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BELL LAKE 010

RECEIV .-j

OCT 1 5PROJECTS SECTION

REPORT ON THEINDUCED POLARIZATIONAND RESISTIVITY SURVEY

CANADORE OPTION, TELEPHONE LAKESTURGEON LAKE AREA,

PATRICIA MINING DIVISION, ONTARIOFOR

NEwcoNEX CANADIAN EXPLORATION LTD.

McPHAR GEOPHYSICS LIMITED

REPORT ON THE

INDUCED POLARIZATION

AND RESISTIVITY SURVEY

CANADORE OPTION, TELEPHONE LAKE

STURGEON LAKE AREA,

PATRICIA MINING DIVISION, ONTARIO

FOR

NEWCONEX CANADIAN EXPLORATION LTD,

i J

1. INTRODUCTION

At* requested by Mr. Patrick H. Taylor, Vice President of Newconex

Canadian Exploration Ltd., we have carried out an Induced Polariiation and

Resistivity survey on the Canadore Option near Telephone Lake in the

Sturgeon Lake Area of Patricia Mining Division, Ontario.

The claim group is adjacent to the property of Mattagami Lake Mines

Ltd., and New Brunswick Uranium Metals and Mining Limited, on which a

new copper-rinc-sllver discovery is presently being outlined. The geology

of the area is covered by ODM Preliminary Map P670. Several outcrops of

felsic m e t* volcanic rocks occur along the southern portion of Claw Lake and

appear to lie on strike with the sequence in which the Falconbridge-Mattagami

discovery was made.

Previous magnetometer and horiiontal-loop electromagnetic surveys

have been carried out over the property. The purpose of the Induced Polarization

and Resistivity survey was to outline any anomalies which could indicate the

- 2 -

|prceence of base metal eulphide mineralization associated with the underlying

volcanics.

The Burvey was carried out over the following claims, believed to be

owned or held under option by Newconex Canadian Exploration Ltd.

PA 205910 PA 205911 PA 205912 PA 205913 PA 205914 PA 205918 PA 205919 PA 205920 PA 205921 PA 205922 PA 205923 PA 205924 PA 205925 PA 205926 PA 205927

PA 225025 PA 225027 PA 225028 PA 225029

PA 227153 PA 227154 PA 227155 PA 227156 PA 227157 PA 227158 PA 227159 PA 227174 PA 22.7175 PA 227180 PA 227181 PA 227182 PA 227183

PA 227209

2. PRESENTATION OF RESULTS

The Induced Polarisation and Resistivity results are shown on the

following data plots in the manner described in the notes preceding this report.

Line

36 W

40W

44W

48W

52W

56W

60W

Electrode Intorvals

200 feet

ZOO feet

200 feet

200 feet

200 feet

200 feet

200 feet

Dwg.No.

IP 5461-1

IP 5461-2

IP 5461-3

IP 5461-4

IP 5461-5

IP 5461-6

IP 5461-7

- 3 -

Line

64W

68W

(Repeat)

(Extension)

72V/

(Extension)

76W

BOW

84V/

88W

92W

96W

(Extension)

100W

104W

108W

JiTlectrode Intervale

200 fee'

200 met

"00 feet

200 feet

100 feet

200 feet

200 feet

100 feet

200 feet

100 feet

200 feet

ZOO feet

200 feet

100 feet

200 feet

100 feet

200 feet

200 feet

100 feet

200 feet

1 00 feet

?00 feet

100 fc-et

200 feet

D w fi. N o,

IP 5461-8

IP 5461 -9

IP 5461-10

IP 5461 -11

IP 5461-12

IP 5461-13

IP 5461-14

IP 5461-15

IP 5461-16

IP 5461-17

IP 5 461-18

IP 5461-19

IP 5461-20

IP 5461-21

IP 5461-22

IP 5461-23

IP 5461-24

IP 5461-25

IP 5461-26

IP 5461-27

IP 5461-28

IP 5461-29

IP 5461-30

IP 5461-31

ne

112W

116W

120W

124W

128W

152W

136W

Electrode Intervale

200 feet

100 feet

200 feet

100 feet

200 feet

200 feet

200 feet

?00 feet

100 feot

200 feet

L. No.

IP 5461-3?

IP 5461-33

IP 5461-34

IP 5461-35

IP 5461-36

IP 5461-37

IP 5461-38

IP 5461-39

IP 5461-40

IP 5461-41

Also enclosed with this report is Dwg, I. P. P. 4777, a plan map of the

Telephone Lake Grid at a scale of l " - 400'. The definite, probable anil possible

Induced Polarization anomalies are indicated by bars, in the manner shown on

the legend, on this plan map ae well as on the data, plots. These bars represent

the surface projection of the anomalous zones as interpreted from the location

of the transmitter and receiver electrodes when the anomalous values were

measured.

Since the Induced Polarisation measurement is essentially an averaging

process, as are all potential methods, it is frequently difficult to exactly pin

point the source of an anomaly. Certainly, no anomaly can be located with

more accuracy than the electrode interval length; i.e. when using 200* elec

trode intervals the position of a narrow sulphide body can only be determined

to lie between two stations 200' apart. In order to definitely locate, and fully

- S -

evaluate, a narrow, shallow source it if. necessary to uce shorter electrode

intervals. In order to locate source.^ at sor..e depth, largwr electrode interval

must be ueed, with a corresponding Increase in the uncertainties of location.

Therefore, while the centre of the indicated anomaly probably corresponds

fairly w*ll with source, the length of tne indicated anomaly along the line

should not be taken to repreaent the exaci edges of the anomalous material.

The magnetic information nhown on Dwg. I. P. F 1 . 4777 hat been taken

from maps made available by the staff of Newconex Canadian Exploration l td.

3. riSCUSSION OF K I". S D ITS

The resistivities in the area are generally quite high, suggesting

relatively non-poroue, unaltered bedrock. An attempt was made to correlate

the changes in resistivity from line to line, and thereby perhaps delirr.it the

different rock typee; however, the changes in the depth and conductivity of the

overburden have apparently caused the greatest variations in the resistivity

data, and the attempt has been abandoned. It may suffice to say that the very

high apparent resistivities (noted, for example, near BS on Line l 32W and

between l OS and IBS on line 100W) usually correlate with the dense, non-

porous acid volcanic sequences,

As a result of the high resistivity background, the apparent Metal Factor

3values are quit* low. Values greater than 1.0 are above background and, la

most cases, have been marked ae "possible" anomalies. K;any of these weakly

anomalous features follow linear trends and have been correlated into zones.

Each zone will be discussed individually.

- 6 -

IZone A

The zone indicates a shallow, narrow source. It ie best defined and

strongest on Line 52W. On this line a source lees than 200 1 wide appears to

lie within 100' of the surface near 31N. Mnce the frequency effects are not

very high, the strong resistivity low may be caused by a fault or shear zone.

