31M8SSE8869 S . 2732 G ILLIES

JUL-61978

MINING LANDS SECTION

ST. JOSEPH EXPLORATIONS LIMITED

REPORT OF GROUND E.M. S MAGNETIC

SURVEYS

GILLIES LIMIT BLOCKS II S III

PROPERTY INCLUDING PART OF BRADLEY

SCHEAK OPTION

TOWNSHIP OF GILLIES LIMIT,

COBALT AREA, ONTARIO

A. W. BEECHAM

JUNE 12, 1978

N.T.S. 31-M-5

tINTRODUCTION i j

; l

The Gillies Limit Block 2 and 3 property consists of thre^

unpatented claims S-399090, S-399091 and S-399094 of approxi- ji

mately 40, 40 and .20 acres respectively. Also covered in thes^j

surveys was one of a group of four patented claims T-47923 optioned

from Messrs. H. M. Scheak and G . E . Bradley both of Toronto.

The unpatented claims were staked in May 1977 and the rec(j)rd-

ing date is May 24, 1977. The four adjoining patented were

optioned in October 1977. The claims were acquired to .cover a j

cluster of moderate to weak INPUT (airborne E.M.) anomalies.

An old grid of north - south picket lines was re-cut on

200 ft. spacing in September 1977.

LOCATIONS AND ACCESS

The property lines ^ mile west of the Cobalt - Hound Chutes -

Ragged Chutes gravel road, some 2^ miles south of the Town of

Cobalt. It i s most easily reached from this gravel road by travel

ling ^ mile west and then north on a bush track, which begins at

the old buildings of the Maki farm. The property straddles the

boundary between Blocks 2 and 3 of the Township of Gillies Limit*

TOPOGRAPHY

The topography is typical of the Cobalt area with about 1EJO

ft. of local relief and small scarps here and there. The valley

which marks the Cobalt Lake Fault through North Pickerel and South

Pickerel Lakes bends to the S-E. and passes the property.

ST. JOSEPH EXPLORATIONSBLOCKS 2 S3 , ond

GENERAL GEOLOGY

The area is underlain by conglomerates of the Gowganda

(or Coleman) Formation of the Huronian Cobalt Grou^. These

conglomerates fill an old north - south trending valley in

the underlying Archean. The Archean basement consists mainly

of mafic volcanics. A N.W. - S.E. trending band of 'interflow 1

sediments is believed to pass directly under the claims, coin

cident with the INPUT responses. Some 600 ft, east of the

property a drill hole (drilled by St, Joseph Explorations Ltd,

in 1976) intersected in excess of 200 ft. of graphitic argil- j

lite, with only minor sulphides and no significant metal values^

The graphitic horizon lies under some 500 ft. of Huronian sediments

at this point. According to drilling by Teck Corporation Ltd.,;

the Huronian rocks are over 300 ft. thick at L64E; 2+OOS and just

over 200 ft. thick at 48E; 4+OON.

PREVIOUS WORK ^ i

The area has been prospected as indicated by old trenches.j

However, trenching is not so extensive as in the main part of the

Cobalt camp. ;

In 1971-72 Teck Corporation covered the area by a soil geof

chemical survey for Ag and Co as part of a large area, which ;

extends westward to the Montreal River. Several apparent anomalies

were located and two drill holes were drilled to test these,

DESCRIPTION OF ELECTRO-MAGNETIC SURVEY

An Apex ParametricsMax-Min II horizontal loop system with ^

200 metre coil separation was used at 1777 Hz. Possibly anomalous

sections were also read at 444 Hz. The instrument specifications

are appended. The survey was run on 400 ft. spaced north - souih

lines approximately at right angles to the Archean basement rocks,

Readings were taken every 100 ft. Readings are not shown to

end of the lines because the plotting point is mid-way between

coils so that when one coil has reached the edge of the property,

the plotting point is still 100 metres (328 ft,) away,

DESCRIPTION OF MAGNETIC SURVEY j

A ground magnetic survey with a total field proton magneto

meter was run in December 1977 and March 1978. The earlier worfc

was done with a Barringer GM-122 magnetometer and a Scintrex MB^S-2

base station recorder. For this, the base station was located fet

the core shed on the Bailey property of Canadaka Mipes Ltd. (at

Glen Lake). The later work was done using a local base station!

on the base line at L56E. The two surveys were tied together by

overlapping areas. Technical data on the instruments are appended.

