richardson lk proj€¦ · title: richardson lk proj author: w troop subject: assaying and analyses...
TRANSCRIPT
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52G03SEe«01 2 .14392 R ICHARDSON010
THE RICHARDSON LAKE PROJECT
(LAT. 49%05'N, LONG. 91%00'W)
ALCANEX LTD. - TORONTO
Report By: W. R. Troup Date : Dec 1, 1991
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52G«3SE0eei 2.14392 RICHARDSON
TABLE OF CONTENTSPage
1 .0 Summa ry ......................................... i
2.0 J nt roduct i on .................................... 1
3 . 0 Locald on And Access ............................. 1
4.0 Geo]ogy ......................................... 1
1>. 0 Hi story Of KxpJ oration .......................... 4
6.0 Summary Of Work Completed 1991 .................. 5
7.0 Cone]usions And Recommendations ................. 6
8.0 Certificate Of Qualifications ................... 7
8 . 0 P.3 b] J ocjraphy .................................... 8
LIST OF FIGURES
(1 ) Local: i on Map .................................... 2
(2) C1 a j H Sketch .................................... 3
LIST OF APPENDICES
A-] Rock Sample Descriptions
A-2 Assay Listings
A-3 Compilation Map, Geology, Sample Locations Etc. Reg i o naJ Ma p Scale 1: 35,840 North Claim Block, 1: 4,158
010C
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SUMMARY
The Richardson Lake Project Area is located in the Atikoken- Riehardson Lake greenstone Belt of the Canadian Prccambrian Shield, Gargoyle Lake 3 s located in the centre of the projecta rea .
Previous goId and
exploration has resulted in the discovery base metal occurrences throughout the region.
of several
Alcanex Ltd., A private president, acquired an option area in 1990.
company of on 49 claims
which the writer is in the Richardson Lake
The current prospecting venture was initiated in the summer of 1991, in an attempt to locate target areas capable of hosting gold and base metal deposits, both within and surrounding theexisting claim group.
The area is underlain by an eastwest trending sequence of mafic and fel sic voJcanics and interbedded sediments. Encouraging base metal values of up to 4.3% Zn. and .2% Cu. were obtained from a chert-argil 1ite horizon asociated with an A.E.M, anomaly in the north central portion of the area. Geocheroically anomalous copper values were obtained from elsewhere on the property.
An extensive overburden cover prevented the surface explanation of many priority A.E.M anomalies in the area. Humus geochemical sampling was applied to one such anomaly and, although not conclusive, produced encouraging values in gold and zinc.
Ground geophysics and diamond .drilling will be required to evaluate the base metal potential of select A.E.M. anomalies present in the overburden covered portions of the area.
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INTRODUCTION
In January 1.990, the government" data was reviewed (i.e. assessment files, government geology, A.L.M. data). Based on the re suits of this con pi ] at ion , and the writers personal knowledge of the- area, specific target areas were seleeted for field ex ami na t ion .
In August 1991, the writer traversed key areas, napped the geology and attempted to locate and sample priority A.E.M. anomalies.
Twenty-four rock samples and 16 humus samples were submitted to X-Ray Assay Laboratories for analyses. All samples were analysed for gold and base metals.
LOCATION AND ACCESS
The Richardson Lake project area is located 90 miles northwest of Thunder Bay. The Trans-Canada Highway and Canadian Pacific Rail Line cross the eastern extention of the belt and pass within eight miles of the area of current interest. Recent logging operations have brought road access to Gargoyle Lake located in the centre of the area.
GEOLOGY
The Richardson Lake Greenstone Belt is part of the Archean Wabigoon Greenstone Belt of the Superior Province. Massive to foliated trondhjernite and granodiorite border the volcanics and sediments of the belt.
Mafic to intermediate volcanics constitute a large portion of the area. In the Gargoyle Lake and Upper Scotch Lake areas narrow felsic horizons are considered to represent felsic tuff horizons and or felsite dikes. The mafic volcanics of the region typically contain horizons of metasediments. A serpentinite body at the east end of Gargoyle Lake is aligned in an east-west direction conformable with stratigraphy. Formational E.M. and Mag anomalies in the area indicate the presence of sulphide facies iron formation.
The terrain is gently rolling with a few hills up to 250 feet high. Bedrock is extensively covered and the stronger ( 1 ect ronagnet. i c conductors of the area are frequently obscurred.
