a:5I-o o

r-4M 3M. 48 0 37'30"

8I 0 26

JAMIESON TWP - M.288

42Ai4se*3aa a.27ee REID 210

THF TOWNSHIPOF j.27*9

MACDIARMIDniSTRICT OF

COCHRANE

PORCUPINEMINING DIVISION

SCALE: MNCH CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

C.S.

Lac.L.O.

M.R.O. S.R.O.

NOTES400'surface rights reservation along the shores of all lakes and rivers.

Flooding rights to areas along Mattagami River reserved to H.E.RC. - 1,0.7085.

This township lies within the M unicipality of CITY of TIMMINS.

™™"*"****^w

DATE OB

JUM-6

SURVEYS AND MAPPING!

PLAN NO. M.294ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

WARK TWP- M.3I7

CO CM

l CL

CLO CO CO LU

256198 1256199

255901 |255909

495616 495619

R R©MRO (L) MROGI089 ' 6IOB6

S.R.O.

MRO IQMRO 61065 i 61082

S.R.O.

GRAVEL l RE S. JS..O.

6IO68 j 6IOB7©MRO l (D MHO

S.R.O.61064 {61063 ©MRO |(pMRO

Littlt B oost

La/if

452385 l 452384

R 'p 28430 128431^

R l R 28429 l 28432

516154 ,5I6I5'3

516314 '5I578S

P P

5788 L 515785

P

S.R.O.

15787 , 515786516152 516316 516313 .515790

S.R,0.l

51 \6309 i 516310515791 , 515792

CD CM

a:

hi

oT.

480 32' 17

12 81 0 I2' 18"

TISDALE TWP - M.3I5

•42A14SE032B 2.2708 REID 220

THE TOWNSHIP OF

MURPHYDISTRICT OF

COCHRANE

PORCUPINEMINING DIVISION

SCALE: 1-INCH 40 CHAINS

LEGEND

PATENTED LANDCROWN LAND SALF

LEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLY

ROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYS

POWER LINESMARSH OR MUSKEG

MINESCANCELLED PATENTED S.R.O.

Kc.

NOTES

400' surface rights reservation a long the shores o f a ll l akes a nd r ivers.

This township ties within the Municipality of CITY of TIMMINS.

Ont. Northland Rwy. spur line R/W for S.R.O. 59e file 177607.

RESERVATIONS:

J)— Reserved for recreational purposes under Sec. 3 P. L. A. File 188543.

- 6 1978

SURVEYS AND MAPPING BRANCH

PLAN NO M.303ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

Duff Twp

i

cLh-

OJ 0) 052

Q.

111(1142A14SE4328 2.2708

J.G.

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p Tp.

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493789 1493788

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A - ^

12 II 10 9^8 7 6 5 4 3 2 1

Gowan Twp. .

*EID 230

i

VI

V

IV th-CL)III "

II

1

rft': '.

fe'ilf^— :

THE TOWNSHIP

j?i22^ O F^ULLY

D STRICT OF COCHRANE

PORCUPINE MIN NG DIVISION

SCALE - INCH ~- 40 CHAINS

kEGENDPATENTED L. AND ( P; CROWN LAND SALE C, S LEASES (g LOCATED .AND LotLICENSE OK OCCUPATION L.O. ROADS rr^r -.-ST.IMPROVED ROADS ^*' - -I*-:: RAILWAYS -^^- ,. *-

POWER tJNES * -jfr-- MARSH OR MUSKEG C-^^^ TRAIL

•f . 3u r *o^ i i -, 0 k f f,

i

NOTESr r? P' g h t s ^ S s er v't 1 ' ri ; J o on j Pvf

DATE OF, ISSUt

JUN - 6 1978

SURVEYS AND MAPPING

4PLAN NO. - M 6C~

ONTARIO

MINISTRY OF NATURAL RESOURCES. SL'RVFYS AND MAPPING BRANCH

GEARY

48 0 45'— THORBURN

LOVELAND

KAM- KOTIAMINES LTD.a

Cu,2n

ROBB JAMELAND JAMIESONQMINES LTD.

Cu,Zn

TURNBULL

48*30' —

H Cu,ZnCANADIAN JAMIESON MINES

LTD.