Zone B

This zone suggests a similar narrow, shallow source lying parallel to

Zone A. The apparent resistivities are not quite as low, but the frequency

effects are slightly higher and consequently more indicative of a metallic-

conducting source.

Zone C

The cone correlates well with a weak magnetic feature. There is an

increase in frequency effect as well as a resistivity low. As illustrated by

the Case History in the Appendix, the anomalies could be caused by a shallow

source whose width is much less than the 200* electrode interval.

The source should be detailed with 100' and perhaps even SO' electrode

intervals along Line 68W and Line 72W.

Zone D

This zone correlates with a more prominent magnetic feature. The

most definite response occurs on the data obtained using 100' electrode intervals

on Line 76W. A narrow source within SO 1 of the surface and possibly dipping to

the south is indicated near 18N. The anomaly pattern on Line 72W is more

complex. Compare with the results over a vertical conducting cylinder

(Model Case VI-0. 25-BX-250-a).

Zone E

The zone correlates with the eastern portion of a long, relatively weak

magnetic trend. The strongest K'eta l Factor response coincides with the

strongest magnetic reoponse near 12N on Line 52\v and indicates a narrow

source probably within 100' of the surface. Unfortunately the IP data ie

incomplete.

Zone F

This zone lies on the flank of the came magnetic feature as Zone F,.

The anomaly near l 5N is characterized by a frequency effect high on the data

obtained using 200' electrode inteivals, and by a resistivity low on the data

obtained using 100' electrode intervale. The anomalies suggest a narrow,

metallic-conducting source within 50' of the surface.

Zone G

This zone lies along the western section of the same weak magnetic

trend as Zone E and Zone F. The anomalies are very weak and poorly defined.

They suggest a shallow source.

Zone H

There is no magnetic association with the zone. The anomalies suggest

a possible weak source within 100' of the surface.

Zone I

The zone correlates well with a magnetic trend. The strongest response

occurs near IN on Line 68W and suggests a narrow source at a depth of about 50 1 .


Theoretical Induced Polarization and Resistivity Studies

Scale Model Cases

01 23 S S 6 7 B 9 10 II 12 13 IN IS 16 17 IB 19

i-1 .

i-l.

LI.

140 111 lit l U

O l 23 t S 6 7 8 9 10 11 12 13 It IS IS 17 IB 19

i.*.

O -0.1 .0.7,

(fe)o

O l 23 t S 6 7 8 9 10 II 12 13 W IS 16 11 18 13

1.1 o

(Mf

CUCTHOOC

(Mf)a

01 23 t S 6 7 S 9 10 11 12 13 IN IS 16 l? 18 19

^/)/27^} 2 = 5

(Mf) 2 = 7000

(fe)

\ 7\ X\ '

VIIW Or AMOMttOUS Z ON l

*NO lUHVlT (.IKt

-*XOM*L(XlJ 1ONC

t r-4) l)

CASE 1ZI-0-25-DX-250-0

- 8 -

The anomalies to the east are considerably weaker; the resistivity pattern

near 7N on Line 5?.W ie typical of a large, flat-lying conductive sheet (compare

with Model Case VH-0. 0-EU-?.50-a).

Zone J

This zone is weak, and variable in width. It appears to lie parallel and

to the north of two magnetic features. On all lines the source appears* to be

within 100' of the surface.

Zone K

The anomalies are extremely weak, bat the rone correlates with a

magnetic feature and may indicate a nhallow source much narrower than the

ZOO 1 electrode interval (see Appendix).

Zone L

The zone is again weak and poorly defined. There is no direct magnetic

correlation. The zone may indicate a narrow, shallow source.

Zone Jvi

The anomalies are very weak on Line l 04W and Line 108W. They could

be caused by the amount of magnetite required to produce the prominent

magnetic feature near the base line. The high frequency effect value measured

near IS with 200' electrode intervals apparently arose when both the transmitting

dipole and receiving dipole were straddling magnetic dykea. Detailing with 100'

electrode interval* confirmed the freouency effects but failed to reveal any

prominent Metal Factor anomaly.



Scale Model Cases

O t 23 4 S 6 t 9 10 H 12 13 H 15 16 IT 18 19

147

(P/2^r)a

O l 21 H S 6 7 R 9 10 11 12 13 It IS 16 H 18 IS

-o.l

0,1

(fe)o

O l 23 S 5 6 7 t 9 10 II 12 13 11 IS 16 17 IS 13

O.I

(Mf)o

01 2 3 t S E 7 t 3 1 0 II 12 l) 11 li 16 17 18 19

{/V27T)| " 250 {^2^)2=2-5

(Mf ) , * 0

tucmooc cox'iouoMiox

(Mf) 2 * 1 0800

l l C J O " 2 i /o

\ x\ x\ /

PUN vi(* orANOUALOUi ZOIC t HO

lUXVf* 1 1*1

MIT* -lluki'TI

lOTn -HUU'll'

IH" -l|u*iljj

CASE3m-0-0-BU-250-o

9 -

Zone N

The zone is long, and relatively distinct. The strongest response

occurs near 9S on Line l 08W and suggests a source within 100' of the surface.

There is no direct magnetic correlation with the zone.

Zone O

This zone includes the strongest response measured on the property.

The definite anomaly near P5+50S indicates a metallic -conducting source at a

depth less than SO 1 . Relatively strong anomalies on Line 88\v , Line 96VV, and

Lire 11ZW indicate a similar, narrow, shallow source.

There is no magnetic correlation with the zone; however, it is still one

of the most interesting anomalous features on the grid.

Zone P

This cone is short, weak and without magnetic correlation. Nevertheless,

the probable anomaly near 33S indicates what could be * shallow source much

narrower than the 200' electrode interval.

Zone Q

The zone is very weak. The anomalies could be explained by the amount

of magnetite required to produce the associated magnetic response.

Zone R

The strongest section c* the zone coincides with a magnetic anomaly.

Detailing both Line 104W and Line 96W with l OO 1 electrode intervals has

indicated a narrow source within 50' of the surface. The pronounced fre

quency effect high between 46S and 4 BS on Line l 04V/ suggeste the presence of

metallic-conducting mineralization.

- 10 -

Z.one S

The zone is very weak except on Line 132'A, where it suggests a

source within 50' of the surface near 33+50S.

There is no correlating magnetic response.

Zone T

The responue is very weak. The anomalies may indicate a shallow

source much narrower than the electrode interval, as discu&ted in the Appendix.

Again, there appeare to be no magnetic association.

4. SUMMARY AND RE. C O M M E N b A T I O N l-

Mo8t of the anomalies revealed on the grid are extremely weak, .sot one-

of the anomalous zones approaches the magnitude of the response over other

economic deposits in the Immediate area or over other typical, large massive

sulphide ore bodies in volcanic rocks in the Canadian i/hield.

However, there are two rones (Zone O and Zone R) which include definite

anomalies, and which may indicate significant mineralization in narrow widths.