The results of the survey are displayed in Fig. 4. i!

RESULTS AND INTERPRETATION i |i i

The axis of a very subtle EM response, apparent in'both inf

phase and out-of-phase readings trends WNW-ESE and Cuts lines

L54E, L58E and L62E at about 3+50S; 6+OOS and 6+50S respective!^.

Although very subtle it dsconsistent enough across 8^)0 ft. to suggest

it is real and as there is no cultural interference it is assumed

to be a bedrock conductor. The shape of the profiles and the iiji-

phase to out-of-phase ratio suggests it is a fairly conductive jl

body at considerable depth. There is no coincident magnetic it

response. i

The magnetic background is about 59000 gammas and the magmatic

relief is low except in the southern part of the property. Thej

anomaly centred at L66E; 14+50S has a relief of 300 gammas abov4

background. It is relatively sharp and is likely a response from

a shallow source i.e. from the Huronian sediments or dyke and not - v

from the Archean basement. ! -

CONCLUSIONS AND RECOMMENDATIONS , \

The weak EM responses coincides well with the airborne EM

anomaly. As far as can be seen, they are on strike with thei

thick (more than 200 ft.) graphitic argillite band intersected j

600 ft. east of the property. This is almost certainly the causje

of INPUT anomaly. As the argillite bed contains only minor i'

sulphides and no base or precious metal values, there is little

encouragement to test the argillite band farther west*

Most sulphide occurrences in the basement rock^ in the

Cobalt area contain significant pyrrhotite. The lacjk of any

magnetic anomaly coincident with weak EM conductor, suggests

the conductor is caused mainly by graphite.

There are some favourable geological parameters, for silver

explorations: the presence of a deep pre-Huronian valley, the

presence of interflow sediments in basement rocks and the pos

sible .existance of the Cobalt Lake Fault through the small lake

near the west boundary. However, the lack of significant base

metal or silver values in the Archean interflow sediments in

dicates it should be given low priority for silver exploration.;

It is therefore recommended that no further work be done on

the property at present.

June 27, 1978

i-

A- W. Beecham,Senior GeologistSt. Joseph Explorations

VfKjCK."'': 1''",'' ' ", :?v .;/--^

MAXMIN I I EM SYSTEM

The Maxmin II is a two-man continuously portable EM

system. It is designed to measure both the vertical and horizontal

in-phase (IP) and quadrature (QP) components of thqt anomalous field ;

from electrically conductive zones. l

The plane of the transmitter (Tx) is kept; parallel tp the

mean slope between the transmitter and receiver (Rxj) at all tijnes.

The Maxmin II is a horizontal loop (HL) system wher} the receiver

measures anomalous components perpendicular to/the mean slope betweei. ) . . ' ' - . ' i , . ; ; . ' . _ :-

the coils. It is a minimum coupled (Min C) system When the receiver;

measures anomalous components parallel to the mean slope betweoni - ' -'Ir' ' -(

the coils. . i

APEX MAXMIN JI EM SYSTEM SPECIFICATIONS

OPERATING FREQUENCIES;

MODES OF OPERATION:

COIL SEPARATIONS: (modes a and b)

PARAMETERS MEASURED;

222, 444, 888,1 1777 and 35f5Hz*

a) Transmitter cpii plafre - andcoil plane horizontal (Max-coup; el* Hprizontal Ippp mpde). Used wit .ft reference

b)

c)

(Vertical loop mode). reference cable, in

25, 50, 100, 150,;200 or 100, 200, 300, 400, (MM li F). Coil separa not restricted to fixed

a) In-Phase and Quadratureof the secondary field 'in^ifipdes and b) . ".-'. . - - * ' /-'4,"-. '- , ,-;/:''. ; "" .' Y

b) Tilt-angle pf ttie tptal -field in mode c). .

Transmitter.. .^.^ ^—^T^ f^,rj ,^e|ijic?||,^|Mj|;

coupled mode) * 'Usedlw:cable."'. " J .. ;- -;-'--; /:'^

Transmitter cpiireceiver CPil planefor null in the receivej:'

l||

;.-v-. -lADOUTS:

SCALE RANGES:

READING REPEATABILITY:

TRANSMITTER DIPOLE MOMENT:

RECEIVER BATTERIES:

TRANSMITTER BATTERIES;

REFERENCE CABLE!

