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4l009NW0eS7 2 .7004 BENTON010
GEOLOGICAL AND GEOPHYSICAL SURVEY REPORT
CANADIAN NICKEL COMPANY - M.L. BURTON -
C.S. BURTON - A.S. BURTON OR. AGREEMENT
ESTHER AND BENTON TOWNSHIPSPORCUPINE MINING DIVISION
NTS: 4109
Canadian Nickel Company Limited Copper Cliff, Ontario May, 1984
Table of Cor
— — -- —-' —m ^ ,m mm mmi mimmmm m t
410e9NWW57 2 .78*4 BENTON010C
Summary
1.0 Introduction
2.0 Location and Access
3.0 Property
4.0 Previous Work
5.0 Summary of the 1983 Exploration Program
6.0 Regional Geology
7.0 Geological Survey
7.1 Basic Metavolcanics
7.2 Intermediate Metavolcanics
7.3 Metasediments
7.4 Diabase
8.0 Structure and Alteration
9.0 Mineralization
10.0 Geophysical Survey
10.1 Magnetometer Survey
10.2 VLF Survey
11.0 Conclusions
12.0 Certificate of Qualifications
2
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3
4
4
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5
5
6
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6
7
8
8
8
9
10
Figures
Figure Number Scale
1 General Location Map 1:250,000
2 Claim Map 1:50,000
3 Geology Map (Sheets 1-6) 1:2500
A Magnetometer Survey (Sheets 1-6) 1:2500
5 VLF Electromagnetic Survey (Sheets 1-6) 1:2500
Summary
The Burton property consists of 41 unpatented claims and 6 patented claims, located in Esther and Benton Townships, 167 kilometres northwest of Sudbury. Canico entered an option agreement with the Burton brothers on May l, 1983 covering the 6 patented claims and 20 unpatented claims. An additional 21 claims were subsequently staked.
The entire property was gridded. Detail mapping indicates that mineraliza tion is hosted by a strongly carbonatized thick gabbroic flow or subvolcanic sill within a pile of south facing pillow lavas. Gold tenor appears related to arsenopyrite content which varies from disseminated to massive. VLF and magnetometer surveys were carried out over the entire property. A total of 1472.3 metres was drilled in 9 boreholes.
P D fi
4—— - -(———
\ __ l___________
Figure l
Canadian Nickel Company Limited
BURTON OPTION, ONTARIO Location MapSCALE 1=250000
TWP. OSWAY TWP
47 0 40
Note :eg 558472 * P558472
Figure 2 Canadian Nickel Company Limited
BURTON OPTION, ONTARIO Claim Location Map
- 2 -
l.0 Introduction
As a result of a property examination made by Canico in August, 1982, an option agreement was entered on May l, 1983 between Canadian Nickel Company and M. Burton, C. S. Burton and A. S. Burton Jr. The option covers 20 unpatented claims and 6 patented claims located in northeast Esther Township, approximately 167 km northwest of Sudbury. Subsequently Canadian Nickel Company staked an additional 21 claims in Esther and Benton Townships to cover any possible strike extension of the mineralization.
The claims cover a showing which consists of massive to disseminated auriferous arsenopyrite hosted by a highly carbonatized gabbro-diorite. This is interpreted to be a thick flow within a thick pile of south facing, predom inantly pillowed, mafic volcanics and thin interflow sediments. The main showing is about 10 kilometres WNW of the old Jerome Mine and lies approximately along the regional foliation from that deposit.
The entire claim block was gridded, detail mapped and prospected, and covered by VLF and ground magnetometer surveys. Subsequently 1472.3 metres were drilled in 9 boreholes.
2.0 Location and Access
The property is located in northeast Esther Township and southeast Benton Township, approximately 167 kilometres northwest of Sudbury (figure 1). Access is by a gravel road (E. B. Eddy Highway 560) which runs west from highway 144 (approximately 34 kilometres south of Gogama) through Sultan to Chapleau. Branches from this road lead to the property boundary from which a drill road leads to the shaft on patented claim S 31117.
3.0 Property
The property consists of 47 contiguous claims (figure 2), 21 of which are owned by the Canadian Nickel Company and 26 under option from Martin L. Burton, Cumming S. Burton, and Archie S. Burton. The option, dated May l, 1983, covers 6 patented claims and 20 unpatented claims.