If the EOneb are to be tested, the following inclined drill holes are suggested:

DDH l, passing beneath 25*50t: on line lOOVV at a depth of 100".

E'DH 2 , inclined to north (the deposit appears to dip south) and passing beneath 46+50S on Line l 08Vv at a depth of 100'.

In addition to the above, there are two weak zones (Zone C am! Zone D)

which lie in a particularly interesting geological environment, on strike with

acid volcanic outcrop. The zones, may indicate narrow widths of poorly-

conducting (perhaps high sphalerite - low pyrite) mineralization. The zones

could be tested by the following drill holey;

- n -

DDH 3, passing beneath 23N on Line 68V; at a depth of l 50'. (There is a flight indication that the source dips tc the north).

DDH 4, pa B e ing beneath l 8N on Line 76\V at a depth of 100'. (The source appears to dip to the south).

All the other weak anomalies are considered of little eignlficance as

direct indication* of economic-sized deposits of massive sulphide mineralization.

The anomalies were correlated into zones mainly to act as an aid in establishing

mineralized trends which could perhaps lead to the discovery of depoeito below

the effective depth of penetration for the eurvey (about ?00' or 300 1 for small

deposits).

Jv.cPHAil GEOPHYSICS LIMITED

William H. telton, Geophyeic'.st.

Robert A. Bell, Ceologist.

Dated: May 17,1971

- 12 -

ASSESSMENT DETAILS

PROPERTY i Canadore Option

SPONSOR: Mewconex Canadian ExplorationLtd.

LOCATION: Sturgeon Lake Area

TYPE OF SURVEY: Induced Polarization

OPERATING MAN DAYSi

CONSULTING MAN DAYSi

DRAUGHTING MAN DAYS t

TOTAL MAN DAYSi

183

EQUIVALENT 8 HR. MAN DAYSi 274.

5

H

290, S

MINING DIVISION* Patricia

PROVINCE: Ontario

DATE STARTEDl January 15, 1971

DATE FINISHED: April 4,1971

NUMBER OF STATIONS! 972

NUMBER OF READINGS? 8228

MILES OF LINE SURVEYEDi 32.3

CONSULTANTS:

William H. Pelton, Apt. 2212, 650 Parliament Street, Toronto, Ontario. Robert A. Boll, 50 Hemford Crescent, Don Mills, Ontario.

FIELD TECHNICIANS:

J. Garland, 86 Augusta Street, Port Hope, Ontario.S. Jarvie, 863 Masson Street, Oshawa, Ontario.M. McDonald, 6135 Pow Crescent, N.W, Calgary, Alberta.Plus Extra Labour i -Paul Banville, 145 Bread* Crescent, Scarborough, Ontario.Lewis Straubert, P.O. Box 21 3, Thunder Bay, Ontario.Russell Browning, 52 CornwalHs Drive, Scarborough, Ontario.

DRAUGHTSMEN:

B. Marr, 1 9 Konewen Court, Toronto 16, Ontario. K, Klngebury, 58 Oak Avenue, Rlchvale, Ontario. ^ Hurst, 230 Woburn Avenue, Toronto 12, Ontario.

\^ MAY l 2 197,9 '~

^i^oh^ -W McPHAR GEOPHYSICS LIMITED ': -

WlUiam H. Pelton, GeophyaicUt,

- 13 -

STATEMENT OF COST

Newconex Canadian Exploration Ltd. - IP Survey Canadore Option, Sturgeon I.Akc Area, Ontario.

Crew; J. Garland, 5. Jnrvle - January l 5th - March l Hh, 1971 M. McDonald, S. Jarvle -Mnrch 12th - April 4th, 1971

l

20 day* 25-3/4 days

31 days 4\ days 5 days 31 days

61 days ?. days 8-3/4 days

Operating OperatingTravel ) Preparation )16|dayn Standby ) Bad Weather )

PreparationStandbyBreakdown

Crew ExpensesAir FareVehicle ExpenseFreight and BrokerageBus FareTaxisMeals and AccommodationRented AircraftTelephone and TelegraphCamp SuppliesExcess Baggage

Plue J07o

r $ 265.00/day f- $ ?.BO.OO/d^y

f1 -tJOO.OO/day

J79.001.Z92.70

189.797.65

118.801.957.47,

463.5822.60

581.5115.00

4,828.05

482.805,310.85

$ 5,300.00 6,437.50

J,650.00

N.C.

$13,387.50

5,310.85

Extra Labour Plus P-0%

3,113.00622.60

3,735.60 3.735.60 $22,433.95

Datedt May 17,1971

McPHAR GEOPHYSICS UMITEJ)

William H. Polton, Gcophyelclat.

McPHAR GEOPHYSICS

APPENDIX

THE INTERPRETATION OF

INDUCED POLARIZATION ANOMALIES

FROM RELATIVELY SMALL SOURCES

The induced polarization method was originally developed to detect disseminated sxilphides and has proven to be very successful in the eearch for "porphyry copper" deposits. In recent years we have found that the IP method can also be very useful in exploring for more con centrated deposits of limited size. This type of source gives sharp IP anomalies that are often difficult to interpret.

The anomalous patterns that develop on the contoured data plots will depend on the size, depth and position of the source and the relative size of the electrode interval The data plots are not sections showing the electrical parameters of the ground. When the electrode interval (X) is appreciably greater than the width of the source, a large volume of unmineralized rock is averaged into each measurement. This is particularly true for the large values of the electrode separation (n).

The theoretical scale model results shown in Figure l and Figure Z indicate the effect of depth. If the depth to the top of the source is small compared to the electrode interval (i. e. d X) the measure ment for n s l will be anomalous. In Figure l the depth is 0. 5 units (X s 1.0 units) and the n ;; l value is definitely anomalous; the pattern on the contoured data plot is typical for a relatively shallow, narrow, near-vertical tabular source. The results in Figure 2 are for the same source with the depth increased to 1. 5 units. Here the n = l value is not anomalous; the larger values of (n) are anomalous but the magnitudes are much lower than for the source at less depth.

When the electrode interval is greater than the width of the source, it is not possible to determine its width or exact position between the electrodes. The true IP effect within the source is also indeterminate; the anomaly from a very narrow source with a very large true IP effect will be much the same as that from a zone with twice the width and 1 /2 the true IP effect. The theoretical scale model data shown in Figure 3 and Figure 4 demonstrate this problem. The depth and position of the source are unchanged but the width and true IP effect are varied. The anomalous patterns and magnitudes are essentially the same, hence the data are insufficient to evaluate the source completely.

The normal practise is to indicate the IP anomalies by solid, broken, or dashed bars, depending upon their degree of distinctiveness. These bars represent the surface projection of the anomalous zones as interpreted from the location of the transmitter and receiver electrodes

- z -

when the anomalous values were measured. As illustrated in Figure l, Figure 2, Figure 3 and Figure 4, no anomaly can be located with more accuracy than the spread length. While the centre of the solid bar indicating the anomaly corresponds fairly well with the source, tbe length of the bar should not be taken to represent the exact edges of the anomalous material.

