RPT ON GEOPH SUR 1981 MAG VLF HEM...42A06SW0206 2.3973 BRISTOL 010 PRKUSSAG CANADA LIMITED TIMMINS...

42A06SW0206 2 .3973 BRISTOL 010

PRKUSSAG CANADA LIMITED

TIMMINS WEST PROJECT

GEOPHYSICAL SURVEYS 3981 Mag, VLF, HEM

RECEIVED,'UN 3 01981

MINING LANDS SfcCi

INTRODUCTION

Magnetometer, VLF electromagnetic and HEM surveys

were undertaken over a group of contiguous unpatented

claims within the southwest part of Bristol township

and the northeast part of Thorneloe township in .the

Porcupine Mining Division of the district of Cochrane

(fig 1). Linecutting and geophysical surveys were initiated

in January, 1 981. Completion of the geophysics was

in late June, 1981.

The surveys represent an initial stage in an overall

objective to evaluate the gold potential of the claim

group which is well situated geologically on the western

extension of the prolific Timmins gold camp. Because

of overburden coverage over a large part of the area

it has not been amenable to evaluation by prospecting.

PH9Ee-r tY-J^fis? ription

The group consists of 109 contiguous claims as

shown on fig 2. Recording dates range from

December 6, 1977 to May 22,1981. The 25 earlier staked

claims were staked and recorded by J. Croxall and

D. Miller of Timmins and have been optioned by Preussag

Canada Limited. The more recent claims, largely in

Thorneloc township, were staked eind recorded for Preussag

Canada Limited. Geophysical surveys cover only

claims as listed in appendix.

Location and Access

The property is located in northern Ontario, 20 km

southwest of the city of Timmins; a main mining and

population centre in the area.

The property is readily accessible from Timmins

by way of highways 101 and 144. The latter crosses

the western part of the claims. Access roads for lumbering

1- D.

fUs/C tntrufirt

Ouortr porpfiyrr, gufrll frkupor

, fr/atpor fw^yrf,

Grey*oc*t, tittsiait, noil

Orgillilt onj minif

COnjiomtrolt

Ftllic Mtlostamitn/i

[f j UndirlOta

Mafic f lo* s on3 p f rofla tt ic

rex:*!

FIG. l

PREUSS AG CANADA LTD

t) Pioducjnq^Mlnti

I Doml Mint) Ud l An Ag Cv )

4 Hollnor Mint! Lid l Au AS l

it Mclnlyfi Porcupini Mind Ud tAu *g Cg )

II Pomour Porcuplni Mir.ji Ud l Au AI l

o P?JiJ*'.Ciut!?')Ji!DUli O iilei 10*1 mint (tuAg) 15 Poynoiltr mint Itu *j l

14 Aunof CoU Minij Lid

Ci Scottllh Ontario m i rt* (lu Ag)

t? Uonetol mini (Au *g l

it Bonvthit mint (AU)

19 Eiroulan mint (Av)

10 Ree) mint (Au)

IT Davidion-Titdoll Mint! Ltd (An Ag)

st Dtlnilt Minn Ud (Au At l

4t Fulltr mint i AU)

M Crown mint Ug Ajl

47 Vioona mine ( Au Ag)

49 NiQTit Howk Ptnintula mlntlAuAt)

to Naybob mint (Au Agl

to Mont'o Porcuplnt Min*t LK) (Aw*tl

*] Bowman mint ink) 64 Foymcr mint (Ay Agl

to Noronda Mines Ltd (AU Ag i

TO Preston Mines Ltd (Au Agl

71 Porcupine tokt mint (Au Ag)

Tt Buffalo Anktnti mint (AuAq)

to Coruoixum mind (AuA^)

loo Hollinger Comolidaltd

Coil Wins) Ltd (Au AJ w l '

Location Plan

Timmins \V?st Property

—t.0000 Vi O Win tt

IM.-

""" |P 6 19266 |P 6192671 9587

B IB90I l 495307 1 17773e

P J P \

52BJOX 3! 528302, "YP ' P/_ . ^0 'i2W30l| /S852----- -~

528298 1528299,5

594659 [5946BRISTOL TWP

THORNELOE TWP663865 663053 ' 686866

Optioned Cloims

P l P 'P 5l'5907i 5I59II l 5I59I3 not covered

by surveyl———| Wholly Owned '———' Preussog Claims

Total of I09 claims - 96 claims covered by survey

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-4-

loperations make ease of activities within the property

quite good. Most parts are within easy walking distance.

Topography is f]at except for outcrop areas in

the Bristol township claims. Otherwise spruce swamps,

cedar swamps and some spruce covered sand plains dominate.

Re s u 31 s jp f J1 revious Invest ig ations

The first recorded work on the property was undertaken

by Rusk Porcupine Mines in 1942 on what are now claims

495307, 495308 and 495309 in Bristol township. Pits,

trenches and 18 diamond drill holes {6,500 feet) were

completed. No assay results from the drill holes are

available, however channel samples in carbonatized andesite

produced assays of: 4.0 ft of 0.71 oz/T Au; 2.5 ft of

0.43 oz/T Au; and 3.0 ft of 0.24 oz/T Au. (ref. ODM

vol 66, pt. 7, 1957).