GODFREY

81 045'

CRAWFORD

CARNEGIE

Chance K IDD C REEK M INE

Prospect 'Cu,Zn,Ag.Cd

KIDD

JESSOP

-— t- -

LUCAS

PROSSER

WARK

MURPHY

DUFF

81*00'

l

MANN

TULLY

GOWAN

HOYLE

Au.Ag MINES[J

TISDALEWHITNEY

a

TIMMINS 2 m iles

LITTLE48 0 45'

EVELYN

MATHESON

CODY

sroo 1

75"

INDEX MAP

TIMMINS EXPLORATION PROJECT

O SO

LEGEND

Great Plains claim blocks

Producing mine

Pasf producing mine

MAP 2

TIMMINS EXPLORATION PROJECT

LOCATION MAP

MILES

lNTS 42A/NWPORCUPINE MINING DIV-,ONTARIO

D.NUTTER J. BARCLAY JULY, 1977

42M4SEO326 2.2708 REID 2-40

J

LO L3E L4E L5E L6E L7E

5N

4N ——

3N

2N

IN

Base Line

li

IS

25

35

4S

Si 0

5N

4N

3N

2N

LEGEND

Measurement Station Along Picket Line

Total Field Value

Main Base Station

Magnetic Contour

Magnetic Depression

Instrument Scintrex MP -2

BL

2S

3S

4S

L7E

CONTOURS 5OO gammas

100 gammas

50 gammas

25 gammas

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

Rood

Fence

Hydro L ine

Building

Drill Hole

Outcrop

x——-x —— x

42A145Ee3ae 2.3796 REID 260

REID TWR LOCATION MAP

"A" BLOCKSCALE: i" = o-s mi.

IMP Hi Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

REID TWP. "A" BLOCK

MAGNETOMETER SURVEY

Scale! l : 2,500

Drown by l g m.e.s. ltd.

Approved b y : W. Brereton

Date! March f 1 978

Drawing No. 2A

8S

LO L8E

LEGEND

Measurement Station Along Picket Line

Total Field Value

Main Base Station

Magnetic Contour

Magnetic Depression

Instrument Scintrex MP-2

C?C?

CONTOURS 5OO gammas

100 gammas

50 gammas

25 gammas 42A14SEC328 2 .8706 REID 270

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

Road

Fence

Hydro Line

Building

Drift Hole

Outcrop

Interpreted Fault or Shear Zone "J J/Leu

MURPHY TWP LOCATION MAP

"A" BLOCKSCALE: i" -- o -s mi.

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

MURPHY TWP "A" BLOCK

MAGNETOMETER SURVEY

Scale : 2,500

Drawn by '. g.m.e.s ltd. Approved by : W. Brereton

Date: March / 1 978

Drawing No. 3A

LO LIE L2E L3E L4E L5E L6E L7E L8E L9E LIOE LIIE LI2E VI

4N --

3N --

2N --

-- 4N

-- 2N

" IN

6S -J-

6N

1

500514 500515

500519 . 50051 B

500516

500SI7

TULLY TWR LOCATION MAP

It *UA BLOCKSCALE : " - O-5 mi.

3N

--BLO

-- is >

-- 23

— 3S

-- 4S

-- 5S

-- 6S

LEGEND

Measurement Station Along Picket Line

Total Field Value

Main Base Station

Magnetic Contour

Magnetic Depression

Instrument Scintrex MP-2

L2E L5E L6E L7E L8E L9E LIOE LIIE LI2E

C?

COMTOUffS 5OO gammas

IOO gammas

50 gammas

25 gammas

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

42A14SE8326 2.27^8 REID

Road -—

Fence *—*'~~ x

Hydro Line r-—T—-i

Building D

Drill Hole (Previous, recomended )

Outcrop / "^ - j

Interpreted Fault or Shear Zone

280

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

""TULLY TWP. A BLOCK

MAGNETOMETER SURVEY

Seal*: 1 : 2,500

Drawn by : g.m.e.s. ltd.

Approved by : W. Brereton

Date! March 1 1 978

Drawing No. 4A

^^TULLY TWR

LOCATION MAP"B" BLOCK

SCALE: i" -- o s mi.