If the source is shallow, the anomaly can be better evaluated using a shorter electrode interval. When the electrode interval used approaches the width of the source, the apparent effects measured will be nearly equal to the true effects within the source. When there is some depth to the top of the source, it is not possible to use electrode intervals that are much less than the depth to the source. In this situation, one must realize that a definite ambiguity exists regarding the width of the source and the IP effect within the source.

Our experience has confirmed the desirability of doing detail. When a reconnaissance IP survey using a relatively large electrode ir- terval indicates the presence of a narrow, shallow source, detail with shorter electrode intervals is necessary in order to better locate, and evaluate, the source. The data of most usefulness is obtained when the maximum apparent IP effect is measured for n ~ Z o r n - 3 . For in stance, an anomaly originally located using X = 300' may be checked with X = ZOO 1 and then X - 100'. The data with X -- 100' will be quite different from the original reconnaissance results with X s 300'.

The data shown in Figure 5 and Figure 6 are field results from a greenstone area in Quebec. The expected sources were narrow (less than 30' in width) zones of massive, high-grade, s-.hic-silver ore. An electrode interval of 200' was used for the reconnaissance survey in order to keep the rate of progress at an acceptable level. The anomalies located were low in magnitude.

The very weak, shallow anomaly shown in Figure 5 is typical of those located by the X = 2 00' reconnaissance survey. Several anomalies .of this type were detailed using shorter electrode intervals. In most cases the detail measurements suggested broad zones of very weak mineralization. However, in the case of the source at 20N lo 22N, the measurements with shorter electrode intervals confirmed the presence of a strong, narrow source. The X - 5 0' results are shown in Figure 6. Subsequent drilling has shown the source to be 12. 5' of massive sulphide mineralization con taining significant zinc and silver values.

The change in the anomaly that results when the electrode in terval is reduced is not unusual. The X ^ 50' data more accurately locates the narrow source, and permits the geophysicist to make a better evaluation of its importance. The completion of this type of detail is very important, in order to get the maximum usefulness from a reconnaissance IP survey.



Scale Model Cases

t t J ) * ) l J l 1 M H l] l) H II H IT M

44 **

l * 1.1 I.I V rt tt H

l i l * t l 1 "f 11 IJ U W IS * IT 11 t)

(fi)o

t l l ) l l i J t 1 l* li II 11 K II 14 P 11 11

(Ml)fl

' l II tit l l t K n ii li n u M li

(Mf) - O (Mf) 2* 0000

(ft)

I\ s

,/

CASE tt-OS-BU-tO-a

McPHAR GEOPHYSICS LIMITEDTheoretical Induced Polarization and Resistivity Studies

Scale Model Cases

i* t t S t ' II t t II II

,t .. S . . t i .1 * t i .

i i i i

t 11 i * ii t i

lil l t i * * l l l i

* * It 4 l x ' ,- 'x'"T^^^xss* t -l . l l

. i 11 i r /fct 111 1 1\ ^y\' * * * '

(ft)o

41 (14 tl *

(U()o

t i l l l I l ) 1C It 11 J] it li l* 11

(MO - O (Ml) 2 ' 9250

(( l ,

P

l

i

W

l

CASE

5 t. 13 14THEORETICAL

INDUCED POLARIZATION n.,. M..... lo I0 (y97 e e ,0 ,0AND n -3 ---.-.(O 10 IO/ 95 8 7 87 95\v!C 1 0 IO

r,. J - —-- 10 10 1 0 f 9 3 88 B9 88 9 3 \tO 1 0 10

RESISTIVITY STUDIES n n --io \o \o /90 se 90 90 SB 9?\ iO ID iO

SCALE MODEL CASE

PLAN VIEW

^______t______10

ni -i-, i -f

A /- s

X EQUALS 1UNIT

}6

7 H 9 Ip M 12 13 14 IS 16

(F*)o02 -02

o o06 O 02

\\-06 -03 O

0.3 ...--o O -06/ 01W40

n J - O O -05/0^47 43

n-4 O -03 -06/^1-^35 42 4

_7___B 9 '.Q l i l? 13 14 l?

n l 17 O -49 W W/ 4 10

//yn.j--......-.. Q 0 ..,9 74^^460

n-3-0 O -59 jjyQJ*) *K

r. 4--o -JO -59 Xi4l/^Ja2 467 467

i 6 7 fl 9 tO II 12 13 14

10

(Mf), ' O ( Mf ) 2 -11700 i

(Fe)2 - SO'/, l

1'l H E I UN' Of S OIIBCI

4 UNITS

f IG 3

THEORETICAL

NDUCED POLARIZATIONAND

6 7

n-i- -- --10 10 10 y" ftV 9 J 99 \IO 10 10

n -? - K) 10 10/^97 91 91 97\^IO 10 !0

n . J 10 10 (O y' 9 7 92 92 92 9 7\. 10 10 10

RESISTIVITY STUDIES n 4 10 10 PO /se 9 j 95 93 93 96 \ 10 10 \o

SCALE MODEL CASE

PLAN VIEW

*___o

M /- \

X EQUALS l UNIT

J____6____7___8 9 ,p i, i? i j (j) 15 16

n -l -.—- o O -03

n 7 ... - . . o O -OB

n.J- -O O -08 05,

n - A - O O -O7 O8

j 6 7 B 9 10 ij 12 1.3 14

56 78 9 K) n 12 li 14

P2x\ ' IO

{Mf), ' OMPtM tfTCNF O' SOU*CC

4 UNITS

FIG 4

••J

INDUCED POLARIZATION AND RESISTIVITY RESULTS

8ATCHELOR LAKE AREA,, QUEBEC.

1*00X/ 4500 x" 12200 M WOO

IMO// 4040 l SI70 WOO// 11700 X IJ20 VI ttOOOO 1700

)720Y\ IZOOO uon.-fi•t— I SOO X X 4*00 J960 ^ X 7*00 l / /Z030

ION I2N UN I6N I8N SON 22N 24N 26N 28N

•l — O-IJ 0-2* 0-M O 0*9 M l T'S/ 0 1 O 01

i-l———087 019 frit 02 01* 07* O 01

i-J————————0-J* O l O J2 02* 0-J* 012 O

(MF),

ION I2N I4N I6N I8N 20N 2 2 H 2 4N 26N 28N

ION I2N I4N I6N I8N 20N 22N 24N 26N 28N

MASSIVE SULPHIDE

ZONC

FIG 5


BATCHELOR LAKE AREA, QUEBEC.

