42AiaSE8ie5 2.5322 JAMIESON 010
REPORT ON
GROUND MAGNETIC AND ELECTROMAGNETIC SURVEYS
IN JAMIESON TOWNSHIP
PORCUPINE MINING DIVISION
TIMMINS AREA, ONTARIO
NTS: 42A/12
TORONTO, ONTARIO, CANADA DECEMBER, 1982
J. A. Mccance, P. Eng. SAMIM CANADA LTD.
. 42A12SE0105 2 .5322 JAMIESON
TIMMINS PROJECT - MAT GRID
JAMIESON TOWNSHIP, ONTARIO
GROUND MAGNETIC AND ELECTORMAGNETIC SURVEYS, 1982
010C
TABLE OF CONTENTS
1. INTRODUCTION
2. THE PROPERTY
3. LOCATION AND ACCESS
4. GEOLOGY
5. PREVIOUS WORK
6. SURVEY PROCEDURES
6.1 LINE CUTTING
6.2 MAGNETICS
6.3 ELECTROMAGNETICS
7. SURVEY RESULTS AND INTREPRETATION
7.1 MAGNETICS
7 .2 ELECTROMAGNETICS
8. CONCLUSIONS AND RECOMMENDATIONS
PAGE
1
2
3
4
5
7
7
7
8
10
11
12
14
APPENDICES
APPENDIX "A"
APPENDIX "B"
CERTIFICATE - J. A. McCance
TECHNICAL DATA STATEMENT including
LIST OF CLAIMS and INSTRUMENT
SPECIFICATION DATA.
LIST OF FIGURES
FIGURE 1: Mat Group, Jamieson Township Scale l" = 1 /2 mile
FIGURE 2: Location MapScale l" = 4 miles
FIGURE 3: Mat Grid Sketch
GEOPHYSICAL MAPS
Magnetic Countours 1:2,500
EM Profiles 444 Hz 1:2,500
EM Profiles 888 Hz 1:2,500
EM Profiles 1777 Hz 1:2,500
EM Profiles 3555 Hz 1:2,500
l Sheet
l Sheet
l Sheet
l Sheet
l Sheet
5 Sheets)in pockets at end of report.
TIMMINS PROJECT - MAT GRID
JAMIESON TOWNSHIP, ONTARIO
NTS: 42A/12
GROUND MAGNETIC AND ELECTROMAGNETIC SURVEYS, 1982
1. INTRODUCTION
In August, 1982, ground magnetic and electromagnetic surveys
began on claims staked in November 1981 to cover an isolated
three channel INPUT anomaly in north central Jamieson township.
Staked by Norcen Energy Resources on behalf of the Timmins
Joint Venture Group, these 11 contiguous claims were subsequently
transferred to Samim Canada Ltd., the current owners and
manager/operator of the joint venture activities, having
assumed Norcen's position upon its withdrawal from all mineral
exploration near the end of 1981.
Evaluation of the exploration potential of these claims was
initiated with the entire property being gridded at intervals
of 125 metres. Field work included Max-Min II horizontal-loop
EM and total field magnetic coverage at regular intervals. All
field work, data and map preparation including profiling and
contouring was effected using contract facilities local to
Rouyn, Quebec. The finished maps and an operational report
were then delivered to Samim Canada Ltd. in Toronto for
interpretation.
This report contains an interpretation of these survey results
with recommendations.
- 2 -
2. THE PROPERTY
The MAT GROUP consists of 11 claims staked in November 1981.
Numbered P.633777 - P.633782 and P.633787 - P.633791 inclusive
these claims are recorded on the Ontario Ministry of Natural
Resources claim map number M-288. They are located in lots
6 and 7 concessions IV and V, Jamieson township.
An outline of this claim group is indicated in Figure l with
all claims listed in numerical sequence on the technical data
statement in the attached Appendix "B".
(Kam Group)
L -1\ (Jamif Group) '
i__
1SC
INPUT Anomaly
MAT GROUP
Jamieson TownshipScale: l"* 1/2 Milt
Figure l
- 3 -
3. LOCATION AND ACCESS
The approximate centre of the MAT GROUP is located about
12 miles (19 kilometres) northwest of Timmins, Ontario (see Figure 2). Co-ordinates of this centre point are 81 0 31'30"W longitude and 48 0 35'30" N latitude as indicated
on the 1:50,000 series topographic map 42A/12 "KAMISKOTIA LAKE".