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Richardson. A '-!-•' % \ ff'-Vi
Property
Figure 1
LOCATION MAP OF RICHARDSON LAKE PROPE-RTY
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RICHARDSON LAK€ CLAIMS
THUNDER BAY MINING DISTRICT
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HISTORY OF EXPLORATION
The first nevol opiviont (ODM Annual
syst s'-nat ie Dep,:i ; i.) icnt report, 6 9) .
napping of the a re-a was by C.P.R.'s n 19H2, followed bv H. Wool vert on an .1900
GoJd was
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In areas t h.'iL had not bi'on cut over, remnants of the old Shell grid were .Kic.it i;--d . i\, -i mant s of tin? oJd Shell grid are the most recent i nc.i i rat. ions of explurat. i on in the area. Preliminary sampling u>'f rusty ankerite rich maf ic \'o K-,i in c-s northeast uf Gargoyle Lake indicated a favourable. 'icKl envj ronnent.
In 1990, theAleanex Ltd.11, 19S9, ro March 1990,work .
writer purehoit and
49 mineral claims in the area for ie claims have recording dates ranging from Dec.
are currently on extent ion pending
SUMMARY OF WORK COMPLETED 1991
In 1991, reconnaissance geological napping and sampling was carried out over the Gargoyle Lake area in order to assess the economic potential. An attempt was roade to locate outcrop proxir.icil to or along strike from priority A.E.M. anomalies.
As was previously indicated by Shell many of the conductors are overburden covered and will be best evaluated by diamond drilling. Overburden cover is thin throughout the area and basal till sampling might prove an effective means of screening priority A.E.M anomalies in advance of diamond drilling.
Prospecting along strike from known A.E.M. anomalies produced very encouraging results for the area north of Gargoyle Lake. Sheared graphitic argillite and chert was located in an old trench located along strike to the west of a strong A.E.M anomaly and parallel to a second isolated conductor of interest. Chip sampling across the old trench returned anomalous values in copper (0.15%/1.5ft.), and zinc (4.3%/0.5ft.). Zinc mineralization occurrs within a 0.5 foot thick conformable, dark grey quartz vein within the argillite unit. Two priority A.E.M anomalies in this area are not exposed and their cause remains unknown.
Humus sampling over a separate anomaly immediately north of Gargoyle Lake returned geochertical ly anomalous gold values of 9 ppb gold where the background is < 2.4 ppb.. Geochemically anomalous values in Zn (240 ppm) and Ba (600ppm) were obtained where the mean values for these elements were Zn (28ppm) and BaU33ppm). While the significance of this one line humus survey is of questionable merit, the observed range in values is e o n s i d e r e d e n e o u r a
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CON-CLUS] ONS AM') RfCOMMFN'DAT ! O\S
Preliminary
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CERTIFICATE OF QUALIFICATIONS
I, William, R. Troup, of Mississauga, Ontario hereby certify and declare the following:
1. I am a Consulting Geologist and President of Alcanex Ltd., a service company providing geological services and project management to the mineral exploration industry.
2. I graduated from the University of Waterloo with an MSc. degree in Geology in 1975.
3. I have been practicing my profession for the past 18 years.
4. I am a fellow in the Geological Association of Canada.
5. I personally carried out the geological mappingand geochemical sampling described in this report.
6. The report is based on my field work and a review of government geological and geophysical maps and reports for the area, and additional data available in the Ontario Gov"t assessment files.
Toronto, Ontario William R. Troup November 5, 1991 Consulting Geologist
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BIBLIOGRAPHY
1). Woolverton, R.S. 1960; GEOLOGY OF THE LUMBY LAKE AREA, Ontario Department Of Mines Vol. 69.
2). Ontario Geological Survey 1980; AIRBORNE ELECTROMAGNETICSJURVEY_AND TOTAL INTENSITY MAGNETIC SURVEY, ATIKOKAN-MINE
CENTRE^AREA_," EASTERN"PART , DISTRICTS OF KENORA AND THUNDER BAY. '
3). Ontario Geological Survey 1981; THUNDER BAY DATA SERIES PRELIMINARY MAP P.2152, REDPAINT LAKE AREA.
4). Ontario Ministry Of Natural Resources, Assessment Files.
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APPENDIX A-l
ROCK SAMPLE LOCATIONS
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SPL # Tvr-i;-:
17963 cj )
17964 grab
17965 O.bn chip
17966 grab
17967 bJdr
17968 0.6m ch
17969 grab
17970 0.5m ch
17971 0.7m ch
17972 1.2m ch
17973 0.2m ch
.1 7974 0.5m ch
J 7975 0.05rn ch
"(H'K S,WLi' DESCRIPTTOK'S
LOCATION
-XIV of Gargoyle Lk .
-15 ft.. S. of 17963
-1 '2 mile E.NE of 17963/64
-as per 17965
-50 m. E. of 17966
DESCRIPTION
-qtz-py 3 ining fracture in felsite dyke
-graph, py. filled fracture in felsite dyke-fracture trends 90 degs.