I9N 20 N 21 N 22N 23N

19 N 20 N 2IN

21 0-1 O )t

22N

(MF!,

O 21

23N

024 O t

2-* S 4 -* 4* S* 2 -*

I9N 20N 2IN 22N 23N

GLACIAL OVERBURDEN

MASSIVE SULPHIDE ZONE —

GREENSTONE

Flo. 6

52G1SSW0026 52G15SW0037 BELL LAKE020

RECEIVED

OCT i 5 I97IPROJtCTG SFCTION

REPORT ON

GEOLOGICAL SURVEY

CANADORE AKI) AL1X CLAIHS

UKE

STURGEON L/XE AREA

ONTARIO

i

INTRODUCTION

Options were taken on the 75 claim Mix group

and the 21 claim Canadore group in November 1969, because

of their favourable location with respect to the Mattabi

base metal discovery in Block Seven near Sturgeon Lake. ;

Lines were cut on the property in January 1970 and hori

zontal loop electromagnetic and fluxgate magnetometer were l

completed in late February. The surveys disclosed severn! j

anomalous systems on the Alix group, but the Canadore claims {

showed no conductivity. When drilled,the conductors on the j

Alix group proved to be pyrrhotite and some graphite with

only minor amounts of copper and zinc, ;\

Discovery of base metols o/' the New Brunswick ;

Uranium property to the west of our Canadore group renewed

our interest in the ground and io th6 winter of

induced polarization survey was run on Lhe 21 claim Canadore

group and about J^ a -J join ing Alix claims. Only very weak

induced polarization response was encountered^ and none of

tlie indications warranted drilling. In order to be assured

that no area of interest: might have gone undetected the

claims covered by t\\Q I -j** curvcy were mapped geologically

in June and July of this yoflr. This report is concerned

with the results of thxs mapping.

CLAIMS

A total of 34 claims were covered by the geolo

gical mapping. They are:

PA205910 - 205914 inclusivePA205918 - 205927 inclusivePA227153 - 227159 inclusivePA227205 -PA227206 -PA227208 -PA227209 -PA225025 -PA225027 - 225029 inclusivePA227180 - 227183 inclusive

LOCATION AND ACCESS

The claims in question are near Claw and Telephone

lakes some 7 miles east of the Mattabi Mine near Sturgeon

Lake. The Canadore group lies south of Claw Lake and west

of Telephone Lake and the Alix group is east of Telephone

Lake. The claims can be reached by aircraft from Sioux

Lookout or Ignace or on foot on a bush road from the end

of the truck road to Lyon Lake.

WORK ACCOMPLISHED

The object of the geological mapping was to deter

mine if any extensive areas of felsic rock remained undetect

ed on the property. Although basic control for the survey

was the geophysical grid lines which are 400 feet apart, ex

tensive outcrop prospecting and stripping was carried out

3/

between the lines. Particular emphasis was placed on areas

where I.P. responses were reported even though these were

weak.

RESULTS OF THE SURVEY

A map entitled "Geological Plan, Canadore Option"

drawn to a ^cale of one inch equals 400 feet accompanies

this report.

The following sequence of rocks was encountered on

the property:

1. Massive metavolcanics

2. Gneisses: quartz, chlorite, sericite,

hornblende

3. Felsic rocks: rhyodacite and felsic

porphyry

4. Tuff: basic to intermediate

Most of the claim group is underlain by highly

altered massive to schistose chloritic volcanic rocks of

intermediate composition. Attempts to differentiate between

the gneissic and massive units were not successful possibly

because the changes are gradational or owing to scarcity of

outcrop. The massive metavolcanics are dark green to black

in colour and consists of feldspar and hornblende and have

metamorphic textures. The gneisses and schists have similar

colouration but consist primarily of chlorite and hornblende

modified by feldspar, quartz and sericite.

The tuffaceous rocks range in composition from

basic to intermediate, and consist of quartz and feldspathic

fragments in a generally basic ground mass. Most of the

tuff outcrops exhibit shearing. This classification includes

some narrow agglomerate bands.

The felsic rocks were purposely classified as fel

site and rhyodacite to call attention to the more acid member.

These rocks are siliceous to cherty, light coloured, massive

to slightly sheared and consist of quartz, feldspar and some

sericite. Other than the outcrops already reported on the

shore of Claw Lake only one outcrop of felsic rock was located

on the claims,, This outcrop of rhyodacite composition occurs

at 800'N, 8250'W and is probably associated with the felsic

outcrops on the shore, but heavy overburden to the west of

the outcrop obscures the relationship.

As no contacts were observed on the claims the

true strike is not known. However lineation, schistosity

and gneissosity strike about N70"W which is the regional

strike. The dip is steeply south in most cases. The presence

of a possible fold in the felsic rocks shown on Map P.670

(west part) published this year by the. Ontario Department

of Mines was not confirmed by our work.

5/

With the exception of one location (100*N, 6800'W)

little was found to explain the weak I,P. response. In the

above location some narrow shears with thin seams of pyrite

were found in gneissic rocks.

CONCLUSIONS

Careful mapping and outcrop prospecting has shown

that felsic rocks are restricted to the northcentral part of

the group around Claw Lake. Although the outcrops examined

are similar to the felsic host rocks at the New Brunswick

Uranium property and Mattabi they have failed to respond to

electromagnetic or induced polarization surveys and can be

considered to be barren of sulphide concentration within the

range of detectability of these instruments. As presently

known the felsic assemblage on the claims is too smnll to

warrant exploration at depths greater than instrument pene

tration.

The balance of the claim group is underlain by

massive metavolcanics and gneisses of basic to intermediate

composition. Electromagnetic measurements of these rocks

were completely negative and induced polarization response

was weak and local indicating that sulphide mineralization

is present only in very small concentrations. ,-" : .

Toronto, Ontario - j . '; 't.,,..... ..,. "SSeptember 30, 1971 R. A. KntifspnA. r : ;;;,- ;

ASSESSMENT DETAILS

Property: Canodoro Option

Mining piv is Ion ; Patricia

RcRistered Holder; Nwconcx Onndion linploration Ltd.

Loco.tlon: Claw Lake iron, Sturgeon Lake, Ontnrlo

oi;. .Survey; Goolo&icnl

Operating Mondays;

I. Percival - 36 - Juno 17 - July 31, 1971

E. Ferris - 22 - Juno 17 - July 16, 1971

W. McDonogh - 21 - July 6 - July 31, 19/1

R. A. Knutoon - 10 - June 24 - July 6, 1971

ConflulUinK Mm U.-sys; 3 - Septcunl^oi; 27 - 30 1971

Ur*ughtinR Msndnya; g^JJ - !;p.pteinbor 21 - 30 1971

Total Itendaya ; 100t

HllcB of line Surveyed; - 30.0

Consul tanto; R. A. Knutaon - 33 Cftehead Rd., Willcn^dwle

Tcchuici/irio;

lain Percival ~ Bundrowes, Bfllblatr, Conon Bridge,Roas-ahire, Scotland

B. G. F*rria - tfox 791, Val d 'Or, Quobec

W. J. McDonagh - 70 Letitio Straat, Birrio, One.

DrauRhtlng; W. J. HcDonajjh

- 8 -

indicated for the corresponding value of Apparent Metal Factor. In

contouring negative values the contour lines are indicated to the nearest

positive value in the immediate vicinity of the negative value.