Access to this property was by boat along the Mattagami River.
This trip required a travel time of approximately one hour each way from a launch point at Sandy Falls in nearby Mountjoy
township. Access to Sandy Falls was by truck north fromTimmins.
On landing in Jamieson township a flagged trail connects with an old northwest trending drill road. Foot traversing along
this path for 3400 feet (l kilometre approximately) will intersect line O north of the baseline.
48*30
MAT GROUP
JESSOP TWP.
SCALE
t olio
l" t 4 mil**
FIG.2 LOCATION MAP
- 4 -
4. GEOLOGY
As indicated on the Ontario Division of Mines Map No. 2255 -
Robb and Jamieson townships {see R. S. Middleton Geophysical
Report l, ODM 1973), the MAT GROUP is underlain by felsic and
mafic metavolcanic rocks. However, a gabbro and ultramafic
intrusive unit indicated in the west central part of the
claim group does not appear to be consistent with either the
airborne or ground magnetic results recently obtained.
The presence of felsic metavolcanics were confirmed on the
basis of an observed airborne magnetic pattern and from the
results of a program of overburden drilling by Cominco in 1974.
These holes intersected bedrock indicating a large area of
felsic volcanics in the northern part of the claims. A mafic
metavolcanic horizon occurs within the felsic unit equally on
the basis of magnetics and some of the overburden holes. Three
of these holes, close to the felsic-mafic contact, encountered
ankeritic sediments plus pyrite or sericitic rocks suggestive
of either a chemogenic horizon or favourable alteration patterns
being developed along this volcanic contact which strikes
through the central part of these claims.
Near the east and west claim boundaries, north and north-north
west diabase dikes cut all rocks. These dikes can be readily
identified from magnetic data.
Magnetic patterns surrounding the claim group indicate the
presence of mafic and ultramafic units near the western boundary,
Whether these units are intrusive or represent flows, possibly
similar to those in the footwall of the Kidd Creek deposit,
remains indeterminate.
No outcrop is known to exist on these claims.
- 5 -
5. PREVIOUS WORK
This area has been surveyed by at least three previous air
borne magnetic and/or electromagnetic surveys between 1963 arid
1975. Work completed on behalf of Mespi Mines included an
airborne EM survey by Canadian Aero Survey Ltd. in July 1963
(AFRO file 63.1324) and an airborne magnetic survey by Hunting
Survey Corporation in 1964 (AFRO file 63.1322). While Hunting's
magnetic results, obtained on northeast oriented flight lines,
provided useful mapping information, the Canadian Aero Survey's
EM results from 8 north-south lines covering this property
detected no anomalies. No subsequent ground follow-up appears
to have been undertaken by Mespi.
A similar survey completed over the northeastern half of this
property by Canadian Aero on behalf of Conwest Exploration
also failed to detect anomalous conditions. These results
obtained from 5 flight lines oriented in a northwest direction
have been previously reported by A. R. Rattew (AFRO file 63.1389)
and are available at a Toronto office of the Ministry of Natural
Resources.
A ground geophysical program to include lot 7 and the west half
of lot 6, concession IV Jamieson township was recommended to
the directors of White Star Copper Mines Ltd. by W. J. Elliott
in the mid 1960's (AFRO file 63.1361). Although details of
instrumentation and procedures used are unknown, this work was
apparently completed and reference to the Ontario Department of
Mines and Northern Affairs preliminary Map P.677 does indicate
that four single line conductors were located.
Most recent prior activity was an overburden drilling program
undertaken by Cominco during 1973-74. A total of 49 holes were
- 6 -
completed in Jamieson township with overburden depths and bed
rock types recorded. A significant area of rhyolite was detected
which Cominco subsequently flew with Mark 6 INPUT in 1975 (AFRO
file 2.1887). These airborne results obtained on 1/8 mile
lines oriented in two directions (north-south and east-west)
indicated four, three and four channel EM anomalies were present
on the claims. These anomalies were interpreted to be over
burden responses and no further work by Cominco is recorded.
