Ontario Geological Survey
Permanent Link to this Record:
MDI52O06SE00027
Record Name(s) | Esker Zone - 1990, Kawashe Lake # 22 - 1990 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Prospect |
Date Created | 1990-Nov-28 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Kawashe Lake Area
Latitude: 51° 20' 40.12" Longitude: -91° 4' 23.39"
UTM Zone: 15 Easting: 634196.081 Northing: 5689895.852 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O06SE
Point Location Description: Diamond drill holes
Location Method: Conversion from MDI
Access Description: The Esker Zone is located about 61 km west-southwest of Pickle Lake and about 4.75 km east-southeast of the Golden Patricia mine. The center of the zone is about 550 m northeast of the northeast shore of Muskegsagagen Lake. Access to this occurrence is best gained through the Golden Patricia mine which is serviced by an all-weather airstrip and a winter road from Pickle Lake. Appropriately equipped aircraft may land on Muskegsagagen Lake to the southwest of the occurrence.
1984: St. Joe Canada Inc. commissioned an airborne magnetometer survey over an area including the occurrence. This was followed up with a ground mag survey over an area including the occurrence. 1985: St. Joe Canada Inc. did ground mag, EM and IP surveys and diamond-drilling around the occurrence. 1986: St. Joe Canada Inc. and Geocanex Ltd. did separate airborne mag and EM surveys over areas including the occurrence. 1986: St. Joe Canada Inc. continued diamond-drilling around the occurrence. 1988: St. Joe Canada Inc. / Bond Gold Canada Inc. did additional geophysical surveys around the occurrence and did the diamond-drilling which located and defined the Esker Zone. 1989 and 1990: Bond Gold Canada Inc. did additional diamond-drilling on and around the Esker Zone.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Lake St. Joseph
Geological Age: Mesoarchean
Dec 07, 2005 (B Nelson) - The Esker Zone is two zones of gold mineralization in close proximity to each other. The first zone of gold mineralization is contained within a silicified and sulphidized portion of an iron formation horizon. The iron formation occurs in a succession of mafic metavolcanic flows. The Esker Zone occurs in a thicker portion of the iron formation and has a strike length of 60 m. A fold closure may have caused the thickening of the iron formation. Quartz-feldspar porphyry intrusives cut the mafic metavolcanic flows. The gold-bearing portion of the iron formation is typically strongly deformed. Often it is cut by blue-grey quartz veins and stringers. The principle sulphide in the zone is pyrrhotite, with pyrite, arsenopyrite and chalcopyrite as accessory sulphides. The second zone of gold mineralization is contained in a zone of biotite-carbonate alteration within the mafic metavolcanics. Locally, the zone contains a blue-grey quartz vein and / or pyrrhotite, but neither are necessary for gold to be present. It is not certain if this second zone is one entity or several erratic occurrences of gold.
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Iron Formation | Host |
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Mafic lava flow-unsubdivided | 2 | Host | ||
Mafic lava flow-unsubdivided | 3 | Near | ||
Quartz-Feldspar Porphyry | 4 | Quartz-Feldspar Porphyry | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
2 | Gold | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore | ||||
5 | Arsenopyrite | Economic | Ore | ||||
Quartz | Alteration | Silicification | 1 | ||||
Unspecified | Alteration | Sulphidation | 2 | ||||
Carbonate | Alteration | Unknown | 3 | ||||
Biotite | Alteration | Unknown | 4 |
Dec 07, 2005 (B Nelson) - Some of the better assay results from the Esker Zone are: ME-88-08: In iron formation, 3.18 g/t Au over 12.3 m, including 3.83 g/t Au over 9.6 m and 5.67 g/t Au over 5.22 m. ME-88-06: Blue-grey quartz vein in mafic metavolcanic, 24.0 g/t Au over 0.3 m. ME-89-15: Biotite-carbonate alteration zone, 2.26 g/t Au over 3.1 m.
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Sheared |
Map - Cat River-Kawinogans Lake area, District of Kenora (Patricia Portion), Ontario
Publication Number: ARM44F Scale: 1:126,720 Date: 1997
Author: Harding W.D.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology of the Cat River-Kawinogans Lake area
Publication Number: ARV44-06.002 Date: 1997
Author: Harding W.D.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Cat Lake-Pickle Lake, geological compilation series, Kenora and Thunder Bay districts
Publication Number: M2218 Scale: 1:253,440 Date: 1976
Author: Sage R.P., Breaks F.W., Troup W.R.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Geology of the Cat Lake-Pickle Lake area, districts of Kenora and Thunder Bay
Publication Number: R207 Date: 1982
Author: Sage R.P., Breaks F.W.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian geology, Muskegsagagen-Bancroft lakes area, District of Kenora (Patricia Portion)
Publication Number: M2507 Scale: 1:50,000 Date: 1986
Author: Stott G.M., Wilson A.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral Deposits of the Central Portion of Uchi Subprovince, Volume 1, Meen Lake to Kesagiminnis Lake Portion
Publication Number: OFR5869 Page: 235 Date: 1993
Author: Seim G.Wm.
Publisher Name: Ontario Geological Survey
Location:
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