The symbol "NR" indicates that for some reason the operator

did not attempt to record a reading although normal survey procedures

would suggest that one was required. This may be due to inaccessible

topography or other similar reasons. Any symbol other than those dis

cussed above is, unique to a particular situation and is described within

the body of the report.

METHOD USED IN PLOTTING DIPOLE-DIPOLE


Stotions on line Electrode spreod length Electrode seporotlon

n

n

n

n

4

3

2

l

n - l

n - 2

n - 3

n - 4

_ P P P1,2-6,7 2,3-7,8 3,4-8,9

P P P P1,2-5,6 2,3-6,7 3,4-7,8 4,5-6,9 Apporent Resistivity

p p p p p1,2-4,5 2,3-5,6 3,4-6,7 4,5-7,8 5,6-8,9

P P P P P P1.2-3.4 2,3-4,5 3,4-5,6 4,5-6,7 5,6-7,8 6.7-8.9

MF M f. M .F. M.r M.F. M F 1,2-3,4 2,3-4,5 3,4-5,6 4,5-6,7 5,6-7,8 6,7-8,9 MF. M.F. M.F. M.F. M.F.

" 1,2-4.5 2,3-5.6 3.4-6,7 4,5-7,8 5,6-8,9_______ M.F. MF M.F. M.F

1,2-5,6 2.3-6.7 3,4-7,8 4.5-8,9 Apporent Metol Foctor__________ M.F. M.F. M.F.

1,2-6,7 2,3-7,8 3,4-8.9

n - l

n - 2

n - 3

n - 4

F.E. F. L F.E. f.t. F. E." F.t. 1,2-3,4 2,3-4,5 3,4-5,6 4.5-6,7 5.6-7,8 6,7-8,9

, F.E. F,E. F.L F.E. F.E.1,2-4,5 2,3-5.6 3.4-6,7 4,5-7,8 5,6-8,9

_______ F.E. FE. F.E. F.E.1,2-5,6 2,3-6.7 3.4-7,8 4,5-8,9 Apporent Percent

______ F.E. F.E, F.E. Frequency Effect1,2-6,7 2,3-7.8 3,4-8,9

Fig. A

J i2- Ji*-

----f

V

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i S i

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4---i--i

iii'

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^*

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SPECIAL PROVISION

ASSESSMENT WORK DETAILS

OCT * * ' Tl1

SECTION

Type *fs..rvyA •rporot* form l* required (or each type ol iurv*y

Chief Line Cutter or Contractor-Nam* Addmi

Party r^j^f Jain Percival, Bundrower. Ralbl.oir, Conon Kridftc, Ross-shiro, Scot landName Addrenn

rnn ...i. n niR. A. Knutson._____33 Gal e he a d Rond.____Wll.lowd.ilc, On t: .ir j o____

COVERING DATES Line Cutting .Natno

Field Geology or r..nrk y .ir.JuilG 17 - July 31. 1971

Office September 21 - 30, 1971_________

INSTRUMENT DATA Moke, Model and Type

Scale Constant or Sensitivity - ————————————————————— Or p rovide cofy o/ instrument data from Manufacturer's brochure.

Total Number of Stations Within Clnim Group

ASSESSMENT WORK CREDITS REQUESTED

MINING CLAIMS TRAVERSED

PA - 205910 - 205914- inclusive

——Number of Miles of Line cut Within Cloim

' r7o) ^Geological SurveyV^— f—Days per Clai

Geophysical Survey———^— Days per Clt*m

30.0

PA - 20591B - 205927- inclusive

PA - 227153 - 227159

PA - 227205. 227206, 227208, 227209

PA - 225025, 225027, 225028, 225029

PA - 227180,- 227183 inclusive

DATE Octpber 5 , 1971

TOTAL 3A claims

SIGNED

Special provision credits do not apply to flodiomelric Surveys.

Type of Survey

SPECIAL PROVISION

ASSESSMENT WOUK DETAILS

Induced Polarization

OHT

Chief Line Cutter or

Party Chief

_________________________ ^A ••parole form Is r*qulr*d lor *och type ot *unr*y

McPh.ir Gcophyics, 139 Bond Avenue, Don Mills, Ontario.Nome Addrrn*

J. Garland 86 Augusta St. Pt. Hope, Ontario

Consultant William ?c 11 onHam*

Apt:. 2212Aridrem

650 Parliament St. TorontoM dm* Addr***

COVERING DATES Line Cutting

Field Geology or Geophysics January l r) - April 14, 1971

Office April 3 - 20th. 1971——————————————

INSTRUMENT DATA Make, Model and Type McPhnr Induced Polarization Unit

ScDle Constant or Sensitivity SCO reportOf p rovide copy of instrument data from Manufacturer1 s brochure.

Total Number of Stations Within Claim Group 972 -Number of Miles of Line cut Within Claim Group—-' '

ASSESSMENT WORK CREDITS REQUESTED Geological Survey Per

MINING CLAIMS TRAVERSED

Geophysical Survey.^-^iLy Days per CJO ^ r f *^~ \

Pn, ?O5c ll l

m

DATE

TOTAL

SIGNED

Special provision credits do not apply to Ho Isometric Surveys.

ASSESSMENT WORK BREAKDOWN

1. Type of Survey . Anduc.etJ.Pp.l*iri;j,a.tion

2. Township or Area Jtek1..a.nd..S.hikpji Lakes JSouth of .Sturgepn.LakeJ) .

3. Numbers of Mining Claims Traversed by Survey . 2/^91,0, .tO.lA..lnc.l,U8 ly.e. t ........ ....

.2 05918 . to .2 7. In c l us.lv e,. 2 2 5 O 2,5. t *2 2.5.0 2 .7. .to . 29. .in c l .us lv e^. .2 2.7.1 5.3 . t p. .5 9. . . . .

-^"pAH? *y.eJL . ? 2.7.1 80 .tO .83 .incl.usly e^ .227205 :p6 , 22 7208-09. .

Surveyed k. N umber of Miles of LineX&X ..........?2,'.3 ......., F lown ....NIL . . ., , , , . .

Q79*5. Number of Stations Established ------.-...----...Ir....................................

*6. Make and type of Instrument Used ..H0.?!??/..?:?.'..^^..................... .............

*7. Scale Constant or Sensitivity .........................................................

*8. Frequency Used and Power Output .... ...................................................

9. Summary of Assessment Credits (details on reverse side)

Total 8 hour Technical Days (Include Consultants, Draughting etc.) .."/..if ...........