No additional exploration work is known over these claims.
- 7 -
6. SURVEY PROCEDURES
All field work was performed under contract arrangements with Samim Canada Ltd. Line cutting was undertaken by Mid-Canada Line Cutting Ltd., Timmins, Ontario between June l and June 20,
1982. All magnetic and electormagnetic tranverses were com pleted by Services Exploration Enrg., Rouyn, Quebec during the month of August 1982.
J. A. Mccance supervised these field operations and prepared this report with interpretation.
6.1 Line Cutting
The entire property was systematically gridded with survey
lines cut perpendicular to an 1,875 metre long baseline striking at 300 0 azimuth {see Figure 3). Sixteen picket lines varying in length from 225 metres to 1.125 kilometres were cut. All lines were spaced at 125 metre intervals along the baseline with stations established every 25 metres on survey lines.
6.2 Magnetics
An Exploration Model G-816 proton precession magnetometer was used throughout this survey. This instrument manufactured
by Exploration Geometrics measures the earth's total magnetic field with a sensitivity of l gamma throughout a worldwide range of values.
Readings on all survey and control lines were taken nominally every 25 metres except where anomalous conditions were encountered or expected by the operator in which case 12 metre stations were observed. Anomalous conditions for the present purpose can be summarized as areas of unusually high or low
- 8 -
magnetic amplitude relative to an arbitrary background value, and areas with magnetic gradients greater than 100 gammas per nominal station interval. Diurnal variation was monitored by completing closed loops through all grid line and baseline intersection points. The time interval between checks to base was kept within one hour throughout the survey. Diurnal corrections were applied by a linear distribution of any observed variations over the time between base checks.
In total 14 kilometres of magnetic surveying was completed over the grid.
6.3 Electromagnetics
The instrument used for these surveys was an Apex Parametrics Max-Min II portable EM system. It was operated in a maximum- coupled horizontal loop mode using the in-line method of traverse. A coil separation of 150 metres was maintained throughout the survey. Observations were recorded at four operating frequencies (444 Hz, 888 Hz, 1777 Hz and 3555 Hz) using a 25 metre station interval on all survey lines. Corrections for topographic effects were not completed nor were such contributions to geologic noise considered significant throughout the area traversed.
The instrument receiver measures the in-phase and quadrature components of the local body-generated secondary field. These parameters are measured as relative quantities to a reference signal produced by the coplanar transmitting coil which is directly transmitted to the receiver console circuitry through an unshielded reference cable. All receiver observations, therefore, are a direct measurement of the secondary field as a percentage of the primary field. The relative strengths of the real (in-phase) and imaginary (quadrature) components are
- 9 -
plotted as profiles for each frequency and coil separation and are a guide to the conductivity-width product of a buried
conductor. This parameter is said to be directly related to the quantity of conducting minerals present. In-phase or
quadrature values more negative than background generally indicate the presence of conductive material as based on generalized dike and half plane models. A simple rule-of- thumb can be applied to such profiles to determine the approx imate location and width of a conductive zone. It is cautioned however, that the form of these EM response curves varies relative to the coil separation used; to the geometry of the conductive source, i.e. body width, depth and thickness, and
also relative to the frequencies involved. Consequently, by using multi-frequency and/or multi-coil separation EM tech niques in horizontal loop measurements it is often possible to:
(1) determine anomalies due to overburden effects and to distinguish these sources from more important bedrock sources.
(2) Acquire information suitable for a detail evaluation of both the lateral and vertical parameters of conductors observed as horizontal loop anomalies.
(3) Detect weaker or multi-source conductors even
under difficult terrain conditions and attempt an evaluation of the associated body width, depth and conductivity-thickness parameters.
A test program report prepared and widely disseminated by J. E. Betz, consultant for APEX PARAMETRICS, is recommended for further discussion on the system components, field performance and handling characteristics of this instrument.