The patented claims are:
S 31116 S 31117 S 31226 S 31227 S 32578 S 32579
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The unpatented claims are as follows:
Claim
P 473385 P 558456-57 P 558458-465 P 558466-467 P 558468-475 P 558476 P 629911-912 P 648044-46 P 648047-48 P 648153-155 P 648198-200 P 648283-84 P 648285-86 P 648362-63
Township Recording Date
Esther October 12, 1978Benton February 14, 1983Esther February 14, 1983Benton February 14, 1983Esther February 14, 1983Benton February 14, 1983Esther September 14, 1981Esther July 9, 1982Esther August 19, 1982Esther September 23, 1982Esther September 23, 1982Esther September 23, 1982Esther November 2, 1982Esther November 2, 1982
Assessment Due Date
October 12, 1985February 14, 1985February 14, 1985February 14, 1985February 14, 1985February 14, 1985September 14, 1984July 9, 1984August 19, 1984September 23, 1984September 23, 1984September 23, 1984November 2, 1984November 2, 1984
Diamond drilling has been recorded as assessment work on the claims as follows:
One Year's Work
P 558456-476 inclusive P 648044-048 " P 648153-155 " P 648198-200 " P 648283-286 " P 648362-363 "
Two Year's Work
P 473385P 629911-912
4,0 Previous Work
The original showing was discovered circa 1928 by Archie Burton Sr. In 1928 Northern Aerial Minerals Exploration Limited (controlled by Burton?) trenched the showing and sank a 10 foot test pit. Subsequently a 33 foot shaft was sunk by Burton to intersect the downdip extension of a west dipping, north-south striking, quartz vein. The shaft was abandoned due to flooding problems. Numerous trenches were blasted along the strike extension to the east up to 750 metres from the shaft.
Hollinger Consolidated optioned the property and carried out a fairly extensive drill program during the late 1930's and early 1940's consisting of approximately 32 boreholes. Not all of the data has been retained. It appears the Hollinger drill program was curtailed by World War II due to a shortage of manpower and never resumed.
- 4 -
The Burton brothers have blasted several new trenches and cleaned out the older ones. They re-established the old grid and carried out a VLF survey. One possible conductor was detected but this could be due to the scrapiron left from the old drilling.
5-0 Summary of the 1983 Exploration Program
A total of 5.82 kilometres of baseline and 98.4 kilometres of grid lines were established on the property by a contract line cutter. Crosslines are at 100 metre spacing and pickets marked at 25 metre stations along the lines.
Detailed geological mapping, prospecting, and sampling was carried out over the entire property. The field data was plotted at a scale of 1:2500 and copies of the maps are appended. More detailed mapping and sampling in the shaft area is plotted at 1:1000.
Nine boreholes totalling 1472.3 metres were drilled using a Canico owned and operated Longyear 24 diamond drill.
6.0 Regional Geology
The claims are underlain by rocks of the southeast arm of the Archean Swayze greenstone belt. The belt is approximately 12 kilometres wide in the area of the claims and thins to the southeast. The rocks consist predom inantly of mafic to intermediate volcanics and metasediments. The regional foliation is 100 to 120 with a very steep to vertical dip.
The mafic volcanics are predominantly fine-grained pillow basalts. Thicker, medium to coarse grained, gabbroic flows and subvolcanic sills are also fairly common. Several major bands of metasediments varying from coarse conglomerates to shales and siltstones outcrop on the property and continue for great distances along strike (10's of kilometres) in either direction.
The rocks within the claim area occur as a south-facing homoclinal sequence, dipping vertically +10 .
7.0 Geological Survey
The. table belox*; outlines the rock units encountered on the property. No age connotation is implied as volcanism is cyclical. A description of the rock units follows:
Legend
4 Diabase
3 Metasediments
3c Argillaceous Greywacke3b Reworked Lapilli Tuff-Conglomerate3a Coarse Conglomerate
- 5 -
Intermediate Metavolcanics
2a Andesite-dacite
Basic Metavolcanics
lg Flowtop BrecciaIf Interflow Metasediments
Ifl - Argillite/SiltstoneIf2 - Chert
le Highly carbonatized gabbro Id Foliated weakly carbonatized gabbro le Medium-coarse grained gabbro/diorite (thick flow) Ib Pillow basalt la Massive basalt
7.1 Basic Metavolcanics
The predominant rock type on the claims is basalt. West of the creek the basalts are commonly massive whereas east of the creek the basalts are predominantly pillowed. The pillows range in size up to l metre in length and have thin chloritic selvages. The pillows always face south and provide excellent top determinations. Several thin horizons of flow top rubble and autobreccia were noted. One such horizon is located south of the showing around line 105E.