Total 8 hour Line-Cutting Days

Calculation

290.5 x 7 - 2033.5 * - . 2033.5 ^.34 B 59.8-~i i i , . 1,^ .i-^~^ ' i .ii-ii MI . i, , - _ f ^m^ -i- - ____ L - ,-n ' lin r , ..~ T- --- . i - I-^^--IM-

Technical Line-cutting Number Assessment creditsof claims per claim

The dates listed on this form represent working time spent entirely within the limitsof the above listed claims (x~l CheckIf otherwise, please explain .....................................................,. ....

/' / /-M /^ l — Dated; ..M.IX.5^ A??.2........ .... ... Signed; ^/.^..^f.{.^j^.^.. .

Note: (A) * Cor,j-iete only if applicable. ., .(B) Complete list of names, addresses and dates on reverse,rs,idd(C) Submit separate breakdown for each type of survey, v' , f -.(D) Submit in duplicate. .-/'

ASSESSMENT WORK BREAKDOWN

1. FIELD WORK

Type- of Work Name A Address Dates Workedof

8 hour days

.15-Mar. 11 ^ ...3?;?.

.-,..---..---------.-..-..-.......-.....-.9?^?.?nA:M^M.McDonald 6135 Bow Crescent, N.W.Calgary Jan.l5-Apr.4 54.9

145 Uremia Cres., Scarborough Jan.l5-Apr.4 54.9

P.O. Box 215, Thunder Bay, Jan.l5-Apr.4 54.9•••WB**BHBVKVVVKBBHVBOMVWB.BIBV**(BIKBBB*1BBK*MM*H*B**V*VB*V BM •••••••••HB.VBH H B* MVKVVAM^VK ••••BBBK

RuBSellBrownlng 52 Cornwallls Drive, Scarborough Jan.J5-Apr.4 54.9

2. CONSULTANTS

Number of Name S Address Dates Worked (specify in field or office) 8 hour days

.Rilli-?H.??itp.n....Aj21^. 2J212j --6-50- i-.a.rliarnen^ S,t. t Tor., Apr.. 6jMajj. 1.7. r... 3.

-RfiJi??.P..A:.?All. ^0 Hemford Crescent^, Don Mills Apr.6-Maj^ 17

3. DRAUGHTSMAN, TYPING, OTHERS (specify)

Number of Name 61 Address Type of Work Dates Worked 8 hour days

Kenewen Court^ Toronto Apr. 6 - May 17 4

5B..Oak Avenue^.Rlc.hvale^.Onta.rio...A^r....6..7.MAX-J-7. ...y.

.F....ljyr-s^t 1---2-30 - WpJ3yrn- Aver,ue t Toronto^.\2j_0nt.^ Ajjr. 6 - Maj^ 1.7. ....3,

TOTAL 8 HOUR TECHNICAL DAYS 2 90.5

A. LINE-CUTTING

Number of Name Address Dates Worked 8 hour davs

TOTAL 8 HOUR LINE-CUTTING DAYS

Pf'liJECMS SECTION

Recorder Holdei

Township or Area

MINISTRY OK NATURAL RESOURCES

REVISED. LE.CHNJCAL A55CSSMENT WORK .CME(,l 1 S

(Supersedes Notice, of Intent statement of May 2, 1972)

........ . . ...Newconex.Canadian.Explorst loo L imited

. . . . . .. .Bell.and.Shikag.Lakes.(S..ot.Stucgoon Lake)

Type of Survey and number of Assessment Days Credits per claim

GEOPHYSICAL

Electromagnetic ....... .. ...................days

Magnetometer ...............................days

Radiometric .... .......................days

Induced Polarization .........58..... .d.iys

GEOLOGICAL............. ............................days

GEOCHEMICAL............. ............ .............days

AirborneMan days

Special Provision!_j Ground

NOTICE OF INTENT TO BE ISSUtP

Credits have been reduced because of pallial coverage of claims.

Credits have been j educed because of corrections lo work dates and figures of applicant.

NO CREDITS have been allowed for the following mining claims as they were not sufficiently covered by the survey:

Mininy Claims

Pa. 205910 to 14 inclusive

205918 to 27

225025

225027 to 29 inclusive

227153 to 59

227180 to 83

227205 - 06

227208 - 09

Tht Mining ftccordfi mty iwiiice tlif above ctnfili if ntxemiy in order that the lutst number ol approved lueumetit rjjyi recorded on twh cl.nin rjon not etcrcil the rnmimum ailnwcd li lollvwt: Ccophyiictl - 80: Ctolotiictl - 40, Grochcmicfl - 40;

L v-.r

Schedule.. og.jBloltra, ,~

PA - 205910PA - 205911PA - 205912FA - 205913 'PA - 205914PA * 205918PA * 2G5919PA - 205920PA * 205921PA - 205922PA * 205923PA - 205924PA - 205925PA - 205926PA * 205927

PAPAPAPA

PAPAPAPA

- 225025- 220027- 225020- 22SC29

- 227205- 27.720*- 227203-- 227209

PA ~PA -PA -PA -PA *PA *-PA -

2271532^71.p.-'j2271552?.73..^62273.572':7iS3227159

PA " ?.27).GOPA - 227? 1HFA - 227'- '-J 2PA - 2?. 7' -v J

ONTARIO

Ministry of Natural Resources

RegisteredRoom W 1617 Parliament Buildings Toronto 182

May 10, 1972

Dear Sir:

Re: Geophysical (Induced Polarization) and Geological Surveys, Mining Claims Pa. 205910 et al, Bell and Shikag Lakes

____(S. of Sturgeon Lake), File 2.639

Further to my Notice of Intent dated May 2, 1972. I have re- examined the above Induced Polarization survey in regards to assessing this work under a "Man-days" basis.

Attached herewith is a revised statement which supersedes the previous list sent with my Notice of Intent and is approved as of the date above.

.'J 11*

O J/raw

encl.

416:965-6918 ,,,,,, : .

t i41

Mr. y . Buchan Mining Recorder Court House Sioux Lookout, Ontario

Yours very truly,

Fred W. MatthewsSupervisor

Projects Section

cc : Newconex Canadian Exploration Ltd, Toronto l, Ontario

cc: Mr. R. A, Knutson

cc: McPh-ir Geophysics

cc: Resident Geologist Kenora, Ontario

2:639

i *

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FREQUENCIESt Q.31-5.Q HZ

NOTEt CONTOURS flT LOGflRITHMIC INTERVflLS 1.-1.5-2.-3.-5.-7.5-10

DflTE SURVEYED! flPfl 1971

flPPROVED: *

DflTE (

•W;.