In total approximately 12 line kilometres of survey were completed,
- 10 -
7. SURVEY RESULTS AND INTERPRETATION
All magnetic data, corrected for hourly drift and diurnal
variation are presented as contours on an enclosed plan map
(see map pockets). A contour interval of 100 gammas has been
used with all corrected data presented as representative values
only. Actual values may be obtained by the addition of 58000
gammas (nanoteslas) to each representative number. A map scale
of 1:2,500 and a plan representation of the grid showing all
stations occupied has been used in the preparation of a base
map for these data.
The electromagnetic data are plotted in profile form as in-phase
and quadrature values according to the operating frequencies
used. Four maps were thus prepared with these profiles plotted
using a data scale of l cm " 10% and a presentation (map) scale
of 1:2,500. All data were presented on a plan of the grid system
presented at map scale. Observed data points are incorporated
into the overall profile lines with respective in-phase values,
quadrature values and station positions identified on each of
these 4 maps.
An index map, any geographic features, observed and assumed
claim post positions, claim numbers and the position of any EM
conductors, as located by the contractor, have been added to
all plans (see map pockets).
- 11 -
7.l MAGNETICS
This grid is generally characterized by weakly anomalous closures
which define several irregularly shaped anomalies with magnetic
values exceeding 1400 units (59400 gammas).
The magnetic anomaly with the strongest magnetic relief {^600
units) occurs on line 11+25W in the vicinity of the baseline.
A short conductor appears to be coincident with this anomaly.
A series of small magnetic anomalies with relief generally less
than 300 gammas are located in the southeastern part of the
claim group. The north-south alignment of these anomalies
suggests the presence of a diabase dike perhaps offset by east-
west faulting near station 3+50N, line 2+50W. A similar linear
trend of anomalous magnetic depressions, with relief approximately
300 gammas below a background level of 59300 gammas approximately,
occurs from 3+50N, line 18+75W to 3+OOS, line 13+75W. This
magnetic low may identify a fault but it is interpreted to in
dicate the presence of a north trending diabase dike near the
western boundary of the claim group. An incompletely defined
500 gamma (approximately) anomaly near 4+50S, line 16+25W may
characterize the magnetization of such a dike.
Other magnetic anomalies do occur near the baseline in the
central part of the grid however no definite trends or patterns
are observable.
- 12 -
7.2 ELECTROMAGNETICS
Six weak conductors were outlined. They are best defined by the profiles of the observations taken using the 1777 Hz frequency. All conductors show a strong frequency dependence making it difficult to distinguish the sources of such features as occuring distinctly within bedrock. Particularly, the data obtained from observations at the 3555 Hz frequency show the distortion effects caused by deep conductive overburden.
Conductor A identified as extending from line 13+75W where it is centred at 3+OON to line 5+OOW, station 1+50N is interpreted to be caused by variable relief on the bedrock surface. Whether this relief reflects prevailing structural conditions within bedrock or a prevalent weathering or glacial effect remains indeterminate. This conductor does not however appear to be coincident with any magnetic anomaly.
Conductor B crosses line 15+OOW at 1+25N and line 13+75W at 0+75N. While it appears to be associated with a magnetic high on line 15+OOW it is interpreted to be an overburden effect. On line 13+75W a bedrock ridge extending from station 1+50N to 2+OON is interpreted to be the cause of both conductors A and B on this line. The presence of a weak sulphide system in bedrock cannot be discounted based predominantly on the in-phase response observed. But the presence of conductive massive sulphides of significant width and depth extent are not indicated directly by these anomalies.
Conductor C, identified as a two line response trends east-west and is directly related to a relatively strong magnetic anomaly. It has been outlined on line 12+50W at 0+50S and on line 11+25W at 0+25N. The effects of conductive overburden are suggested to
- 13 -
cause the quadrature reversal observed at 1777 Hz on line 12+50W
and a positive effect on the negative in-phase peak on line
11+25W. A thin sulphide source in bedrock perhaps containing
pyrrhotite is suggested to be the source for this EM feature.