* Several conformable units of (medium to coarse grained) gabbroic to dioritic rocks, locally diabasic textured, are located on the property. These are interpreted to be thick basaltic flows although in part they may represent subvolcanic sills. The upper phases of the largest of these units hosts the gold-arsenopyrite mineralization where the "gabbro" has been variably carbonatized and foliated. The host "gabbro" can be traced for 2.7 kilometres and appears from surface mapping to be 200 metres thick. The thick gabbroic . flows can also be traced by magnetometer and IP as the upper phases tend to be magnetite rich. /'
Several horizons of interflow siltstone, sandstone and chert were located on the property. The thickest of these units is located stratigraphic- ally above the showing and below the upper pillowed basalts. It is presumed that such metasediments are much more common than those located in the field due to their recessive weathering nature.
7.2 Intermediate Metavolcanics
Several outcrops of andesitic to dacitic composition are located west of the creek south of the showing. These rocks are whitish-pale green on the fresh surface and white on weathered surfaces. They comprise a very minor part of the volcanic pile.
- 6 -
Trenches on line 103 contain a rusty carbonatized paper schist which may be a metasediment or altered intermediate to acid volcanic. Drilling intersected several thin rhyolitic flows.
7.3 Metasediments
Several continuous bands of metasediments, representing major breaks in volcanism, cross the property conformable to the stratigraphy. These metasedimentary belts range in thickness from 50 to 300 metres. Top determina tions from graded bedding confirm pillow facings as the metasediments become finer grained to the south indicating tops in this direction.
Three distinct bands of metasediments cross the property. At the east end of the property a pseudo-graded bedding is apparent. Basal units consist of coarse polymictic conglomerates with clast lithologies which include granite, porphyry, quartz, volcanics, and iron formation. The well-rounded clasts range up to l metre in length and are stretched parallel to foliation. The matrix is fine grained, sericitic, chloritic and locally carbonatized. These conglomerates grade upwards into finer units as the clast size decreases. At the top of the section lies siltstones, argillites, and probably ash tuffs; it is difficult to distinguish fine grained epiclastic and volcaniclastic metasediments.
At the west end of the property the conglomerate does not exhibit graded bedding. Clasts are typically 1-3 cm in size.
7.4 Diabase
Several discontinuous medium grained, moderately to strongly magnetic, diabase dykes outcrop on the property. The dykes often exhibit a strong east-west jointing pattern. Drilling intersected several medium to coarse grained bodies of apparently crosscutting diabase which had been mapped as phases of the gabbro.
8.0 Structure and Alteration
The rocks within the claim area occur as a southfacing homoclinal sequence which dips vertically -f 10 . The regional foliation is approximately HO0 .
One small fault is proposed to explain an apparent offset of the most i southerly of the metasedimentary bands. However this could also be explained as an interfingering of the volcanics and sediments. Previous mapping has suggested that a north-south trending fault runs up the creek, which could have implications for locating mineralization. No evidence was found to confirm this fault; both the metasedimentary band and the thick gabbroic flow cross the creek with no apparent offset.
- 7 -
The rocks of the region have undergone lower greenschist facies meta morphism. The basalts are predominantly "fresh" having undergone some chloritealteration. As stated previously the metasediments exhibit local carbonatization and sericitization.
A strong pervasive carbonate alteration of the upper phases of the thick gabbroic flow hosts the auriferous arsenopyrite-pyrite mineralization. Discontinuous areas of carbonatized "gabbro" can be found throughout the unit, however, the mineralization appears confined to the upper phases,. Carbona tization, locally approaching 1007o, can be traced for over l kilometre of strike length.