Various geophysically directed programs were undertaken

over scatered parts of the present property from 1951

to 1962 as follows:

1 - 3953 Dominion Gulf did a raag survey north and south

of the Tatachikapika River in Thorneloe Township. Three

holes intersected iron formation.

2 ~ 1959 - ]962 Hollinger drilled at least 20 holes

as follow up to magnetometer and EM surveys in Thorneloe

and Bristol Townships. A variety of rock types such

as basic volcanics, ultramafics, porphyries, iron formation

and slates were intersected. Assays are not available,

but massive pyrite and pyrrhotite stringers and carbonated

inctasediments with quartz and pyrite are recorded.

No recent exploration has been undertaken on the

property itself, but over the last ten years there has

been intermittent activity on the Holmer property immediately

to the north where a shear zone up to 150 feet wide

in carbonated metavolcanics carries gold in quartz-

tourmaline veins.

-5-

Survcy Sj^ecJ^f icaj:.jic)i^s

The surveys were completed on picket line grids

as shown on Maps. Baselines were oriented parallel to

what is believed to be the regional trend of the litho-

logies. Picket line spacings are at 120 metres.

The survey was carried out by Mr. F.A. Hodgkinson,

assisted by Mr. Beaulieu and Mr. G. Mason-Apps.

(a) Magnetometer Survey - Readings were taken at 30

metre intervals along the picket lines using a Scintrex MP-2

(see appendix) proton precession magnetometer. Readings

were corrected for drift by tying into the baselines

which had been read and corrected previously by using

the looping method of baseline correction.

(b) VLF Survey Readings were taken at 30 metre stations

with the Geonics EM-16 {see appendix) to record the

]n-Phase and Out-of-Phase components. The Cutler Maine ^

transmitter at 17.8 k Hz was utilized for the entire

survey. Signal strength from Panama station was extremely

weak and hence could not be used for Baseline "B" in

spite of its ideal locaion. Readings on Baseline A and

B were taken with the operator facing south in both

instances.

(c) HEM Survey - Readings were taken at 30 metre stations

with the Apex Parametrics MaxMin II EM system (see appendix)

j ri the horizontal loop mode. A coil sep^lration of 120

metres was used and readings at 444 Hz and 1777 Hz were

recorded. Since the topography is fairly level no corrections

were necessary.

-6-

Survey Resjults^ a n d I n t c rp r c t a t i on

(a) Majgnet^icjs - Contoured magnetics are illustrated

on maps 2a, 2b, 2c.

The gr j d A area (maps 2a, 2b) is dominated by a

series of parallel and en echelon mag highs along and

adjacent to the baseline from line 1680E to the east

end of the grid. The strongest and most continuous of

these linear mag features exists from line 2160E to line

5880E with local intensities to greater than 42,0002^

above background at two locations - namely* at the baseline

on lines 3240E to 3480E and at 150N on line 5280E. The (

magnetic intensity and linearity of this feature is typical

of that caused by magnetite iron formation. Steep gradients

suggest shallow depths locally (see line 5280E) . However,

on line 3360E not only is a deeper source interpreted

from shallower gradient but the broad nature of the

anomaly is also more consistent with a thickening,

probably by folding.

The en echelon mag high from L 1800E to L 2520E

has similar characteristics to the previously mentioned

feature and is also attributed to a magnetite iron formation

source . Tt is interpreted as either an isoclinally

folded repetition of the main magnetite iron formation

zone or else a faulted segment. If the latter inter

pretation is taken, the fault would have to strike at

N70W in order to achieve the noted geometric relationship.

A third linear mag feature is at 240N on lines

3000E to 3360E. It is another stratigraphic feature

of iron formation character but of short strike length.

A series of north striking weakly magnetic features

marked by low cimplitude ( +1 0 00"^ above background) isolated

peaks and ridges coincide with what are interpreted

as diabase dikes. These occur randomly across the claim

group. The more prominent dike related magnetics occur

along or parallel to lines 240E, 480E, 4080E, 4440E

and 57GOK. Other possible dikes which occur as more

7

subtle features are along L120E, L1920E, L2640E, L3240E,

1,384 OE and L5160E.

1'he only other notable magnetic feciture on grid

A is an irregular pattern in the northwest under claims

586865, 586874, 586875 and 515915. The bullseye pattern

with anomalies to 1500"Zf above background suggests the

underlying presence of ultramafic intrusives such as

arc found to the immediate north and are responsible.for

the pattern seen on map 2c.

Magnetics of grid B are dominated by a linear bullseye

pattern along the entire length of the grid from along

the baseline to the west edge of the grid. The 60,000"^

contour essentially marks the eastern limit. To the

east of this the magnetics are flat with not more than

100 7f variability throughout except where magnetic ridges

corresponding to the presence of diabase dikes are seen

{e.g. through the centre of claims 586236, 515914, 515911

etc and along the west side of claims 586887, 586886

etc) .