Conductor D is also observed as a two line anomaly located on
line 5+OOW at 1+OOS and line 3+25W at 1+50S. There is no co
incident magnetic anomaly and it is interpreted that the source
does not occur within bedrock. On line 5+OOW it is suggested
that anomalies A and D reflect the presence of a buried ridge
perhaps 50 metres to 60 metres wide which is centred at station
0+25N on this line. Overburden drill results in the vicinity
of this ridge confirm the presence of up to 15 metres of relief
on the bedrock surface. This relief may be fault controlled
and occurs within a zone of ankeritic sediments containing
pyrite located at a depth of approximately 30 metres.
Conductors E and F occur only on line 3+75W. These one line
responses occur at 0+25N and at 2+25N respectively on this line.
They are interpreted to reflect the development of a bedrock
ridge perhaps associated with east-west faulting interpreted
to extend form 3+OON, line 2+50W to 0+50N, line 5+OOW. Neither
conductor is associated with magnetic anomalies.
- 14 -
8. CONCLUSIONS AND RECOMMENDATIONS
There are no distinct indications of a conductive massive sulphide
body occurring within this grid. However, the favourable strati
graphy, positive geological and geochemical indications and
possible similarity to the geologic environment at the Kidd Creek
mine suggest that more exploration is warranted.
It is recommended that conductor C be considered a tentative
drill target pending the completion of limited IP traverses on
line 13+75W, 11+25W and 8+75W. Further drilling to test other
indications in this area should await these results.
Respectfully Submitted,
J.A. Mccance, P.Eng.
APPENDIX "A"
CERTIFICATE
CERTIFICATE
I, JOHN A. MCCANCE of the Borough of North York, Metropolitan Toronto,
Province of Ontario do hereby certify:
1. That I am a geophysicist and reside at 113 Hendon Avenue,
Willowdale, Ontario.
2. That I graduated from Queen's University at Kingston in 1970
with a degree of Bachelor of Science, Faculty of Applied
Science and have completed post-graduate training at the
University of Western Ontario, London.
3. That I am a member of the Association of Professional
Engineers of the Province of Ontario (Mining Branch).
4. That I have been practising my profession for a period of
ten years.
5. That I am employed by Samim Canada Ltd. as Chief Geophysicist.
6. That I supervised all 1982 survey operations.
Date: December 27th, 1982 J. A. Mccance, P.Eng.
APPENDIX "B"
TECHNICAL DATA STATEMENT
including LIST OF CLAIMS
and INSTRUMENT SPECIFICATION DATA
EiViAXBV1IE\JEM
m Five frequencies: 222, A44, BBS, 1777 and 35SS Hz.
m Maximum coupled C horizontal-loop 3 operation with reference cable.
m M inimum coupled operation with reference cable.
m Vertical-loop operation without reference cable.
B Coil separations: 25, 50,100,150,200 and 25Om C with cable ) or 1OO,2Oa,3OO,4OO,BOOand BOO ft.
m Reliable data from depths of up to ISO m C BOO ft 3.
m Built-in voice communication circuitry with cable.
m T ilt meters to control .coil orientation.
• - -"•^*
P:' .
SPECIFICATIONS :
Frequencies:
tVlodes of Operation:
222.444. BSa. 1777 and 3555Hz. Repeatability i
Coll Separations:
Readout*:
Scale Ranges :
NOW ALSO ± QUADRATURE FULL SCALE,
Readability:
MAX: Transmitter coil plane end re- ceiver cxail plane horizontal CMax-coupled; Horizontal-kjop mode). Used wtthi refer.cable.
M l N: Transmitter coil plane horizon tal end receiver coil plane ver tical C Min-coupled mode). Used with reference cable.
V.L. : Transmitter coil plane verti cal and receiver coil plane hori zontal tVertical-loop mode J. Used without reference cable, in parallel linea.
25.5O,1OO.15O.2OO S25Om CMMID or 1OO. 2OO. 3OO. 4OO.BOOand BOO ft. tMMHF). Coil separations in VL.mode not re- atricted to fixed values.
Parameters Read: . In-Phase and Quadrature compo nents of the aeoondary field i n MAX end MIN modes.
- Tilt-angte of the total field in V.L. mode .
- Automatic, direct readout on SO mm (3.5") edgewise meters in MAX end MIN modes. No null ing or compensation necessary.
- Tilt angle and null in SO mm edge wise meters in VL.mode.