9.0 Mineralization
As stated above, gold/silver mineralization is related to massive to disseminated arsenopyrite/pyrite within a variably carbonatized thick basaltic flow.'A stratigraphic section through the mineralized zone from bottom to top consists of basal fresh, massive, gabbroic textured basalt. Approaching the zone, foliation intensifies and spotty carbonatization develops. As carbonatization increases, minor quartz veins develop along with disseminated arsenopyrite and pyrite. Within the main zone foliation is fairly intense (dipping vertically +10 ) and carbonatization pervasive, locally 1007,,. At this point the host rock develops a dioritic appearance. Sulfide mineralization consists predominantly of arsenopyrite with lesser pyrite, pyrrhotite and chalcopyrite, either disseminated or massive. Gold tenor appears to be roughly proportional to the arsenopyrite content. Stratigraphically above the minera lized zone, the intensity of carbonatization and foliation decreases gradually until the rock grades into fresh "gabbro", which is magnetite rich. Above this lies a band of interflow metasediments overlain by another cycle of pillowed basalts.
Gold values from massive arsenopyrite-mineralized rocks taken from the rock dump at the shaft grade as high as 6J. ppm. Rocks with disseminated arsenopyrite from trenches 55tTmetres east of the shaft assayed as high as 15.8 ppm gold. "^ l II l l. l l linn. ~.~ *~^*
A lower zone of foliated carbonatized gabbro on the baseline at 105Eis weakly mineralized with disseminated euhedral arsenopyrite. Gold values of up to 90 ppb were recorded.
Mineralization at the shaft area occurs on the grid at 100N, 100E. At 103E the mineralization has moved south to 99N. The mag survey suggests a flexure along the upper contact of the thick flow which results in this apparent offset. A similar sort of flexing may occur in the shaft-creek area as well.
* O ~"
10.0 Geophysical Surveys
The entire property was covered with magnetometer and VLF surveys.
10.1 Magnetometer Survey
Procedure;
The instrument used is a Scintrex MF-2 fluxgate magnetometer which measures the vertical component of the earth's magnetic field directly in gammas, positive or negative, over a range of 100,000 gammas. This hand held magnetometer requires no orientation and after coarse levelling the magnetic reading is recorded from a meter mounted on the top of the instrument.
Magnetic base reference stations were established at the 100 metre grid line intersections along the 100N base line from 64E to 116E. All of these base station readings are relative to the initial reading taken at 100N - 64E where the magnetometer was arbitrarily adjusted to read 1275 gammas. During the course of the survey magnetic diurnal variations were determined by tying into the base reference stations and then making necessary drift corrections to the grid line station readings. Using this correction method all magnetic readings are made relative to the first reading taken at 100N - 64E.
Results:
The entire grid was covered by a ground magnetometer survey with stations at 12.5 metre intervals. Magnetic anomalies of about 3000 gammas were found to closely correlate with the upper portions of the thick gabbroic flow. This strong anomaly weakens to the west and dies out about 500 metres west of the shaft. A second linear magnetic anomaly occurs southwest of the shaft and is coincident with the southernmost gabbroic thick flow or subvolcanic sill. Other scattered anomalies appear related to gabbroic basalts or diabase dykes.
10.2 VLF Electromagnetic Survey
Procedure:
The "Radem" VLF electromagnetic unit used on this survey was designed by Crone Geophysics Limited. An explanation of the Radem's operation is quoted
from Crone's operating instructions.
"The VLF Communication Broadcast stations are positioned throughout the world. At present, 17 of these stations broadcast steadily except for maintenance periods usually of 1/2 to 1/3 days per week. The RADEM receives any 7 of these stations with selection by means of a switch. The usable range of the stations varies widely with power and transmission conditions but is usually between 1000 and 5000 miles. Two types of signals are broadcast "keyed" (on and off) and "frequency shift" (FM).
- 9 -
A station should be selected that is located in the same direction as the regional strike. For example, if the geological strike is east-west then a station located east or west of the operator should be used. If indoubt of the geological strike two orthogonal stations should be read."
Parameters measured by the Radem unit are: (a) dip angle of resultant field, (b) out-of-phase measurement, (c) horizontal component of the field strength.
The claims surveyed electromagnetically were read at 25 meter station intervals on 100 meter spaced grid lines. Transmitting station used is NAA Cutler, Maine operating at 17.8 KHz with power output of 1000 kw. The dip angle of the resultant field and the out-of-phase measurement were recorded at all stations read.
Readings are plotted in profile form and a conductor axis is indicated when EM readings cross the section line from west to east while the operator is traversing southward.