The bullseye pattern with highs locally to 6000 "if

above background correspond to a N30E trend and confirms

the presence of pyroxenite intrusives such as that rioted

in outcrop at 30E on L3480N. These intrusives are apparently

located somewhat randomly within non magnetic rocks

of volcanic origin such that magnetics between the pyroxe-

nilic intrusives decrease to background intensity,

b) VLF - Results of the EM-16.VLF survey are plotted

as profiles on maps 3a, 3b and 3c. Conductor traces

are illustrated by solid lines.

In the Grid A area a network of more than forty

parallel to sub-parallel conductors cross the entire

area from west to east. None have a configuration typical

of bedrock conductors close to the surface. However,

four (lettered A, B, C and D) show characteristic profiles

of deeper bedrock conductors with moderate to good conduc

tivity. Their symmetrical profile shape is typical

of near vertical sheet like bodies. Qualitiative data

is supplied by the HLEM data which is discussed in the

next section.

The remainder of the conductors are typical of

sources having weaker conductivity. Peak to trough

distances of greater than 120 metres and asymmetry of

the profile suggest Cciusative features related to variable

thicknesses of conductive overburden (i.e. buried overburden

filled valleys and edge effects). Nevertheless, the

conductive trends which range up to 1600.metres in length

are sometimes parallel to magnetic trends, and hence

could be related to either bedrock lithologies which

c'ire less resistant or to shears.

VLF EM results over Grid B are erratic and peaky

because of the presence of outcrop hummocks and sand

hills separated by swamps and overburden filled bedrock

troughs. Conductors are mostly sub-parallel conductors

and have characteristics typical of edge effects along

either outcropping and buried outcrop knobs, creek bottoms

or overburden troughs. Except in certain instances,

their continuity from line to line has been interpreted

somewhat arbitrarily assuming a strike direction sub-

parallel to the baseline i Poor directional coupling

of the grid in relation to the location of the Cutler

transmitter station hcis helped to compound the inter-

pretational problems in this type of terrain.

Typical of grid B conductors is the one which coincides

with the beaver pond on line 3000N at 300E. This feature

traces the creek val l ey both north and south of the pond

and can be attributed to the overburden filled valley

which is mapped between outcrop hills on each side.

A weak shear in the underlying trough could be responsible

for some enhancement of the anomalous amplitude but

~ Q ~

overburden thickening is the dominant force.

Qua]d tatj ve appraisal of these weak conductors

will be discussed in the next section covering HLEM

results.

c) HLEM - Horizontal loop EM results are plotted as

profiles on maps 4a, 4b, 4c and maps 5a, 5b, 5c for

444 hz and 1777 hz respectively.

In the grid A area (maps 4a, 4b, 5a and 5b), four

boncifide bedrock conductors are detected in the central

part of the grid to the north of the baseline. Anomaly

A is 110 metres long and is very narrow wi'th a vertical

or near vertical dip. Estimated depth is approximately,

40 metres. There is no mag association and conductivity

thickness values are low as evidenced by the rapid decrease

in IP/OP measured at 1777 hz and at 444 hz.

Anomaly B is directly on strike with anomaly A

and is probably on the same horizon. As shown on maps

4a and 4b it is composed of two thickenings for a 2000

metre strike length. It varies from O to 15 metres

in thickness. The thickest and most conductive part

of the body is at the eastern end on line 3240E at 240N

where it is calculated to have greater than 18 mho

conductivity -thickness and to have a 60 metre depth.

Immediately to the east on line 3360E a depth estimate

of greater than 44 metres and a conductivity-thickness

value of greater than 10 mho is calculated. Although

there is no magnetic response indicated for anomaly

B, the portion from L2880E to L3360E has a linear mag

high of greater than 12000 V parallel and flanking at

30 metres south.

Anomaly C is a 360 metre long conductor centred

at 4ON on line 3000E where is has its maximum calculated

thickness of approximately 20 metres. Conductivity-

thickness is approximately 30 mho and depth is 40 metres,

-10-

It Ides 150 metres to the north and parallel to the

strong magnetic feature producing the -44200"^

mag high of map 2b.

Anomaly D, which defines a short 20 metre wide

bedrock feature at 45N on line 3840E shows up on only

two picket lines. It has a conductivity-thickness value

of greater than 30 mhos and is estimated to be less

thc'm 45 metres deep. It appears to be on strike with

anomaly C but a direct magnetic correlation of up to

5000 o suggests a different causative source.

Only two other types of anomalous responses are

noted for Grid A - namely weak out-of-phase responses ,

and local high in-phase peaks. The former type of response

is widespread and is illustrated on maps 4a, 4b, 5a

and 5b as dashed lines defining axes of weak out-of-

phase trends. They vary from single line anomalies

to ten line anomalies and are typically quite readily

traceable. The lack of in-phase response and decrease

in intensity from 1777 hz to 444 hz puts their cause in

the category of overburden filled bedrock troughs adjacent

to bedrock ridges. The lack of significant response

at 444 hz confirms this interpretation although bedrock

shears could be coincident with some and could be partially

responsible for the trough and ridge configuration of

the bedrock surface.

VLF anomalies are seen to coincide exactly with

the weak HEM responses.