In-Phase: ±2Oy..±1OO14 by push button switch .
Quadrature:*2O%.t1OO% by push button switch.
Tilt: *75*A slope .NullCVLJ: Sensitivity adjustable
by separation switch.
In-Phase and Quadrature : 0.25 */. to O.5V. ; Tilt: 1V. .
±O.25*Ato*1^i normally, depending on conditional frequencies and coil separation uaed.
Transmtttar Output i. 222Hz i SSOAtm8- 444Hz tSOOAtm0- BBS Hz : 12OAtmE- 1777 Hz s BOAtmB-3555 Hz t 3OAtmB
Receiver Batteries t sv trans, radio type batteries 14). Life: epprox. 35hrs. continuous du ty (alkaline. O.5 Ah), lees in cold weather.
Transmitter Betterlaa t
Raferenca Cabla t
Voice Link i
Indicator Lights:
12V B Ah Gel-type rechargeable battery- (Charger supplied).
Light weight S-conductor teflon cable for minimum friction. Unshield ed. All reference cables optional at extra coat. Please specify.
Built-in intercom system for voice communication between re ceiver and transmitter operators In MAX and MIN modes, via re ference cable .
Built-in signal end reference warn ing lights bo indicate erroneous readings .
Temperature Range: -4O*Cto*BO*C C-4O*Fto*14O*F).
Raoelvar Weight: 6kg (13lba.)
Transmitter Weight! 13kg (SSIbs.)
Shipping Weight: Typically BOkg C135lbs.), depend ing on quantities of reference cable and batteries included. Shipped in two field/shipping cases.
Specification* aubjacc to c ne ne* without notification.
APEX PARAMETRICS LIMITED2OO STEELCASE RD. E., MARKHAM, ONT. CANADA. L3R 1G2
Phone: (41B) 4S5-1B1S Cables: APEXPARA TORONTO Telex :O6-B66776 APEXPARA MKHM
Minislryof Natural
•ourcesOnianl
Report of Work(Geophysical, Geological, Geochemical and Expenditures)
42A12SEei05 2 .5323 JAMIESON)"
The Mining n**900
a p^.^ - w -jp'vpo of Survfly(s) " ————————
j Electromagnetic and Magnetic_______i Cl.-mn l-iolcior(s)
S am imjCanada^ Ltd..———————-————.Address
^wn.hip or Area
Jamieson -JLLicence No,
T-1193
Suite 2116, 130 Adelaide Street West, Toronto, Ontario, M5H 3P5Date of Survey (from 81 to)Survuy Company
Services Exploration E.N.R. Rouyn, Quebec Day l MO.Name and Address of Author (of Geo-Technical report)
J. A. Mccance c/o Samim Canada Ltd. (see above)
14 ,08,82 30 .09X82Day l Mo. j Yr.
Total M iles of l ine Cut
14j) Kilometres
Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Slioulnl Provisions
For first survey:Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter total (s) here
j Airborne Credits
Note: Special provisions credits do not apply to Airborne Survuys.
Giophyiical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days perClaim
20
40
Days per Claim
Days per Claim
Expenditures (excludes power stripping)1 Type of Work Porformod
- ) \:i ! ormod on Cluirn(s)
i
i
Calculation of Exinindituro Days Credits
'1 oUil Exponditures
^ -*-15
cTotal
Jays Credits
Instructions Touil Days Credits may be apportioned at the claim holder's choice. Enter numbur of days credits per claim selected in columns at right, "^
Uiiio Recorded Holden
November 3/82 \ . tVfA/^-ir Agent (Signature)
Curtiliciition Vcsrifyiiiti Fiep/irt of Work (1 hereby certify that 1 have a persona or witnessed same during and/or after
Mining ClaimPrefix
P
Numbtr
633777
633778
633779
633780
633781
633782
633787633788
633789
633790
633791
RECO1f*U'V
Keceipt No. . .
Expand. Diyi Gr.
.'
*DE
5^969
T
For Office Use OnlyTotal Days Cr. Recorded
'A 7
Date Recorded . .