Results:
Numerous conductors were located roughly parallel to the general strike but are not directly correlatable with the magnetic anomalies except between 103E and 107E at about 99N, where the heaviest concentrations of arsenopyrite occur. The majority of the conductors are most likely caused by overburden features or bedrock shears. It is proposed that a HLEM survey be carried out over several of the conductors to test their validity.
11.0 Conclusions
Surface mapping traced a variably mineralized zone within a strongly carbonatized thick flow for 750 metres of strike length. Gold assays as high as 60.1 ppm are closely related to disseminated to massive arsenopyrite. The magnetometer survey traced the upper phases of the thick gabbroic flow host rock. The majority of the VLF conductors appear to be due to overburden features or bedrock shears.
- 10 -
12.0 CERTIFICATE OF QUALIFICATIONS
I, Robert C. Bell, of the City of Sudbury, in the Province of Ontario,
HEREBY CERTIFY
1. That I reside at 1149 Southview Drive, Sudbury, Ontario, P3E 2L7.
2. That I am a graduate of the University of Western Ontario, London, Ontario, with a degree of Bachelor of Science (1980).
3. That I am a Geologist with the Canadian Nickel Company Limited (subsidiary of Inco Limited) of Copper Cliff, Ontario, POM 1NO.
4. That I have practised my profession as a geologist since 1980, having worked in British Columbia, Ontario, Quebec, and the Northwest Territories.
5. That I visited the areas discussed in this report and that the work described in this report was carried out under my supervision.
6. That I am an associate of the Geological Association of Canada.
Dated at Copper Cliff, this 22nd. day of May, 1984.
Ministry ofNaturalResources
OntariowjfiReport of Work(Geophysical, Geological, Geochemical and Expenditures)
The M in. ,41009NW0057 8.7004 BENTON 900
Type of SufvoyU) |Touj0OWiyw^W^^"*w^*M^^^^^^
Geophysical (Magnetometer, V.L.F. E. M.); Geological cEsther S Benton Twps.^)Claim Holder(s)
Canadian Nickel CompanyAddress
Copper Cliff, OntarioSurvey Company
Canadian Nickel Company
Limited j A 17527
POM 1NODate of Survey (from fii to) Total Miles of line Cut
Lifted W v 1 06. i 92 3JV i 02. P?, 91-4 kmName and Address of Author (of Geo-Technical report) *
Robert Bell, c/o Canadian Nickel Company Limited, Copper Cliff, Ontario POM 1NOCredits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provitions
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
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits
Total Expenditures
Date
June 20, 1984Certification Verifying Report of Work
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
,Electromagnetic"; j- ,tj" *- Magfyetomete
Total number of mining claims covered by this report of work.
Total Days Cr Recorded
DaYe-'Approved *T)RecordedRecorded Holder or Agent (Signature)
Airborne Credits
Note: S pecial provisions i Electromagneticcredits do not appiy ito Airborne Surveys, i Magnetometer
InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.
l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true,
Name and Postal Address of Person Certifying
I. D. McCaskill, c/o Canadian Nickel Company LimitedCopper Cliff, Ontario POM 1NO tfi Certified
June 20, 1984Certified lw (Signature)
l
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
FUe.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Type of Survey (s) Geological; Geophysical (Mag S VLF EM) Township or Are* Esther and Burton Twps. ~^g,,^*
ClaimHniHer( s) Canadian Nickel Company Limited______ Copper Cliff, Ontario POM 1NO————
Survey company Canadian Nickel Company Limited______ Author of Report Robert Bell, c/o Canadian Nickel———— Address of Author Company Limited. Copper Cliff, Ont. POMCovering Dates of Survey June 1 July 31. 1983__________
(linecutting to office)
Total Miles of Line Hut 91.4 km___________________
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——————
DAYS per claim
4020
Geological.Geochemical.