Positive in-phase responses occurring from L1680E

to L3480E and from L4680E to L5760E are the only remaining

cinomalous responses. These are directly attributed

to nuignetite in magnetitic iron formation. The fact,

that amplitude of the readings remains constant at both

444 h z and 1777 hz and that no anomalous out-of-phase

response is produced substantiates the interpretation

of narrow magnetic, non-conductive tabular bodies. Positive

] P responses are produced only when either the transmitter

or receiver is directly over the magnetic body. Unlike

a true conductor, no anomalous readings are noted when

the body is straddled by the two instruments.

-31-

For Grid B (maps 4c and 5c) anomalous responses

arc produced by effects of variable overburden thicknesses

and by effects of magnetite in the bedrock. As with

Grid A, overburden features are defined by negative

out-of-phase responses. The majority are parallel or

sub-parallel to the regional stratigraphy and are hence

believed to be related to a bedrock topography dominated

by differences in hardness of the volcanic and intrusive

units. Conductors to the south of the baseline from

L1320N to L3120N coincide remarkably well with the south

edge of pyroxenite intrusives. Two others in the vicinity

of 81OE on L1800N correspond very closely with an inter

pretation conforming to a bedrock ridge along the diabose

dike defined by magnetics on map 2c.

The remaining anomalous feature of Grid B coincides

with highw^^y 144 from 360N to 1560N and has a character

typical of a grounded wire. The negative out-of-phase

response is normal for an overburden response but the

f]at bottom to the profile indicates a flat cylindrical

source. It is concluded that the grounding of the wire

causes it to take on the conductivity character of the

overburden or hence only an out-of-phase response.

Summary

Results of the mag, VLF and HEM surveys illustrate

a si nip] o pattern of magnetics and conductivity as follows:

(a) grid A shows a predominant E-W lithologic trend

dominated by a strong mag feature over the eastern two-

thirds of the grid. The intensity of the magnetics

is typical of magnetic iron formation for the most part.

However, an ultramafic flow or intrusive is interpreted

for a shorter mag feature at the north edge of the main

mag high;

(b) magnetics in the central part of grid A indicate

cither a thickening by folding or else a repetition

of magnetic horizons;

.../l 2

-12-

(c) associated with the wide mag zone of grid A are

four moderate bedrock conductors with little to no coinciden

magnetic response;

(d) diabase dikes show up as weak north trending magnetic

ridges;

(e) weak conductive trends conforming to edges of bedrock

ridges occur throughout the gird;

(f) no conductors of merit are noted on Grid B. However,

a number of weak features related to buried bedrock

topography are recognized;

(g) irregular magnetic features of Grid ,B are coinbident

with pyroxenite sills which are partily exposed in the

northern part of the grid. Diabase dikes show up as

magnetic ridges striking due north.

Ontario

APPENDIX I

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.

Type of Survcy(s) ____Y^IL'... MfL?JL 21EI"L....—,. —— Township or Area . Br i s tol b Thor ne loe Twps

Claim Ilolder(s). ... Preussag .Canada.^LjJlit

Survey Company^. Pr

Author of Report . T T E. Warden __ _ - ————^^————-——— Address of Author. JkiLl ^Righrnon^ St . VI, Penthouse FI^

Toronto, OntarioCovering Dates of Survey _ .^,j.an,JL. - Jnnp, 2 Q, 1981

(linecuttirig to office)

Total Miles of Line Cut-. ____ 85.5 miles (136.8 km)

.

SPECIAL PROVISIONS CREDITS REQUESTED

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

ENTER 20 days for each additional survey using same grid.

DAYS per claim

40Geophysical

VLF - Electromagnetic

- Magnetometer—

— Radiometric,——————

Other_________20

20

Geological.

Geochemical.

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

Magnetometer_____Electromagnetic _____ Radiometric .-———

DATE:.

(enter days per claim)

SIGNATURE:Author of Report or Agent

i* -J fcO wt/3u

Res. Geol.^ ,

Previous Surveys File No. Type

_ Qualifications....

Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

See attached list(prefix) (number)

6 •o B

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS li more than one survey, specify data for each type of survey

Number of Stations ___ i2j04 _________ __________ Number of Readings VLF S. Mag 4204, Ijifc

Station interval .........AOjl^res __ ___________ Line spadng -120jnetres ____________ 'HEM; l cm ^Profile

Contour interval Mag 250 gammas

H

aWyto

.H

Oi

Instrument .Accuracy — Scale constant ___r—zDiurnal correction method. Return to base station regularly

Base Station check-in interval (hours)__ 2 hours_________________Base Station location and value Established base lines for Grid A S B

Instrument _ Apex Parametrics Max Min II

Coil configuration ____Horizontal Loop

Coil separation _.......Accuracy .^ . ^ ...... ... L A/ 2 . ?erCenfc .