JlO'l^n.'f-i'i^^/O.-'iLr" tftiflir"y^*^** i ** "t"* j
Mining ClaimPrafix
•'.T-
'
:-'' .:
Number
— -
Total number of mining claims covered by this report of work.
' \
piinlng Recorder ,
T? u —————
Expend. Days Gr,
j
i
.... . . ...
t
i 1
i 11
**-"1 f
* ~ .' t ' .|
^ ~
and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work its completion and the annexed report is true.
Ncunu and PoMiil Addross of Purson Certifying
John A. McCance y 130 Adelaide Street West
I3U2 (81/0)
finite 511 fi Toronto. Ont . . M5H 3P5Date Certified |Ce
November 3/82 |^M If lad by (SignjU/ire)
' Mat Group VJ
RECEIVEDWOV-919& "
MINING LANDS SECTION
Ontario
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.
gMK)
Type of Survey(s) Magnetic and Electromagnetic
Township or Area Jamieson Township (Mat Group)
Claim Holder(s)___Samim Canada Ltd.——————^——-
130 Adelaide St. W. Suite 2116, TorontoSurvey Company__Services Exploration Enry. — Rouyn. Oue.
Author of Report J. A. Mccance——^^—-——^^————— Address of Author 130 Adelaide St. W. Suite 2116, Toronto
Covering Dates of Survey June l, 1982 - December 27, 1982(linecutting to office)
Total Miles of Line Cut. 14.0 Kilometres
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical—Electromagnetic.—Magnetometer——Radiometric———Other———-——.
DAYSper claim
20
40
Geological.Geochemical.
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
Magnetometer. .Electromagnetic.(enter days per claim'
HATE- December 27/82 SIGNATURE:
Res. Geol.. .QualificationsPrevious Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
(number)
,i?.t....
.P.,,,,,,,,S.3,3.7,8,0,
.P.,,..,,.,
P.
P, 633787•••••••••••••••••••••••••••••••••••••
• Act **t****t****** •VfTVT* i *V*T* ****t
• /••^•••••••••••••* *5r *T*V* 1 1rt •TT* •••••
i * n *t •••••••••••••* rt*"s*T * t rt *V* •••••
l
TOTAL n.ATMfi Eleven (11)
837 (5/79)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS — If more than one survey, specify data for each type of survey
Number of Stations. Station interval —-— Profile scale ————Contour interval.
EM 416 MAG 662
25 metres, 12.5 metres
EM 1664 .Number of Readings MAG 662.Line spacing_______125 metres
l cm = 1 0% EM only
100 nanoteslas — magnetics only
ctizc<3
Instrument. Exploranium G-816 proton precession total field device
Accuracy — Scale constant Accuracy greater than 5 nanoteslas at each station.
Diurnal correction method — 1 nnpg t:n si^wey 1 ine^intersection no jnts
Base Station check-in interval ( l Base Station location and value
l hour or less
Line 0. Baseline 00 equals 59.264 nanoteslas
yh a zcssaj w
InstrumentCoil configuration Coil separation —. Accuracy ————— Method: Frequency————
Apex Parametrics Max—Min II EM Unit
Horizontal Coplanar
150 metres
In-Phase and Quadrature
CD Fixed transmitter CI Shoot back 444 Hz. 888 Hz. 1777 Hz and 3555 Hz
S] In line O Parallel line
Parameters measured In-Phase and Pug{specify V.L.F. station)
ants of anomalous field as a
percentage of the primary field strength at the receiver.
Instrument —— Scale constant.Corrections made.
O Base station value and location .
Elevation accuracy.
Instrument
INDUCED POLARIZATIO
Parameters — On time^ — Off timeH JJ — Delay timeH — Tntpgratinn t imeNH
f^ Powerc*
Electrode array. ———————————————————Electrode spacing . ———————————————————Tvoe of electrode .. ———————————
Frequency
Ranpe
———————————————————— |
SELF POTENTIAL Instrument___________i_____________________________ Range.Survey Method ————————:—————,—,——:———————.—^—————^—...——
Corrections made.