20
AIRBORNE CREDITS (Special provision credits do not apply to airborne lurveyi)
Magnetometer .Electromagnetic Radiometric
June 25, 1984 STHMATTTRF.: *J#&6&S&&)Author of Report or Agent
DATE:
Res. Geol.. .Qualifications.Previous Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
(prefix) (number)
D J
TOTAL CLAIMS. 41
837 (5/79) J
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS - If more than one survey, specify data for each type of survey
Number of ststinn, 6992 (Mag); 3496 (VLF) Station interval 12.5 metre (Mag); 25 metre (VLF)Profile scale 1 cm ^ 1QO (EM)_^________
.Number of Readings 6992 (Mag); 3496 (VLFj
.Line sparing 100 metre_____^__
Contour interval 200 gammas
ca z o•*s
Instrument Scintrex MF-2 FluxgateAccuracy — Scale constant — ^___
Diurnal correction method ___ " "2 hoursBase Station check-in interval (hours).
Base Station location and value 10.000N - 6400E
O
Ss
W Ja
Instrument Crone "Radem" VLF
Coil configuration Coil separation ——
Accuracy —————
Method:
Vertical LoopVariable
10
Frequency.
(^p Fixed transmitter CH Shoot back 17.8 KHz________NAA Cutler, Maine
D In line D Parallel line
Parameters measured.(specify V.L.F. station)
dip angle of resultant field, out of phase, horizontal component offield strength
Instrument
Scale constantGRAVITY Corrections made
Racp ctatinn value anrl Inratinn
Elevation accuracy.
[NDUCED POLARIZATION
Method D Time DomainParameters — On time
SM Off timpH > — TVlay timpH c/i — Integration time
W Power
Electrode array ———————————————————
Electrode soacine . . . . —————————————————
CH Frequency Domain FrequencyRange
Type of electrode
SELF POTENTIAL
Instrument_________________________________________ Range.Survey Method——-——-——-————-^——-————--^——.——^^—-.-——————
Corrections made.
RADIOMETRIC
Instrument.Values measured.Energy windows (levels)—^——^——-—-^^—^———————^—————-———^^——.
Height of instrument______________________________Background Count.Size of detector———-^^^————-———-—————-—^—^————....—,————..^——.
Overburden —^^—^^——————.^^^^^—-—.———————^^^^—.————————(type, depth — include outcrop map)
OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)\' Type 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 Sparing 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.
ANALYTICAL METHODSValues expressed in: per cent O
p. p. m. Dp. p. b. D
Cu, Pb,
Others—
Zn, Ni, Co, Ag, Mo, As.-(circle)
Field Analysis (.Extraction Method. Analytical Method- Reagents Used——
Field Laboratory AnalysisNo. .—————————
SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)
Mesh size of fraction used for analysis———.
Extraction Method. Analytical Method. Reagents Used—™
Commercial Laboratory (- Name of Laboratory— Extraction Method~—— Analytical Method __ Reagents Used -———.
.tests)
.testsL
-tests)
General. General
SCHEDULE "A"
473385558456558457558458558459558460558461558462558463558464558465558466558467558468558469558470558471
P 558472 P 558473 P 558474 P 558475
Mining Claims Traversed
P 558476 P 629911 P 629912 P 648044 P 648045 P 648046 P 648047 P 648048 P 648153 P 648154 P 648155648198648199648200648283648284648285648286648362648363
Total Claims s 4 1
ario
Ministry ofNaturalResources
1984 08 27 Your File: 273-84 Our File: 2.7004
Aj
Mr. Bruce W. HanleyMining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7
Dear Sir:
Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at 416/965-4888.
s sincerely,
ttor Land Management Branch
Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3
Hurst:mc
Encls.
cc: Canadian Nickel Company Limited Copper Cliff, Ontario POM l NO
cc: Mr. G.H. FergusonMining S Lands Commissioner Toronto, Ontario
845
Ministry ofNaturalResources
Ontario
Notice of Intent
for Technical Reports
1984 08 27
2.7004/273-84
An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.
If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.
If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.
If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.
846 (82/5)
1984 08 06 Your File: 273 Our File: 2.7004
Mr, Bruce HanleyMining RecorderMinistry of Natural Resources60 Wilson AvenueT1mra1ns, OntarioP4N 2S7
Dear Sir:
We have received reports and maps for a Geophysical (Electromagnetic fi Magnetometer) and a Geological Survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims P 473365 et al 1n the Townships of Esther 8 Benton.
This material will be examined and assessed and a statement of assessment work credits will be Issued.