120 metres

, Method: CD Fixed transmitter CD Shoot back 0 In line CD Parallel line 444 hz S, 1 77 hzFrequency__.O

W J ' ' (specify V.L.F. station)W Parameters measured IP and OP at both frequencies

Instrument ^^

Scale constant _ ^Corrections

Base station value and location _____...,.__________

Elevation accuracy.^ —

Instrument —Method LI Time Domain CD Frequency Domain

Qp; Parameters- On time__..^^. ._....^..._______________ Frequency_____

N tx 2 H

t—*

2 fe ti-i i—(D [ii Power __U ^ Electrode array ~-

Off time ______._____________________ Range —Delay time __ ^. _____________________

Integration time ___._....__._____________

Electrode spacing _—. -^—- - —

Type of electrode ____...____

Instrument___......_....___..._..—.,......_.__.___________________ RangeSurvey Method _ ,, . ... ......... ....-..,.......-..—.......-_—.__________________.

Corrections madeM

Instrument_

Values measured _ ......_- -^__ __________Energy windows (levels) __—————^—————-Height of instrument___. _.,._ ____________________Background Count. Size of detector-_.-...._._______________________________________Overburden —..——...__... ......^. . — — .^..____————.—-———-—--———---.———-—-——.—--^

(type, depth — include outcrop map)

THKKS (SEISMIC, DRILL WELL l/KiGJNG ETC.)of survey__,- .^ _ .YML—J™,--—.————

Instrument_______Geon ic^ JEM^G^_

Accuracy___......__.Parameters measured.

Additional information (for understanding rcsnlis) Transmitter = Cutler Maine 17.8 k Hz - all readings taken facing southerly

Type of survey (s) -.-.—....- -..—... _—-..—.-—...-_———~—————————Instrument(s) __—..-..—_-————————————————————————

(specify for each type of survey)Accuracy__________.-__.___..____..__________..——

(specify for each type of survey)Aircraft used____^.....,..—... . —....____..._.______________Sensor altitude___ ——^—Navigation and flight path recovery method ...m.

Aircraft altitude____.___.________________________ Line Spacing ——. Miles flown over total area__ _^______.--_____________Over claims only..

GKOCHKMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken..,

Total Number of Samples. Type of Sample.

(Nature of Material)

Average Sample Weight——————— Method of Collection———————--

Soil Horizon Sampled.

Horizon Development. Sample Depth————.Terrain——————

Drainage Development——————.—————

Estimated Range of Overburden Thickness...

ANALYTICAL METHODSValues expressed in: per cent d

p. p. m. CDp.p. b. D

Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-( circle)

Others.—-^————--——-.----.-—--.——--^————

Field Analysis (.-Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. -————-———-.

SAMPLKI'RKl'ARA'riON(IncliiHes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis -—-——.

Extraction Method.Analytical Method — Reagents Used ———

Commercial Laboratory (- Name of Laboratory.— Extraction Method- Analytical Method.. Reagents Used ^^———

.tests)

.tests

.tests)

General- General .

M3N3NG CLAIMS TRAVERSEDAPPENDIX II

Number c

5P63 9266

P619267

P495307 20 c

P495308 20 d

P495309 2 0 d

P515901 20 d

P51S906 80 d

P535907

P515908

P535909

P515910

P515911

P515912

P525913

P5 3^914

P53 935

A P553050

P553053

P553052

P553053

P553054

P553055

P553865

P fi S 3 8 C 6

P530884

P583234

PS86228

P586229

P586230

P586231 ^

)f Days that can be Applied

ays P 5 86232 so

P5.86233

PS86234

' P586235 ays

P586236ays

P586237ays

P586238ays

P586239ays

P586240

P586261

P586264

P586265

P586864

P586865

P586866

P586867

P&86868

P586869

P586870

P586871

P586872

PS86873

P f Q C D "~1 A ^5 O O O 7 T

P586875

P586876

PS86877

P586878

P586879

P586880

P586881

f P586882 ,^

to Each Claim

days P586883 80

P586884

P586886

P586887

P586891

P586892

P586893

P586894

P586900

P58.6901

P586902

P586904

P586905

P586906

P586910

P586911

P586912

P586914

P586915

P586916

P586918

P586919

P586920

P586922

P586923

PS86924

P596926

P586927

P586928

P596927

f 9 3 Claims

days

CM

Godfrey Twp.-M.284

23M. BASE LINE 22 M.

jL---i--- -l--- —— t****. .9*9.* ' 506703 , 508702 595996 5959 57 i 598958 , 5989591 595960 595961 , J l——— li"-P~ ' P f P |P 1522255,522253 l , ^ '' —— .4 — - M .. J____j.. - - -u,- - - -——| P T

553206/5532051853201 |983200 l~- - t~p- ~ ~r~P~ ~T V ~T p |~p Tp l P P P | P | P l P U 28 , 60J

-PH"."; -t-7-t——p""U." 1553,94 '853,93 553,90 l l 928,72 W"' .526 I 70 ,528,63 , 528,62 1528,6, , ^

5M.-

4M.- -

5532,6 1553217 J5B32I8 Tp __ - l - - J-- __J '

p j P l P j jl l .460315 ,479904 \f_i_ ^.

553221 1653220 J 553219 |—- —— 4p- f, /p \

3M

2M.

l M.

148 1147 553203 1553196 j,P

f ; ' i 11 553207/8532041983202 |S53I99 .