LIOOOW L875W L750W L625W L500W L375W L250W LI25W LO

IVA

1000 N

875 N

750 N - -

<

625 N --

SOON

< 500521

375 N

L250N --

LI25X

LO -

S -

250 S -

375 S -

50OS -

LEGEND

Measurement Station Along Picket Line

Total Field Value

Main Base Station

Magnetic Contour

Magnetic Depression

Instrument Scintrex MP-2

625 S -

-.Stfff

s? 3? i

- l OOON

- 875 N

- 750 N

- 625 N

- 500 N

-- 375 N

--L250N

LIOOOW L875W L750W L625W L500W L375W L 250 W LI25W LOW

LI25N

--BL OSO0

-- 125 S

-- 250 S

375 S

500 S

625 S

CONTOURS 5OO

IOO gammas

50 gammas

25 gammas42A14S60328 2.2708 REID

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

Road

Fence

Hydro Line

Building

Drill Hole

Outcrop CV-'

Interpreted Fault or Shear Zone

708

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

TULLY TWR "B" BLOCK

MAGNETOMETER SURVEY

10 E

f-

5 E

Cre

ek

ION

9N

8N7N

6N5N

4N3N

2NN

IS2S

3S

tf

0 E

l

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SE

LIN

E 00

Co

nsu

ltin

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imit

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as

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nshi

p —

"A

" B

lock

MA

GN

ETO

ME

TER

SU

RVE

Y

Dra

fted

By

: J.

Hoi X

gm

es

Con

sulta

nt:

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ton

Cov

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g D

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Fi

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ce

Dra

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g N

umbe

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urve

y By

G

EOEX

Lim

ited

T

imm

ins,

O

NT.

IA

SOU

TH

L4W L2W LIW LO LIE L2E L3E L4E

4N i-

3N --

UTICA MINES

HOLE l, I965-7H

500336500520

597005930059900

Claim Post

Witness Post

S f-? 46CONS. NOVELLHOLES 2,2,A

O ov.215 500337

United Co m stock Utico Drill Camp

a

4S --

5S -L

i^^^^M

IV

III OTULLY TWR

LOCATION MAPB" GRID

SCALE: - 0 -5 mi.

LEGEND

Measurement Station Along Picket Line

Total Fietd Value

Main Base Station

Magnetic Contour

Magnetic Depression

Instrument Scintrex MP -2

CONTOURS 500 gammas

IOO gammas

/f 00

Rood

Fence

Hydro Line

Building

Drill Hole

Outcrop

Q

O—"

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

TULLY TWR "B BLOCK

MAGNETOMETER DETAIL

Project No: C-287

Scale: l : 2,500

Date: J une , 1978

By: W. Brereton

Drawn: g .m.e.s. ltd

Chkd by:

Survey by Geoex Ltd

Consulting Limited

42AMSEO328 2.2798 REID 330

-L

IS

2S

4S

5S

6S

7S

8S

LIS

L2S

L3S

-90", MB m t.d. ovtrbuntoftf 37m lithologi**: inttr- . m td id t* tuff with graph itic section*: minor py, pa

8 7

452385

4523B2

452384

452383

MURPHY TWP LOCATION MAP

"A" BLOCKSCALE: i" = o -s mi.

L4S

L5S

L6S

L7S

L8SL7E L8E

LEGEND

EM Conductor (indicating width) —

Conductivity Thickness (mhos) l Depth Estimate (m)

//i - Phase Profile

Quadrature Profile

Profile Scale / cm. - 10 *fc

Instrument Apex Parametrics Maxmin J7

Cable 183 m. (600')

Frequency 444 Hz.

50/ '30

A

Claim Post

Witness Post

CreekSwamp

Lake

Trail

-f42A1456*328 2 .2708 REID

Road ~**

Fence *—* —-*

Hydro Line r—-r—-i

Building n

Drill Hole (Previous, recommended} O—l

Outcrop c' ~*t

340

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

MURPHY TWP "A" BLOCK

HEM SURVEY

( 444 Hz)

Scale: l : 2,500

Drown b y ', g.m.e.s. ltd.

Approved by : W. B rereton

Date! March f 1 978

Drawing No.

LO

as

LO

LIE L2E L3E L4E L5E L6E L7E

LEGEND

EM Conductor (indicating width) ~

Conductivity Thickness (mttosJ/Dep/h Estimate (m)

In ~ Phase Profile

Quadrature Profile

Profile Scale f cm. - 10 %

Instrument Apex Parametrics Maxmin 77

Cable 183 m. (600')

Frequency 1777 Hz.

'30

42A14SE032B 2.2708 REID 350

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

Road

Fence

Hydro Line

Building n

Drill Hole (Previous, recommended) O——l i

Outcrop Ci I/-

MURPHY TWP LOCATION MAP

SCALE: i - o -s mi.