-sheared rnetaseds, 1- 3 % d i s s. py
-3.0 cm q.v.; tr. py. x-cutting, trend 170 deg., dip 80 deg west
-sh metased., 5-8% py as laminations
-8m S.E. of 17965/66
-loc'n as for 17968
-30m S.E. of 17968/69 S. end of old trench
-N from 17970
-N from 17971
-N from 17972
-N from 17973
-N from 17974
-sh graph-arg.; 1-4% diss py
-10 cm q.v. within sh.;4-6% diss py
-graph., py, and argillite with 8% py as diss & lam's
-graph arg. with minor veinlets of grey-black qtz
-graph-arg. + py
-black q.c. w incl of arg. and 5% py
-grey q.v. w minor py on fractures
-friable graph arg. w 1-3% py
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17976 (i. i;i . li
17977 hi el--.
17978 hi dr.
17979 b I dr.
17980 hi dr.
17981 bldr.
17982 1.0m eh
17983 grab
17984 grab
17985 0.3m ch
17986 1.0m ch
17987 2. OIT. ch
17988 grab
17989 1.0m ch
17990 bldr.
from 1707"
-.' 2 II i ](' IVM'r.V t.
20OKI S of J7976
- SF end of ( 'j a rgoy 1 e
-•3f>0n south of east t i p of G a r g o y1e Lk.
-S.E. shore of
-S. shore of large bay, E. end of Gargoyle Lake
-near A.E.M anomaly
-S.E. Gargoyle Lk.
-5 ro S. of 17983
-S. shore Gargoyle
-N. end of peninsula,S. shore Gargoyle L.
-3m N of 17986
-N.N. of Gargoyle Lk., east of Mil.ten Lk.
-S.W. of Gargoyle Lk., near A.E.M.
-as for 17989
- -, i.l 'd felsJc vole.? or fr-1 si l.r- dyke'';1-3 PY
g v,.i j.'l'i. ,j L'cj. , 20 : py
- n i e t a - g r e y vc a c k e , 1-4 diss. py, possible Cu staining
-banded py and arg.
-peridotite? serpentinite? v\ magnetite
-qtz-carb vein
-chert-mag-sulph I.F.
-sh. mafic vole, tuff argillaceous, 5-8% py
-sh'd and silicified argillite, 20 % py
-qtz-ank vein in sh mafic vole., 1-2% diss py
-graph-arg w 20-30% py as laminations
-sh'd chert-arg w 1- 15% py + 3% mag.
-carb'd shear in m.v.
-mag, po, py, chertI.F.
-angular, chert-mag py Mposs Cu stain?)
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17991 gr,-u-
17992 grab
17993 grab
17994 grab
17995 grab
-I'M road (JO n i j
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APPENDIX A-2
ASSAY LISTINGS
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1 111
VRAM ^ "r*rtl «^«« u,«wi»r%iwi*.i.w| V^ §\ r\ 1^ I A DIVISION or SGS SUPERVISION SERVICES INC.1 ^L ^" " 1885 LESLIE STREET DON MILLS. ONTARIO H3B 3J4 CANADA
r̂
TO: WILLIAM
TEL: (416)445-5755 TELEX: 06-986947 TAX: (416)445-4152
OERTX-FXCATE OF AJST AJL, Y S X S
REPORT 16884
R. TROUP1365 CLARKSON ROAD WEST CUSTOMER No. 1482
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MISSISSAUGA, ONTARIOL5J 2W6
REF.
DATE SUBMITTED4-Sep-91
FILE 10739- Total Pages 3*»
16 HUMUS Proj. RICHARDSON LK
AU PPB
NA PPM
CA X
SC PPM
CR PPM
FE %
CO PPM
NI PPM
ZN PPM
AS PPM
SE PPM
BR PPM
RB PPM
MO PPM
*** UNLESS
METHOD DETECTION LIMIT METHOD DETECTION LIMIT
NA 1. AG PPM NA 2.
NA 100. CD PPM NA 2.
NA .5 SB PPM NA .1
NA .2 BA PPM NA 100.
NA 1. LA PPM ^ _ NA 1.
NA .OS CE PPM NA 1.
NA 1. SM PPM NA .1
NA 20. TA PPM NA .5
NA 20. W PPM NA 1.
NA 1. IR PPB NA 10.