1—rn r-1—r- 1 l l l

150870^50870! l"^J52996^p29954 J529953I•J p~ ~ ~ 7 P~ ~ ~ i" ~P~ -~- L-— -----

\ V turvayfld 2IM\ [ in 1 399 by O ,L.S. ^ 2-0 M. A . NIVEND l D

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2M IM.

Thorneloe Twp. - M. 313

K. K.42A86SW0206 2.3973 BRISTOL 200

THE TOWNSHIP OF

BRISTOLDISTRICT OF

COCHRANE

PORCUPINE MINING D IVISION

SCALE: 1 -INCH-4O C HAINS

DISPOSITION OF CROWN LANDS

PATENT, SURFACE AND MINING RIGHTS ..__ *" , SURFACE RIGHTS ONLY_______. O" , MINING RIGHTS ONLY _______. 9

LEASE, SURFACE AND MINING RIGHTS___ B" t SURFACE RIGHTS ONLY^______. HH , MINING RIGHTS ONLY ________ H

LICENCE OF OCCUPATION____________ T

ROADSIMPROVED ROADSKING'S HIGHWAYS

RAILWAYSPOWER LINESMARSH OR MUSKEGMINES

CANCELLED

, NOTES

400' Surface Rights Reservation along the shores of all lakes 8, rivers

Areas withdrawn from staking under Section 43 of the Mining Act t R.S.0.19701.

Order No. F ile Date Disposition164584 Surface Rights Only.

DWE OF ISSUE

FEB101982

This township lies within the Municipality of the CITY Of TIMMINS.

PLAN NO. M-264ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

roNOJ

cO)Q

Bristol Twp. M.264

5M-

61265553865 5586S7P-J 58^880 , ,, (

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Me Keown Twp. M.299

2-3973 BRISTOL

THE TOWNSHIP OF

THORNELOE

DISTRICT OF COCHRANE

PORCUPINE MINING DIVISION

SCALE: 1-INCH 4O CHAINS

LEGEND

PATENTED LAND

CROWN LAND SALE

LEASESLOCATED LAND

LICENSE OF OCCUPATION

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

ROADSIMPROVED ROADSKING'S HIGHWAYS

RAILWAYS

POWER L INESMARSH OR MUSKEG

MINES

CANCELLtDPATENTED S.R.O.

ce

NOTES :

400' Surface Rights reservation along the shores of ali lakes and rivers.

Reservation for Deputy Chief Ranger's Headquarters site shown thus •••••••vi F ile 1 10657

Flooding rights on Mattagami River 8 Kenogamissi Lake are r eserved to Ont. Hydro- L.O. 7598

File 1163 vol.3

Areas withdrawn from staking under Section

43 of the Mining Act t R.S.O. 1 970.) Order N- Fil*—— Pu l ffi Disposition

FEB10882

Ministry of Natural ResourcesTORONTO

S.R.O.

SAND and GRAVEL

( j) M.N.R. GRAVEL PIT 256 , FILE III46T

g) GRAVEL FILE 143834

5) M.N.R. GRAVEL RESERVE

This township lies within the Municipality of the CITY of TIMMINS.

PLAN NO. M.3I3ONTARIO

MINISTRY OF NATURAL R ESOURCESSURVEYS AND MAPPING BRANCH

\ \ ?,9??

PREUSSAG

TIMMINS WEST CLAIM GROUPGrid A

WEST HALF)

TOTAL FIELD MAGNETICSi—i i—i i—i ]—i l—t "1

Map 2a

Contour Interval - 250 gammas(l000gammas in areas of

high gradient )Operator - F. A. Hodgkinson

Instrument - Scintrex MP-2

Date - May 18I

515909

60323

51591560283

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PREUSSAG

TIMMINS WEST CLAIM GROUPGrid A(EAST H ALF)

TOTAL FIELD MAGNETICS100 100 200 300 Metres

March 81 Scale l! 3,000

Map 2bNTS 42/A/5

Contour Interval - 250 gammas(l000gammas in areas of

high gradient )

Operator - RA. Hodgkinson

Instrument- Scintrex MP-2

Date - May '81

4440 E

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PREUSSAG

TIMMINS WEST CLAIM GROUPGrid B

TOTAL FIELD MAGNETICS100 100

March 81 Scale 1:3,000

Map 2c

Contour Interval - 250 gammas(lOOOgammas in areas of

high gradient )Operator - F. A. Hodgkinson Instrument - Scintrex MP-2

Date - June '81

59 735

55386659799

200 300 Metres

NTS 42/A/5

—— BOO W

—— 870 W

—— 840W

—— 810W

—— 78OW

—— 75OW

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—— 660W

—— 63OW

—— 6OOW

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" — 5IOW

—— 48OW

—— 45QW

—— 42OW

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—— 36OW

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PREUSSAG


VLF EM515908

Map 3a

In-Phase Profile

Quadrature Profile

Profile Scale : l cm to IO GXo

In Phase Quadrature

Conductor Trace.515909

Operator-B.Beaulie (facing south) Instrument- Geonics EM-16 Date -May '81

\ 515915

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March ' 81 Scale l: 3,000

Map 3b

•x In-Phase Profile

*——* Quadrature Profile

Profile Scale i l cm to I07o

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l

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300 Metres

In Phase Quadrature

4440E

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Date - May '81

-2

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424065*0206 2 .3973 BRISTOL 290