RADIOMETRICInstrument———.Values measured.Energy windows (levels) ——^^—^^——^^———————————^^—.^———^-^^—.Height of instrument———.——————-——^^^^——.—.^^^——,Background Count.Size of detector^—^-———————^^————^^.^—————————^-^^—.^^^^^^^^^Overburden ———^^^^——————————^—^^^—...—..——.......^^—^—..—
(type, depth — include outcrop map)
j)THERS (SEISMIC, DRILL WELL LOGGING ETC.)ppe of survey———————————————————————
Instrument ——^^——^—^^—^^—————^-^— Accuracy———————————————————————————Parameters measured.
Additional information (for understanding results).
AIRBORNE SURVEYS 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.
Aircraft altitude_______________________________Line Spacing—— Miles flown over total area________________________Over claims only.
GEOCHEMICAL 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.
Mesh size of fraction used for analysis.
General.
ANALYTICAL METHODSValues expressed in: per cent
p. p. m. p. p. b.
D Dn
Cu, Pb,
Others_
Zn, Ni, Co, Ag, Mo, As,-(circle)
Field Analysis (. .tests)
Extraction Method. Analytical Method- Reagents Used——
Field Laboratory Analysis No.(——————————
SAMPLE PREPARATION(Includes drying, icreening, crushing, ashing)
Extraction Method. Analytical Method. Reagents Used——
Commercial Laboratory (. Name of Laboratory— Extraction Method—— Analytical Reagents Used
.tests)
General.
Ministry ofNaturalResources
Ontario
GeotechnicalReportApproval
Mining Lands Comments
To: Geophysics
Comment*
QAfSp'roved f~] With to tee again with correctioni
To: Geology - Expenditures (7Comment!
^ Approved f~| With to tee egeln with correctioniDate Signature
To: Geochemistry
Comments
Approved |~| With to tee agal n with correction!Date Signature
j fro: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)
1593(81/10)
1983 01 07
413
2.5322
Mining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioPAN 2S7
Dear SinMe have received reports and maps for a Geophysical (Electromaonetlc and Magnetometer) Survey submitted under Special Provisions (credit for Performance idd Coverage) on Mining Claims P 633777 et al 1n tbe Township of Jamieson.This material will be examined and assessed and astatement of assessment work credits will be Issued.Yours very truly.
E.F. AndersonDirectorLand Management BranchWhitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380
DW:sc
cct SabUM Canada Limited Toronto, Ontario Attnt J.A. Mccance.
July 15, 1983 2.5322
Samlm Canada LtdSuite 2116130 Adelaide Street WestToronto, OntarioM5H 3P5
Attention: J.A. HcCance
Dear Sir:
RE: Geophysical (Electromagnetic and Magnetometer) survey on mining claims 4* 633777 et al 1n the Township of Jamieson
With reference to the above-mentioned survey, returned herein Is the last page of the report (1n duplicate). Please sign these pages and return them to this office quoting file 2.5322.For further Information, please contact Mr. W.W. Matthews at (416)965-1380. kYours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6450 Queen's Park Toronto, Ontario M7A 1M3
:*:
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j me -'
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1^-S:l.';^Stli:SJ"*gl-- --'it"fi*fe-tf^"*a5i A*l5rl-;...
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WBSV 4, r'^jf:
Canada Ltd.
December 31, 1982
Ontario Ministry of Natural Resources, Mining Lands Branch, Whitney Block Queens Park, Toronto, Ontario
Attention: Mr. F. W. Matthews
Re: Submission of Ground Magnetic and Electromagnetic Data for Assessment Work on 11 claims in the Por cupine Mining Division: P. 633777... etc.
Dear Mr. Matthews,
Enclosed please find two copies of a report plus maps resulting from combined ground magnetic and electromagnetic surveys recently completed in Jamieson township, Porcupine Mining Division. This work was completed under contract for a joint venture group of companies for which Samim Canada is currently the operator/manager.
We are hereby requesting that this submitted work be recorded as 60 days assessment credit on each of these 11 claims.
Yours truly,
JAM/dg J. A. MccanceChief Geophysicist
Encl: Report and map c.c.: D. S. Kerby
130 Adelaide St. W. Telephone - (416)863-0168 Suite 2116, P.O. Box 7 Telex 06-217829 Toronto, Canada AA5H 3P5
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