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

MURPHY TWR "A" BLOCK

HEM SURVEY

(1777 Hz)

Scale: l ; 2,500

Drawn by '. g.m.e.s. ltd. Approved by! W. B rereton

Date: March l 1 978

Drawing No. 3B

5N

4N--

3N

2N

IN

Bose L ine f-

IS

2S

3S

4S

LO LIE L2E L3E L4E L5E L6E L7E

\

495326

X

495323

495324

4N

LOCATION MAP

3N

2N

>

LEGEND

EM Conductor (indicating width)

Conductivity Thickness (mhos) f Depth Estimate (m)

In - Phase Profile/

Quadra ture Profile

Profile Scale l cm. = /O%

495325

BL

IS

y2S

3S

4S

L3E L4E L5E LG E L7E

Instrument Apex Porametrics Maxmin 77

Cable 183 m (60O 1 )

Frequency 444 Hz.42A14SE8328 2 .2708 REID 360

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

-f-f

Road

Fence

Hydro Line

Building

Drill Hole

Outcrop

K ———— X -——-K

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

REID TWP. "A" BLOCK

HEM SURVEY ( 444 Hz)

Scale: l : 2,500

Drown by l g.m.e.s. ltd.

Approved by '. W, Brereton

Date! March l 1 978

Drawing No. 2C

5N

4N--

3N

IN

Base L ine

IS

2S

3S

4S

\

LO LIE L2E L3E L4E L5E L6E L7E

495326

\\

\ \

\

l

495323

\1

/,

J/'

l

LEGEND

I

i\

y

i \

EM Conductor (indicating width) — —oZZZl^^'

Conductivity Thickness (mhos)l Depth Estimate (m) z/*

in ~ Phase Profile

Quadrature Profile

Profile Scale t cm. - 10 5K

Instrument Apex Parametrics Maxmin 77

Cable 183 m. (600')

Frequency 1777 Hz.

X

\

\ \\

!\ i!

495325

\

495324

L3E L4E L5E L6E

42A14SE0328 2 .2708 REID 370

Claim Post

Witness Post

Creek

Swamp

Lake

Trait

4-Road

Fence

Hydro L ine

Building

Drill Hole

Outcrop

X————H -——-K

O

O——l

•ri "V

L7E

l - - IN

5N

4N

3N

>

BL

IS

2S

3S

4S

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

REID TWP. "A" BLOCK

HEM SURVEY ( 1777 Hz )

Scale: l : 2,500

Drawn by '- g.m.e.s. ltd. Approved b y: W. Brereton

Dote! March / 1 978

Drawing No. 2 B

LO LIE L2E

4N -

3N -

ZN-

^

IN -

0 -

^x^H-^^vvN"1

X ^.

X

2S -

3S -

4S -

5S -

6S -

liU

i

is

"ii

ii jf\ \

\\* ^k

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. \

j* '

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T*

1.i

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\ii

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^

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i /'

1* pI l

\ l

\ !\ ;

*

i

V ''K \ ''

1

500514

|

ii', \'

i\

\

LEGEND

EM Conductor Axis ^™ ™ ™ "^

f/W Conductor (indicating width) —— — *z3Z2Zj ^-^"^

Conductivity Thickness (mhos) /Depth Estimate (m) /so

//? - Phase Profile y7

Quadrature Profile y

Profile Scale f cm. * /0*fc

Instrument Apex Parametrics Maxmin ft

Cable 183 m. (600 1 )

Frequency 1777 Hz. |||||||||^42AI4SE0328 2.2708 REID 3 SO

Claim Pos t ~Y~ Road ^~^

Witness Post —A— Fence * — * —*

Creek ' — - .^~ Hydro Line r — -r — -i

Swamp jit Building D

Lake jfTC^) Drill Hole (Previous , recommended )

Trail *~**es. Outcrop ^~ ]Y

!

l

4)\i*1i

\

i

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L3E L4E L5E L6E L7E L8E

—

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LOCATION MAP"A" BLOCK

SCALE : " : 0-5 mi.

4321

- 4N

- 3N

- 2N

- IN

'-

-BLO

- s \)D'

~ 2 S

- 3S

- 4S

- 5S

- 6S

L3E L4E L5E L6E L7E L8E L9E LIOE LIIE LI2E

V

o —— i , * —— i ts

/^^ JMPHp Consulting Limitedy ^^2L^p^y GREAT PLAINS DEVELOPMENT COMPANY

J O F CANADA LTD.