INDICATOR LIGHTS:

OPERATING TEMPERATURES:

WEIGHT OF RECEIVER UNIT:

WEIGHT OF TRANSMITTER UNIT:

VOICE LINK:

a) Automatic, direct readout on 90mm edgewise meters in modes a) and b), No nulling' or compensation necessary^

b) Tilt -angle and null on 90mm (3V1 ) edgewise mete'rs in mode o).

In-phase: - 2056 normal, i 10056 by switch^ Quadrature: 4- 2056 normal, fj 10056 by switch Tilt: * 7 556 slope 1 Null: Null sensitivity adjustable by

separation switch. .j. .j. . i - ij56 to - 56 normally, depending on condi tions, frequency an4 99H s 150 Atm2 @ 222; Hz, 150 Atm2

888Hz, 40 Atm2 1777hz

3555hz.

used,

9Q

30 Atm @

9V transistor radio type, 4 bat; Life: aprox. 35 hrs. continuous' (alkaline; .5Ah), less in cold"We^th^r.

a) 12V7.5Ah Gel -Cell rechargeable ;j (2 x 6V in series)

b) 18V21Ah alkaline lantern (3 x 6V in series] drain O. 5A to v2*2A ing frequency.

Light weight, minimum friction, reference cables Please specify. - ''-\' !^''\f^

Built-in intercom' system communication between; i mitter operators.

Built-in sign lights to indicate

-40 0C to 4- 60

6kg (13 Ibs.)

Typically 65kg (143 quantities of reference* included. Shipped in twp cases. ' - ; '.'. : . ',

Built-in intercom system ication between receiver operators. ; ': ;

'- ^Q^^^(^^^J^\--',

Jtllf'r'

, e'Y .., f ,*:*;K l!:: .--, ,':;iJ,-..;:v: ;'.MS '',:-. '^, :: , i v^!fW'-"'^"- ''--'~3W5'8

•' - '.iV^. --' , : f "~rj:.;:' : V," -. -:p-.r, ' . :. K, -- . - :-: .-;. i ' 1-.\: i);;?i;;'.--':". ; ' : "-' | .'''- ; -r;: ' " '

: ,, ; J. '. . l ;t"*'tj,". ..'i -V.' :' .".. '.jl'-ff'-.'^J

. - ; - " ; ' -' '.'-.i ;!''^.;^ ; - " : - "- ;L ; . ^i ;.\:.: ;:

Magnetometer and Base Station Instrument Data | f'- ' ' ; li

If a proton rich fluid such as Kerosene/ jet fuelj f

heptane, etc. is placed into a magnetic field the protons

will align along the magnetic field vector. Th,e magnetic ; '

field is induced in the sensor upon depressing tfne push

button. Then- this field is suddenly removed. Protons ji

which behave-as elementary gyroscopes will start P^e-

cessing around the remaining magnetic fie!4'that; of the j

earth. The precession frequency is directly proportional jx . . l

to the magnetic field of the earth. The magnetometer |

counts this frequency/ divides it by the appropriate

constant to obtain a reading in gammas and displays the j: '' ' - i

reading in the form of a 5 digit number. j

Coupling a standard proton magnetometer!' with a j

strip chart recorder provides a magnetic base station.' Thej

magnetometer reads the field as described above but electrically

transfers the reading to the recorder which makes a printed ^

record on a strip chart. Typical recorders allow various l

reading rates, paper speeds/ scale widths/ and display formats. ;W

SPECIFICATIONS

Range:

Accuracy:

Sensitivity:

Gradient Tolerance:

Power:

Power Consumption:

Polarizing Power:

Number of Readings with l Battery Set:

Frequency of Readings

Controls:

Output:

Indicators:

Mechanical;

Instrument: Dimensions

Weight:

Sensor:

Dimensions

Weight:

Ambient Conditions:

Environmental:

BARRINGER RESEARCH LIMITED

GROUND MAGNETOMETER

MODEL GM-122

20,000 to 99,999 in 12 ranges j ji - i 'i- l gamma through operating temperature rangej

;l gamma

600 gamma/ft.

