Ontario Geological Survey
Permanent Link to this Record:
MDI42A07NW00012
Record Name(s) | Cross Lake DDH Sk98-22 - 1998, Selco Occurrence - 1990, Selco DDH 67-9 - 1967 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1997-Feb-19 |
Date Last Modified | 2023-Feb-06 |
Created By | |
Revised By |
Primary Commodities: Copper, Zinc
Secondary Commodities: Gold
Township or Area: Sheraton
Latitude: 48° 26' 16.62" Longitude: -80° 46' 20.68"
UTM Zone: 17 Easting: 516832.821 Northing: 5365003.549 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A07NW
Point Location Description: Drill collarat 20+00E/10+00S on former claim L 96127
Location Method: Based on Assessment
Access Description: The site is accessible via a series of disused logging roads heading east from the Gibson Lake Road.
1966-67: Selco Exploration Co. Ltd. - 1 ddh (357 ft). 1971-73: Cominco Ltd. - airborne geophysics. 1977: Noranda Exploration Co. Ltd. - ground geophysics. 1998-99: Golden Knight Resources/Cross Lake Minerals Ltd./East West Resource Corporation/ Canadian Golden Dragon Resources Ltd. - ground geophysics, 1 ddh (257 m).
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-1339, 10 | 42A07NW0120 | 42A07NW0120 |
T-4159, 2.19367 | 42A07NE2007 | 42A07NE2007 |
T-341, 13 | 42A07NW0117 | 42A07NW0117 |
T-4208, 2.19365 | 42A07NE2010 | 42A07NE2010 |
T-4209, 2.19379 | 42A07NE2012 | 42A07NE2012 |
T-4228, 2.19447 | 42A10SE2005 | 42A10SE2005 |
T-650, 2.490 | 42A07NW0162 | 42A07NW0162 |
2.962, T-0650 | 42A07NW0115 | 42A07NW0115 |
2.698, T-0341 | 42A07NE0173 | 42A07NE0173 |
2.961, T-0650 | 42A07NW0116 | 42A07NW0116 |
2.1755, T-0650 | 42A07NW0112 | 42A07NW0112 |
2.1718, T-0650 | 42A07NW0113 | 42A07NW0113 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
Metamorphism Grade: Greenschist
Dec 07, 2005 (C Salo) - Geological mapping (Sutcliffe and Steele 1989; Gupta and Johnstone 1987; Jensen and Langford 1985; Pyke 1980, 1976; Berry 1942; McClenaghan et al. 1989, 1988, 1987; Steele 1988; Richard and McClenaghan 1985) indicates that most bedrock in the occurrence area is glacial drift covered. Bedrock consists mainly of weakly metamorphosed (greenschist or lower metamorphic grade) subaqueously deposited tholeiitic volcanic rocks and interflow sedimentary rocks of the (Archean) Kinojevis Group. The basement supracrustal rocks strike east northeast, dip steeply, face south, and occupy part of the north limb of the east striking and east plunging Blake River Synclinorium. Intrusive rocks in the area include large felsic bodies, northeast striking diabase dikes of the (Proterozoic) Abitibi and/or Preissac swarms, and generally north striking diabase dikes of the (Proterozoic according to Heaman 1989) Matachewan swarm. Several regional scale south southeast striking faults have been interpreted to occur in the area. A recent geophysical survey of Sheraton Township (OGS 1984) detected several bedrock conductors in the occurrence area.
Rock Type | Rank | Composition | Texture | Relationship | Felsic lava flow-unsubdivided | 1 | Rhyolite, Dacite | Host |
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Breccia-unsubdivided | 2 | Host | ||
Feldspar Porphyry | 3 | Feldspar | Near |
Dec 07, 2005 (A Wilson) - Diamond drilling intersected a sequence of rhyolite, rhyolitic tuff and breccia intruded by feldspar porphyry dikes. Two sections containing massive pyrite returned low gold values.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
1 | Pyrite | Economic | Gangue |
Dec 07, 2005 (A Wilson) - A 12.5 ft section of Selco's core returned an assay of 0.01 oz/t Au; a 3.9 ft section of drill core returned an assay of 0.01 oz/t Au. The best assay returned from the Cross Lake core was 1.73% Zn, 0.6% Cu over 1.3 m.
Dec 07, 2005 (C Salo) - Selco Exploration Co. diamond drill hole no. 9 is reported (assessment files, Resident Geologist's Office, Timmins) to have yielded within felsic volcanic and fragmental rocks 12.5 and 3.9 foot sections of nearly massive pyrite mineralization. Both sections assayed 0.01 ounce of gold per ton.
Mono - Mineral occurrences, deposits, and mines of the Black River-Matheson area
Publication Number: OFR5735 Page: 1700-1703 Date: 1990
Author: Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Watabeag River area, districts of Timiskaming and Cochrane
Publication Number: P1078 Scale: 1:63,360 Date: 1976
Author: Pyke D.R.
Publisher Name: Ontario Division of Mines
Location:
Part - Geology of the Langmuir-Sheraton area
Publication Number: ARV49-04 Date: 1997
Author: Berry L.G.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Precambrian Geology, Sheraton Township
Publication Number: P3387 Scale: 1:20,000 Date: 1999
Author: Vaillancourt C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Lake Abitibi Area, Abitibi Greenstone Belt
Publication Number: P3398 Scale: 1:100,000 Date: 1999
Author: Ayer J.A., Berger B.R., Trowell N.F.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of the Watabeag Lake area, districts of Cochrane and Timiskaming
Publication Number: OFR5290 Date: 1980
Author: Pyke D.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Precambrian Geology of the Watabeag Lake Area
Publication Number: OFR6042 Date: 2001
Author: Vaillancourt C.
Publisher Name: Ontario Geological Survey
Location:
Folio - Sheraton Township, District of Cochrane
Publication Number: GDIF402 Date: 1997
Author: Kirkland Lake RGO
Publisher Name: Ontario Geological Survey
Location:
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