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42A06SW0Z06 2.3973 BRISTOL310

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—— 750 N

—— 720N

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—— 660 N

—— 630 N

—— 600 N

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—— 450 N

—— 42ON

—— 39ON

—— 360 N

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4440 E

N0l-89l2-89O3-8994-90O

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48OS

5IOS

54OS

5705

6005

6 3O S

660 S

69OS

72OS

7505

78OS

8 tO S

87OS

BOOS

4440 E

—— 660N —— N0I-89I

-8

1 1" 5 i

-4

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^-^ ————'Yi

II X

\/' ^t

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9

10

9

14

II

,,

8

S

4

0

49,

N0 I-9182-9173-9214-922

2 * N0 f-9IO2-9O93-913

z jt 4 -9/4

1-90O2-8993-9O34-904-4

586918

\586904586900

586915 ' 586919

3-900 6 ?:4-9OI \\ l 586911 ;586905. \

/i! 586920N0l-893

2-8923-9014-902

586912

586902

N02-9I6 3 ,x

A

X

x\288OE

42A86SW0206 2 .3973 BRISTOL 260

N

PREUSSAG


VLF EM100 100

March 81 Scale i:3,000

Map 3c

x In-Phase Profile

i——* Out-of-Phase Profile

Profile Scale i lcm to \07o

4- ve -ve

14

-23

-5

-14

-9

In Phase Out of Phase

Operator -B.Beaulie Instrument- Geonics EM-16 Date -June '81

\J6I9267 '

200 300 Met res

NTS 42/A/5

Conductor Trace —

9OOW

870 W

840 W

810 W

780 W

7SOW

72OW

69OW

66OW

63OW

6OOW

57OW

54OW

stow

48OW

45OW

42OW

39OW

36OW

33OW

3OOW

270 W

24OW

2IOW

18OW

150 W

i2O W

9OW

60 W

SOW

OO

3OE

60E

9OE

I2OE

t SO E

ISO E

2IOE

240E

27OE

300 E

330E

36OE

39OE

42OE

450E

- 480 E

- 5IOE

- 540E

- 57OE

- 6OOE

- 63OE

- 660 E

- 690 E

- 720E

- 75OE

~ 780 E

- 8iOE

- 840 E

- 87OE

- 900E

,

PREUSSAG


WEST HALF)

HLEM 444hz100 O

I—I t—l l—l l—l l—l l-iOO 200

March 81 Scale 1:3,000

Map 4aNTS 42/

)09

x In-Phase Profile Out-of-Phase Profile

Profile Scale ; l cm to I0 07o Instrument Max-Min HOperators- F A. Hodgkinson, B. Beaulieu

Coil Separation - 120metres

Axis of Very Weak Conductor (Centre of Overburden Trough)

Bedrock Conductor Trace

-ve

Out of Phase

i

West Sheet

586236

In Phase

Date- May '81

A/ 0 f-2322-9O93-2364-23T

N0 t-237 -236

3-2624-263

586237

1-8912-8903-8994-9OO

586891586238586264586233

586265 586892586234

N 0l-893 - \2-892

586884

586240 \ 586893586235

N02-235 3-24O

N 0 2-893 3-9O2

O3

300 Metres

-2

y/ 70 N

H40N

IIION

IO8ON

S05ON

IO20N

990N

960N

930N

870 N

/V

750N

T2ON

69ON

660N

63ON

GOON

570 N

54ON

5ION

48ON

450 N

42ON

33ON

27ON

240 N

l SON

60N

ION

00

60S

330-

BIOS

84O

8?O S

9OOS

93OS

96OS

28 80 E

3773PREUSSAG

TIMMINS WEST CLAIM GROUPGrid A(EAST HALF)

HLEM 444hz100 300 300 Metres

March '81 Scale i: 3,000

Map 4bNTS 42/A/5

(——x In-Phase Profile

,——* Out-of-Phase Profile

Profile Scale ! icm to I07o Instrument Max-Min H Operators - F A. Hodgkinson, B. Beaulieu

Coil Separation - 120metres



4- ve -ve-3

3

O

4320 f

-l

444O E

-4 -l


Date- May'81

X -l

x -i

A/ 0 f -926 2-925

N0 l-922 5O4OE 2-92!