NA 2. HG PPM NA .5
NA 1. TH PPM NA .5
NA 20. U PPM NA .1
NA .5
INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 90 DAYS ***AND REJECTS 30 DAYS FROM DATE OF THIS REPORT
nhTT? nK_/">r"T> Q i r>i?D'PTT?TTH'n wv \ \/&*-''^ — -
Philip Doctor, Laboratory Manager
Member of th" SGS Group ( Soci6t6 G6n6rale de Surveillance)
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05-OCT-91 REPORT 16884 REF.F1LE 10739- PAGE 1 OF 3
SAMPLE AU PPB NA PPM CA X SC PPM CR PPM FE X CO PPM NI PPM ZN PPM
G1-0+OONG1-0+10NG1-0+20MG1 -0+30NG1-0+40N
932
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05-OCT-91 REPORT 16884 REF.FILE 10739- PAGE 2 OF 3
1111111
SAMPLE
G1 -0+OONG1-0+10NG1-0+20N G1-0+30NG1-0+40N
G1-0+50N G1 -0+60NG1-0+70NG1-0+80NG1-0+90N
61-1+10MG1-1+20NG1-1+30N G1-1+40NG1-1+50N
G1-1+60N
AS PPM
233 22
2 2222
142 23
4
SE PPM
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:RAL05-OCT-91 REPORT 16884 REF.FILE 10739- PACE 3 OF 3
i i i i i i i i i i i i i i i i i
SAMPLE LA PPM CE PPM SI1 PPM TA PPM W PPM IR PPB HG PPM TH PPM U PPM
G1-0+OONG1-0+10NG1-0+20NG1-0+30NG1-0+40N
G1-0+50NG1-0+60NG1-0+70NG1-0+80NG1-0+90N
G1-1+10NG1-1+20NG1-1+30NG1-1+40NG1-1+50N
57
1295
42353
1223212019
71119159
73474
1735272127
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I I I I I I I I I I I I I I I I I I I
IgRALI A~r\M I MOO/A i i-rvDV/rtM iA DIVISION OF SGS SUPERVISION SERVICES INC.1885 LESLIE STREET • DON MILLS, ONTARIO M3B 3j4 • CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE
REPORT
OF ANALYSIS
16-745
TO: WILLIAM R. TROUP1365 CLARKSON ROAD WEST MISSISSAUGA, ONTARIO L5J 2W6
REF. FILE 10741-
32 ROCKS Proj. RICHARDSON LK
CUSTOMER No. 1482
DATE SUBMITTED 3-Sep-91
Total Pages 1
AU PPB CO PPM NI PPM CU PPM ZN PPM MO PPM AG PPM CD PPM PB PPM
METHOD FADCP DCP DCP DCP DCP DCP DCP DCP DCP
DETECTION LIMIT 1. 1. 1..5.5
1..5
1.2.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 90 DAYS *** AND REJECTS 30 DAYS FROM DATE OF THIS REPORT
DATE 21-SEP-91 CERTIFIED BY .Philip Boctor, Laboratory Manager
Member of the SGS Group
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21-SEP-91 REPORT 16745 REF.FILE 10741- PAGE 1 OF 1
111111111111111
SAMPLE
179631796417965 1796617967
17968 17969179701797117972
179731797417975 1797617977
17978 17979179801798117982
179831798417985 1798617987
17988 17989179901799117992
179931799417995
AU PPB
50SMP MISSSMP MISS
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APPENDIX A-3
COMPILATION MAP
GEOLOGY, SAMPLE LOCATIONS ETC,
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Ontario 2.14392 RICHARDSON 900
Ministry ofNorthern Developmentand Mines
Ministere duDeveloppement du Nord et des Mines
Mining Lands Branch Geoscience Approvals Section 159 Cedar Street, 4th Floor SUDBURY, Ontario P3E 6A5
Toll Free: Telephone: Fax:
1-800-465-3880 (705) 670-7264 (705) 670-7262
Mining RecorderMinistry of Northern Development Your File: W. 9140. 5080and Mines Our File: 2. 14392435 James Street SouthThunder Bay, OntarioP7C 5G6
February 24, 1992
Dear Sir:
SUBJECT: APPROVAL OF ASSESSMENT WORK SUBMITTED ON MINING CLAIMS TB. 1044057 ET AL. IN RICHARDSON LAKE AREA.
The assessment work credits for the geochemical analyses work, under Section 17 Mining Act Regulations, submitted on the above work report has been approved as of the February 24, 1992. You have been awarded the total value of credit recorded on the work report.
Please indicate this approval on your records.
Yours sincerely,
Ron C. GashinskiSenior Manager, Mining Lands BranchMines and Minerals Divison
Enclosures:
cc: AfiSfiRRmen,t Files Office Toronto, Ontario
Resident Geologist Thunder Bay, Ontario
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•Ministry ofNorthern Developmentand Mines
Ontart
Report of Work Conducted After Recording Claim
Mining Act
Transaction Numb*
Personal Information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines. Fourth Floor, 1S9 Cedar Street, Sudbury. Ontario, P3E 6A5, telephone (705) 670-7264. f . - „ ..
Instructions: • Please type or print and submit In duplicate. ••"•' ' •- *-••-•' -^ A/• Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.• A separate copy of this form must be completed for each Work Group.• Technical reports and maps must accompany this form In duplicate.• A sketch, showing the claims the work Is assigned to, must accompany this form.
Recorded Holder(s) Client No.
AddressA/
Mining Division Township/Area
Telephone No.
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