12 "D" cells

^50 Joules (Wsec) per reading

0.8 A @ 13.5 V for 1.5 sec. (3 second cycle) '

0.8 A @ 13.5 V for 3 sec. (6 second cycle)

2,000 - 10,000 depending on type of batteries

l every 3 seconds l every 6 seconds

Pushbutton switchRange Selection switch - Slide switch ;for 3 and 6 sec. located on P/C Board \**- '5 digit incandescent filament readout i

LED point r Lock Indicator - last three digits of the t display blanked off when phaselock not achieved Segment Function Indicator - all segments lidht up to permit visual inspection of the display function

: 7" x 3.5" x 11"(18 cm x 9 cm x 28 cm)

8 Ibs (3.6 kg) including batteries

Omnidirectional noise cancelling toroidal sensing head

: 4-7/8" (12 cm) diameter 4-3/8" (11 cm) height

3 Ibs (1.4 kg) :

Operating Temperature Range - -40 0F to 131 0F (-40 0C to 55 0C)

Relative Humidity - O to 10096

Instrument and sensor case made impact plastic

SCINTREX

TOTAL FIELD MAGNETIC BASE STATION

MODEL MBS-2

SPECIFICATIONS;

Resolution

Total Field Accuracy

Operating Range

Gradient Tolerance

Sensor

Sampling Rate

Clock Accuracy and Stability

Visual Outputs

External Outputs

Time Marker

l gamma

- l gamma over full operating range

20,000 to 100,000 gammas in 25 overlapping switch selectable steps

Up to 5000 gammas/metre

Omnidirectional, shielded, noise-tanceliing, dual coil

Internal control: switch selectable every 2, 4, 10, 30 seconds or l, 2, 10 minutes

External control: manual command or by external clock at any rate longer than 2 seconds. For external trigger, a positive transition from O to +4V or greater initiates one reading

- 10 ppm over full temperature raftge

5 digit light emitting diode numerical display lasting 0.1 seconds ia automatic jj-ecycle and 1.7 seconds in manual mode. ! V-. . l - '. -v Internal strip chart recorder witty 65 nunwidth and 100 or 600 mm/hr chart s;peed f''"'., less recording. Switch selectable at 10, 100 or 1000 gammas full scale

5 digit, 1-2-4-8 BCD DTL, TTL compatibly Y --:(2 loads) with 0.5 msec, 5V.,pulse']f9a:J'..^/;';'^ synchronization of MBS-2 and external recorileil i^-' ' ' '' ' ' ' ''- -o'--/'''/-'vv^'l; 1-" Analogue recorder output of IV at il mA max^y; ;; .Switch selectable for 10, 100 or l^OOp gainma^*|^ full scale. . ":l '. . '' ' ""'' v; ;-'-;- ; :,;'';; :]V-;'"

A 1.5 second pulse every 10 minutes gener^^s^j?;; a time mark on the internal or on external;:' analogue recorders. , ' V'.'.i;

. ! ,5*V;

For an external analogue recorder,la switch tc ground is provided (NPN transistor, 40V maj?., 250 mA max). No side pen is required for - continuously writing recorders as Ithe peni rew-, turns to zero at every event mark. ;

Intervals of less than 10 minutes are optibnail^,''

isor Cable

Power Requirement

Battery Test

Operating Temperature Range

Dimensions

Weights:

Shipping Weight

Optional Accessories

50 m length is standard !

The internal batteries of the MP-2, (8 "D" cells) are used to power all functions of the MBS-2. This power source lasts appoxj- imately 80 hours, at 25 0C and a once per minf ute sampling interval. i

An external 10 to 32V DC supply may altern atively be used.

Current drain is approximately 0.9A during polarize time and 35 mA during standby, de pending upon supply voltage.

Digital readout of normalized internal battery voltage activated by touching switch.