W TULLY TWP. "A" BLOCK

' HEM SURVEY

(444 Hz)

Scale! : 2,500 Date! March t 1 978

\ ^ \ 1 C*— —— Drawn by ! g.m.e.s. ltd.7 * \ ) l ? \ A , Drawing No. 4 C ( A J^xLJ /VjCAJ- V V/W Approved by ; W. Brereton

LO LIE L2E L3E L4E L5E L6E L7E L8E L9E LIOE LIIE

4N ~ -

EM Conductor

EM Conductor (indicating width) —-

Conductivity Thickness (mhos)/Depth Estimate (m)

in - Phase Profile

Quadrature Profile

Profile Scale l cm. = IO%

instrument Apex Parametrics Maxmin 77

Coble 183 m. (6O0 1 )

Frequency 1777 Hz,

/

L3E L4E

VL5E L6E L7E L8E L9E LIOE LIIE

/

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

H-42A14SE9328 2.27*8 REID 330

Road ^~~~~

Fence

Hydro L ine

Building D

Drill Hole (Previous, recommended ) o—)

Outcrop c~i. ~l*

LI2E VI

-- 6N

-- 5N

-- 4N

~- 3 N

-- 2N

-r IN

fiBLO\

\IS\

-- 2S

-- 3S

-- 4S

-- 5S

-- 6S

LI2E

(AMI

>

1 1500514 500515

500519 . 5O05I8

500516

500517

TULLY TWR LOCATION MAP

"A" BLOCKSCALE : l" : 0-5 mi.

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

M .11TULLY TWP. "A" BLOCK

HEM SURVEY

(1777 Hz)

Scale: l : 2,500

Drawn toy '. g m.e.s. ltd. Approved b y : W. Brereton

Date! March l 1 978

Drawing No. 4 B

oTULLY TWR

LOCATION MAP

< 500521

LEGEND

EM Conductor Axis

L1000 W

1000N --

875N --

750 N --

625N --

SOON --

L250N --

L125N

375 S -

500 S -

L875W L750W L625W L500W L 375 W L 250 W LI25W

EM Conductor (indicating width) ——-

Conductivity Thickness (mhost/Depth Estimate (m)

In - Phase Profile

Quadrature Profile

Profile Scale f cm. = fO%

Instrument Apex Parometrics Maxmin 77

Coble 183 m. (6OO't

Frequency 1777 Hz.

/

L1000W

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

4-Rood

Fence

Hydro Line

Building D

Drill Hole (Previous, recommended )

Outcrop C' "t

L 875 W L750W L625W L 500 W L375W L 250 W LI25W

42AMSE8328 2 .2708 REID 400k)/ A

LO

LOW

- 1000 N

- 875 N

- 750 N

-- 625N

- SOON

-~ 375N

-L250N

>

LI25 N

BL 0500

-- 125 S

- - 250 S

3755

500 S

625 S

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

TULLY TWP.

HEM SURVEY

(444 Hz)

"B" BLOCK

Scale. l : 2,500

Drown by : g.m.e.s. ltd.

Approved by : W. Brereton

Date'. March l 1 978

Drawing No. 5 C

l

oTULLY TWR

LOCATION MAP"B" BLOCK

SCALE: i" ; 0-5 mi.

III

< 500521

LEGENDf M Conductor Axis

L1000 W L875W L750W L625W L500W L 375 W L 250 W LI25W

1000N --

875N --

750 N - -

625N --

SOON --

375 N

L250N --

LI25N

EM Conductor (indicating width) ——^

X 50, Conductivity Thickness (mhos)/Depth Estimate (m) '30

In - Phase Profile

Quadrature Prof ((e ,

Profile Scale t cm. = IO%

Instrument Apex Parametrics Maxmin 77

Cable 183 m. (6OO 1 )

Frequency 1777 Hz.

Claim Post

Witness Post

Creek

Swamp

Lake

Trail

L1000W

42A14SE8328 2 .2708 REID

Road

Fence

Hydro Line

Building D

Drill Hole (Previous, recommended )

Outcrop Ci. Z*

410

L875W L750W L625W L 500 W L375W L 250 W LI25W

LO

\\\

LOW

-- lOOON

-- 875 N

-- 750N

-- 625N

-- 500 N

375 N

--L250N

LI2J5 N

\ \

-BL 0^0'

-- I25S

- - 250 S

-- 375 S

— 500 S

-- 625 S

Consulting Limited

GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

"B" BLOCKTULLY TWP.

HEM SURVEY

(I777 Hz)

Scale: l : 2,500

Drawn by l g m.e.s. ltd. Approved by: W. Brereton

Date! March / I 978

Drawing No. ^ lj)

10 E

J—

5 E

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\

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k

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5E

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LI

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GREAT PLAINS DEVELOPMENT COMPANY OF CANADA LTD.

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Date: J une , 1978

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Project No: C -287

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Date: J une , 1978

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