3-9254-926N0I-9I4

2-9133-917

9/8N 0I 9(8

2-9/73-9214-922

586926

586922586918

586927

586923586919

K -2 -3

586928X -2

-595027•x -i

X -l -3

586920-K -2 -3

586924

N02~928 3-027

N02-92O 3-924

N02-9I6 3-920

504OE

IO2ON

99ON

960 N

93QN

9OON

87ON

84 ON

8ION

780 N

7SON

T20N

69ON

660 N

630 N

600 N

570 N

54ON

5ION

48ON

45ON

42ON

390N

36ON

33ON

300N

270 N

24ON

2 ION

I8ON

I5ON

I20N

9ON

60N

3ON

OO

3OS

60S

90S

/?OS

150 S

ISO S

2105

240 S

270 S

N02-027 __ m r ——

33OS

3605

39OS

4205

45OS

4805

510S

54OS

57OS

6OOS

63OS

66OS

6 90S

72OS

750 S

78OS

8IOS

84OS

8 70S

9OOS

N

PREUSSAG


HLEM 444hz100_____________O

100 200


Map 4c

x——x In-Phase Profile* —— * O ut-of- Phase Profile

Profile Scale \ l cm to I07o Instrument Max-Min HOperators - F A. Hodgkinson, B. Beaulieu Coil Separation - IZOmetres

3840N r

Date - June '81


-ve

In Phose Out of Phase

O 9 X

553051O 9 X

/j 495308 j

-l 2 x

583234-l 2

300 Metres

NTS 42/A/5

9OOW

87OW

840 W

8 IOW

780 W

750 W

720 W

69OW

66OW

63OW

60OW

57OW

54QW

510 W

43OW

45O W

42OW

390W

360 W

33OW

3OOW

270 W

2 tO W

180 W

ISO W

!2OW

60W

3OW

00

3OE

6OE

9OE

1 20 E

i 50 E

I8OE

2IOE

24OE

270E

3OCE

33GE

360 E

39OE

4 2O E

450E

480 E

5IOE

54OE

57OE

600E

63O E

66OE

690 E

72OE

7 50 E

78OE

8IOE

84OE

87OE

90OE

PREUSSAG

TIMMINS WEST CLAIM GROUPGrid A(WEST HALF)

HLEM 1777hz100 Oi-l l—l l—l t—l t-rq^

100 200 300 Metres

March 81 Scale l : 3,000

Map 5 aNTS 42/A/5

——x In-Phase Profile——* Out-of-Phase Profile

Profile Scale ". l cm to I07oInstrument Max-Min H.Operators -FA. Hodgkinson, B. Beaulieu

Coil Separation - IZOmetres



I2OON

II7ON

II4QN

HtON

IO8ON

I050N

IO2ON

990N

960N

—— 93ON

—— 9OON

West Sheet

586236


Date- May 81

N 0 l- 2372-2363-2624-263

1-89!2-89O3-8994-9OO

586891586238

586264

2-891 03-9OO

4-9O!continued

586892586265

586239

586884586893

586240586235

N0 2-893 3-9O2

i-X

PREUSSAG

TIMMINS WEST CLAIM GROUPGrid A(EAST HALF)

HLEM 1777hz100 100 200 300 Metres


Map 5bNTS 42/A/5

,—— K I n-Phase Profile f'-—* Out-of-Phase Profile

Profile Scale i l cm to I0 07o Instrument Max-Min H Operators - FA. Hodgkinson, B. Beaulieu Coil Separation - I20metres



-f ve —*- ve

-5444OE

O

-3

-2

-2

n Phase

Date-May'81

Out ot Phase i

N0 l-922 504OE 2-921

3-925

5I6O E

IO2ON

99ON

960 N

93ON

9OON

870 N

84ON

8ION

78O N

7SON

T20N

69ON

660N

63ON

6OON

57ON

54O/V

5ION

480 N

450 N

42ON

390 N

36ON

33ON

SOON

270 N

24ON

2 ION

I8ON

/50N

120N

9ON

60N

SON

oo

3OS

60S

90S

12OS

150 S

180S

2IOS

240 S

27OS

3OOS

33OS

36OS

39OS

420 S

45OS

48OS

5IOS

54OS

5 70S

GOO S

63OS

66O S

69OS

72OS

7SOS

78OS

8IOS

84OS

87OS

9OOS

N

PREUSSAG


HLEM 1777hz100 100 200

Marcti '81 Scale 1:3,000

Map 5c

x——x In-Phase Profile .——* Out-of-Phase Profile

Profile Scale l l cm to I07o Instrument Max-M in IEOperators -FA. Hodgkinson, B. Beaulieu

Coil Separation - IZOmetres

l Date - June !8I



300 Metres

NTS 42/A/5

900 W

-ve

840W

e tow

78OW

75O W

72OW

69OW

66 O W

6 30 W

6 00 W

57OW

54OW

5 IOW

48OW

45OW

42O W

390 W

36OW

33OW

3OOW

270 W

2 to W

180 W

1 50 W

t 2O W

9OW

6OW

3OW

OO

30 E

60 E

90 E

1 20 E

iso e

18OE

2IQE

2405

27OE

3OGE

330E

36OE

390E

4 2O E

450E

48OE

5IOE

540E

57OE

6OOE

63OE

66OE

6 90 e

720E

750 E

78OE

810 E

84OE

87OE

9OOE

RPT ON GEOPH SUR 1981 MAG VLF HEM...42A06SW0206 2.3973 BRISTOL 010 PRKUSSAG CANADA LIMITED TIMMINS...

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Transcript of RPT ON GEOPH SUR 1981 MAG VLF HEM...42A06SW0206 2.3973 BRISTOL 010 PRKUSSAG CANADA LIMITED TIMMINS...