jul-61978 mining lands section st. joseph …€¦ · lines approximately at right angles to the...
TRANSCRIPT
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
u!
SSw j
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y, Instrument Barringer GM-122H W
O
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
5SLEGEND
Mox-Min n
Frequency: 444 Hz.
Coil Separation: 200 m.
Operators: M.Marren C. Rsrity
April 2,1978
-10
In-Phase
* z
Out-of-Phase
. iProfile Scale: f-20%
10 S l O
-i
-15 S
-20 S
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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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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ST. JOSLPH E XPLORATIONS LIMITED
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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)