Yours sincerely,
S.E. YundtDirectorLand Management Branch
Whitney Block, Room 6643Queen's ParkToronto, OntarioM7A 1W3Phone: (416)965-6918
A. Barr:se
cc: Canadian Nickel Co United Copper Cliff, Ontario POM 1NO Attn: Robert Bell.
r
1984 09 13 Your File: 273-84 Our File: 2.7004
Mining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 257
Dear Sir:
RE: Notice of Intent dated August 27, 1984Geophysical (Electromagnetic It Magnetometer) and Geological Survey on Mining Claims P 473385 et al 1n the Townships of Esther 4 Benton
The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.
Please Inform the recorded holder of these mining claims and so Indicate on your records.
Yours sincerely,
S.E. YundtDirectorLand Management Branch
Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-4888
S. Hurst;me
cc: Canadian Nickel Company Limited Copper Cliff, OntarioFOM lNO
cc: Mr. G.H. FergusonMining A Lands Commissioner Toronto, Ontario
Encl.
cc: Resident Geologist Timmins, Ontario
r/^jv Ministry ot Technical Assessivy r Natural .,, , . ... V2/ Resources Work CreditsOntario j**
ment file 2.7004
Date Mining Recorder'^ BeDQCt of
19840827 WorkU ^m
Recorded Holder CANADIAN NICKEL COMPANY LIMITED
Township or AreaESTHER AND BENTON TOWNSHIPS
Type of survey and number of Assessment days credit per claim
Geophysical 40 rifl ,
20
Other Hays
Section 77 (19) See "Mining Claims Attested" column
onRonlngira! t u days
Man days CD Airborne d
Special provision Q Ground C3
CD Credits have been reduced because of partial coverage of claims.
CD Credits have been reduced because of corrections to work dates and figures of applicant.
Mining Claims Assessed
P 473385 558456 to 470 inclusive 558473 to 476 inclusive 629911-12 648044 to 048 inclusive 648153-54-55 648198 to 200 inclusive 648283 to 286 inclusive 648362-63
Special credits under section 77 (16) for the following mining claims
30 DAYS ELECTROMAGNETIC 20 DAYS ELECTROMAGNETIC1 5 DAYS MAGNETOMETER 1 0 DAYS MAGNETOMETER1 5 DAYS GEOLOGY 10 DAYS GEOLOGY
P 558472 P 558471
No credits have been allowed for the following mining claims
LJ not sufficiently covered by the survey 1 — 1 Insufficient technical data filed
The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77119)—60:828 (83/6)
Canadian Nickel Company LimitedCopper Cliff * Ontario POM 1NO
REGISTERED MAIL
July 25, 1984
Mr. F. W. Matthews Supervisor, Projects Section Ministry of Natural Resources Whitney Block, Queen's Park Toronto, Ontario M7A 1X1
Dear Mr. Matthews:
Enclosed is a geological and geophysical (Mag and EM) report in duplicate, being submitted under the Special Provisions Section as assessment work on the following 41 claims located in Esther and Benton Townships, Porcupine Mining Division.
P 473385^ P 648153-155 incl.P 558456-476 incl. P 648198-200 incl.P 629911-912 P 648283-286 incl.P 648044-048 incl. P 648362-363
The report of work covering this submission was forwarded to Mr. B. Hanley in Timmins and subsequently recorded on June 27, 1984.
I trust that this will be considered satisfactory by your department.
W. V, Rodney Exploration Departmi
IM/nk
Exploration subsidiary of
INCO LIMITED
Mining Lands Section
Control Sheet
File No J? ~)OO Y
TYPE OF SURVEY GEOPHYSICAL
GEOLOGICAL
GEOCHEMICAL
EXPENDITURE
MINING LANDS COMMENTS:
P
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Dra
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by:
Ron
Jo
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n
File
Surv
ey d
ate
AU
GU
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SE
PT
1983
Dat
e dr
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. O
CT
1983
Rev
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N.T.
S41
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July
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Dro
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by!
Ron
Jo
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File
Surv
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SEPT
. 19
83
Dat
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O
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1983
Rev
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.
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Pro
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l cm
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SHEE
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Porc
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in. D
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Ben
ton/
Est
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Inst
rum
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E
V.L.
F.
Dro
wn
by
Ron
Jo
hnso
n
File
Surv
ey d
ate
SE
PT
19
83
Dat
e dr
nwn
OCT
. 19
83
Rev
ised
41 0
/9