McPHRR GEOPHYSICSINDUCED POLflRIZflTION flND RESISTIVITY SURVEY

NOTEi THIS PLOT MRS PRODUCED WITH flN IBN 3SO/6S COMPUTEfl RND fl CftLCOHP PLOTTER

N - 5

N -

N - 3

N - 2

N -

3420 f 2250 2710 2580 . 3050 3850 , , . 1390 . 1800 . 2550 2989 v 3750 3810 1764 , , 3389 .2800 2870 , y 1090 v . 2710 . 1550

3400 X 2430 2860 2860 2100

1610 X, 2210 2707 2640 2660

1320 1740

1315

N - 5

N -

N - 3

N - 2

N -

RESISTIVITY (flpp.) IN OHM FEET f RESISTIVITY (flPP.J IN OHM FEET / 2*

16S 123 l OS , 83 6S 23 O 2N 6N . 8N ION 12N 14N 16N9 * * J* J J S

18N—i—

20N 22N 24N 26N 28N—t

lllllllllllllllllll

METflL FflCTOR (HPP.) METflL FflCTOR IflPPJ

N - l

N - 2

N - 3

N - 14

N - 5

2.9 2.3

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0.6

0.1 0.4 0.9 0.9

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1.0 X 0.7

0.4 0.6 0.3 0.8 0.6

0.6

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N - l

N - 2

N - 3

N - U

N - 5

16S 143 J2S IDS 83 6S 4S 2S 2N 6N . 8N ION 12N -- 14N . 16N ., 18N , '- 20N 24N 26N 28N

FREQUENCY EFFECT tflPP.) IN X FREQUENCY EFFECT (flPP.) IN X

N - l

N - 2

N - 3

N - 4

N - 5

4.7 5.1 2.2 v H.l 3.8 v 2.H

NEC

0.5

2.6 . l.B 1.6 1.5

1.2 \ . 1 .9

1.6 1.5

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3.1 3.6 , 2.6 2.7

2.3 2.3 S 1 .7 f- 1 .0

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N - 5

N - 4

N - 3

N - 2

N - 1-,

2105 2455 , 1715 1 835 , 1400 ^ v 2510 1600

2220 1125

2130

1250 1270

1260

RESISTIVITY (flPP.) IN OHM FEET /

1705

RESISTIVITY (flPPJ IN OHM FEET / 2*

N - 5

N - U

N - 3

N - 2

N - l

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N - 2

N - 3

N - 4

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N - l

N - 2

N - 3

N - li

N - 5

40S 38S 36S 34S. 323 303 288 26S 2U8 203 183 163 143

FREQUENCY EFFECT (flPP,) IN 7.

N - l

N - 2

N - 3

N - H

N - 5

i.o 0.8 0.6 0,6 0.7 0.1 0.3 O.U 0.3

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0.8 0.7

1.1

1.1

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0.9 0.8 i 1 .3 l 0.7 0.1 0.4 0.6 0.1 0.8

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N - 2

N - 3

N - 14

N - 5

DWG. NO.- I.P.- 5461- 14

NEWCONEX CRNflDIflN EXPLORflTION LTD.CflNflDORE OPTION, TELEPHONE LflKE

STURGEON LRKE RREfl

PRTRICIfl M.D., ONTRRIO

LINE NO.- . 72W (EXTENSION).

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\ s\ s\ s

PLOTTING \ s 'POINT —*-X X = 200*

SURFRCE PROJECTION OF RNOMflLOUS ZONES

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FREQUENCIES: 0.31-5.0 HZ

NOTE: CONTOURS RT LOGflRITHMIC INTERVflLS 1.-1.5-2.-3.-S.-7.5-10 DflTEi

McPHRR GEOPHYSICSINDUCED POLRRIZflTION RND RESISTIVITY SURVEY

NOTE* THIS PLOT MRS PRODUCED WITH RN IBM 360/65 COMPUTER RNO fl CflLCOMP PLOTTER

N - 5

N -

N - 3

N - 2

N -

7410 . , 2900

7279 6640 \ 3140

527U 5730

4290 6200 / 3700

N - 5

N - 4

N - 3

N - 2

N -

RESISTIVITY (flPPJ IN OHM FEET / 2 n

53 .. 43 33 . 23 IS 2N 3N

RESISTIVITY (fiPP.J IN OHM FEET / 2 n

5N 6N 7N 8N

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N -

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N - 3

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N - 2

N - 3

N - 4

N - 5

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DWG. NO.- I.P.- 5461-15

NEWCONEX CflNRDIAN EXPLORATION LTD.CRNADORE OPTION, TELEPHONE LflKE

STURGEON LRKE RREfl PRTRJCIfl M.D.. ONTRRIO

LINE NO.- 72W

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SURFflCE PROJECTION (OF flNOMflLOUS ZONES {(* ^AY j ^ , \

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FREQUENCIES: D.31-5.Q HZ

NOTEt CONTOURS flT LOGflRITHMIC INTERVflLS 1.-1.5-2.-3.-5.-7.5-10

DflTE SURVEYED t

RPPROVED:

DflTEt

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NOTEi THIS PLOT MRS PRODUCED WITH flN IBM 360/65 COMPUTER RND fl CflLCOMP PLOTTER

N - l

N - 2

N - 3

N - li

N - 5

DWG. NO.- I.P.- 5461-13

NEWCONEX CRNRDIRN EXPLORATION. LTD.CRNRDORE OPTION, TELEPHONE LRKE

STURGEON LRKE RREfl PRTRICIR M.D., ONTRRIO

LINE NO.- 72W

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S S .

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7V7-,

FREQUENCIES^ 0.31-5.0 H?

NOTEi CONTOURS RT LOGflRITHMIC INTERVflLS 1.-1.5-2.-3.-5.-7.5-10

DflTE SURVEYED: MflR 1971

DflTE:

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N -

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0.3

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N - 14

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METflL FflCTOR (flPPJ METflL FflCTOR (flPP.)

N - l

N - 2

N - 3

N - H

N - 5

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N - 2

N - 3

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FREQUENCY EFFECT (flPPJ IN X FREQUENCY EFFECT (flPPJ IN 7.

N - l

N - 2

N - 3

N - U

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N - 14

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RESISTIVITY tflPPJ IN OHM FEET / 2" RESISTIVITY (flPPJ IN OHM FEET /

323 30S 28S 26S , 245 . \ 22S . 20S . 18S 16S——L——

14S 12S l OS —l—

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23X X X S X S f

METflL FflCTOR (flPPJ METftL FftCTOR (flPPJ

N - l

N - 2

N - 3

N - U

N - 5

0.7

0.3

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NR NR 0.1 0.7 NR 0.2 0.3 0.3 0.3 NR 0.3 0,5

N -

N -

N -

N -

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FREQUENCY EFFECT (flPPJ IN 7. FREQUENCY EFFECT tflPPJ IN X

N - l

N - 2

N - 3

3.9 3.2

52G15SW3026 52G1SSW0037 BELL LAKE 350

3.0 3.1 . 2.7 , 3.5

3.6 f 2.2 l H.O X 2-8

4.0 S 6.S A V.V 4.1

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McPHRR GEOPHYSICSINDUCED POLflRIZflTION RND RESISTIVITY SURVEY

MOTE. THIS PLOT HRS PRODUCED WITH RN IBM 360/65 COMPUTE* WC fl Cd-CWr PLOTTER

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