Console: O to 50 0C Sensor: -35 to 50 0C

Console: 140 mm x 310 mm x 390 mmSensor: 80 mm diameter x 150 mm lengthTripod: 130 mm extended length

Console: 7.7 kg Sensor with cable: Tripod: 1.5 kg

Approximately 18 kg

5.5 kg

Sensor monopod, harness, sensor backpack and ' 2 m sensor cable allow field portable survey j use of MP-2 magnetomater. See MP-2 specific^ tion sheet. j

Ontario

Ministry of Natu

GEOPHYSICAL - GEOLOGI 3' Me5SEa069 a 2^32 G i LL i ES TECHNICAL DATA

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETCj,

900

Type of Survey (s) Geophysical EM ex Magnetic Township or Area Gillies Limit N. Part____' Claim Holder(s) St. Joseph Explorations Ltd* '

Box -350 f Cobalt Se 90 Eglinqton1^m——, ,. Toronto, Ont. Exoloration

MINING CLAIMS TRAVERSEDList numerically

t H

oSurvey Company fit-.,

Author of ReportAddress of Author Box 86 7 y Hail-eybury, Ontario

A. W. Beecham

Covering Dates of Survey Peg. 1977 - June 1978(linecutting to office)

_____6.9^——————Total Miles of Line Cut.

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 claimGeophysical

—Electromagnetic—f** ,

TT —Magnetometer____20.-Magnetometer.-Radiometric—-Other—————Geological.Geochemical.

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

Magnetometer. .Electromagnetic.

DATE:.

(enter days per claim)

SIGNATURE:.

S-39909Q (""""'""ipVehxi"yj^

S-399091 yt-

S-399094 .Jh

(number)

y

(T 47923 psitented claiih)

enrrSii * * t * r* * * * * *^^K* * * * * * * *

Res. Geol.. QualificationsPrevious Surveys

File No. Type

Author of Report or Agent

Date Claim Holder

TOTAL CLAIMS.

GEOPHYSICAL TECHNICAL DATA

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

Number of Ration* EM - 64* Magnetic 472_______Number of Readings EM 94; Magnetic 4,72

Station interval EM 100 ftj Mag, 50 ft^—^————Line sparing EM 400 ftj Mag* 200 |ft. Profile scale EM l" - 20&______________________________________________ Contour interval Magnetics 100

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Accuracy — Scale constant ___± IffDiurnal correction method Base station recorder Scjntriex MBST 2 Base Station check-in interval (hours) Reading every fBase Station location and value Core shed Bailey property near gfldfr Lake, Coleman

Twp.; value 59056 Y——.——————\——.—— v _________ . . . \-* - , :

Instrument Apex Parametric Max-Min II EM System.____-' ' i______ iCoil configuration Co-planar Horizontal________________' ________':- '. -.-- i.Coil separation ______200 metres.___________________________j - \ j

y i ^ j . j :

Method: D Fixed transmitter D Shoot back GH In line G3Parallel li^ie Frequency_________________1777 gc 444 # -L.- ——————^—^4^-—————.

(specify V.L.F. station)

Parameters measured In-phase S out-of-phase_________________;^^^^

Instrument.Scale constant.

Corrections made.

Base station value and location .

Instrument ————————————————————————————————————————————.—;—— Z Method D Time Domain d Frequency Domaino ———H Parameters — On time __________________________ Frequency -—---—. 4

CO53W Power.

U *13 Electrode array —2 Electrode spacing .

Type of electrode .

— Off time ___________________________ Range.— Delay time ——————————————————————————— Integration time _____________________

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BASE LINE

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Mox-Min n

Frequency: 444 Hz.

Coil Separation: 200 m.

Operators: M.Marren C. Rsrity

April 2,1978

-10

In-Phase

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. iProfile Scale: f-20%

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ST. JOSEPH EXPLORATIONS LIMITEDTORONTO. CANADA

Blocks 2S3 of Gillies Limit Twp. and Bradtey-Scheak OptionCobalt, Ontario

— KLE.M. SURVEY—SCALE.APPROX. LAT. S LONG Of1 LOWF.R RT COR OF DWG

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PHO.IfcCI NO 133.4

REPORT

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LEGEND

Mox-Min II

Frequency: 1777 Hz.

Coil Separation: 200 m.

Operators: M. Marten C. Ferity

April 2,1978

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Profile Scale: 1=20^0

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— KLE.M. SURVEY-

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LEGEND

Instruments: Barringer Research GM-122 Scintrex MP-2

Contour Interval: 100 gammas

Operator: R. Roscoe

Survey Dates: December 21,22, 1977 March 13,14, 1978

ST J OSEPH EXPLORATIONS L IMITED

Cobalt, Ontario

-GROUND MAGNETOMETER SURVEY(Tb1al Reid)