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Permanent Link to this Record: MDI52F07NE00010

Record: MDI52F07NE00010

General

Mineral Record Identification
Record Name(s) Selby Lake - 1936
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1984-Feb-02
Date Last Modified 2022-Feb-14
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Boyer Lake Area

Latitude: 49° 25' 49.23"    Longitude: -92° 42' 58.05"

UTM Zone: 15    Easting: 520583.8   Northing: 5475335.33    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52F07NE

Point Location Description: Precise

Location Method: Conversion from MDI

Access Description: The prospect is located in claim K 919 on the eastern shore of Trafalgar Bay of Upper Manitou Lake, about 1.8 km south of Gold Rock community at the north end of Trafalgar Bay. It is 1.2 km WSW of the northern tip of Selby Lake and 40 km SSE of Dryden. (Historical File F07NE00010, SMDR#001418, Kenora Resident Geologist Office)



Exploration History

Selby Lake Mines Limited was organized in 1936 to develop a group of three claims that adjoin the Laurentian and the Big Master Mines to the south. The company was privately financed. Intensive surface work and diamond drilling had disclosed 11 quartz veins by the end of 1936. Work was concentrated on the extension of the Jubilee vein, and an ore shoot 2.7 metres wide and 97.0 metres long was reported to average 0.37 oz. Of gold per ton. In the autumn of 1937, a mining plant was installed and underground work begun. A two compartment shaft was sunk to 76.2 metres with levels at 125 ft. and 250 ft. Drifting was carried out on the 250 ft. level. /the results of this work was probably not encouraging since the mining plant was moved to the Big Master property in 1939. The assets of Selby Lake Mines Ltd., were taken over by Kenwest Gold Mines, Ltd., and operations thereafter were confined to the Big Master property. (Historical File F07NE00010, EMR#502600, Kenora Resident Geologist Office)


Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Western Wabigoon

Belt: Eagle-Wabigoon-Manitou

Geological Age: Precambrian  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Basalt Adjacent
Mylonite/Fault Gouge/Pseudotachylite 2 Shear Zone Contains
Vein 3 Contains

Lithology Comments

Feb 24, 2010 (C Ravnaas) - Early Precambrian greenstones, contain horizons of porphyritic lavas which occur locally in the flows and may be traced for considerable distances along the strike. A narrow band of agglomerate and tuff occurs along the shore line of Upper Manitou Lake. The lavas have been intruded by felsite dykes. These rock assemblages belong to Superior Structural Province. A number of NE - striking quartz veins were found. They are mostly quartz lens located along zones of shearing in the volcanics. The main vein, near the lake shore on claim K 919, lies along a sheared zone that follows the contact between a felsite dike and metabasalt. The sheared zone was exposed in trenches for a distance of 135 m, attaining a width of 1.6 - 2.4 m. It contains quartz lenses and stringers banded by graphite and chlorite schist. The vein material ranges from a few cm to about 2.4 m. An ore shoot 2.7 m wide and 97 m long was reported to average 12.7 g/ t (0.37 oz/ton ) Au. (Historical File F07NE00010, SMDR#001418, Kenora Resident Geologist Office)




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GoldEconomicOre

Mineralization Comments

Feb 24, 2010 (C Ravnaas) - Resource of the E zone is 529,650 tons of 0.103 opt au, this is indicated and inferred from drilling, from AF 52F/07NEYY-1 Canamerica Precious Metal Inc. Selby Lake Mines Limited was organized in 1936 to develop a group of three claims that adjoin the Laurentian and the Big Master Mines to the south. The company was privately financed. Intensive surface work and diamond drilling had disclosed 11 quartz veins by the end of 1936. Work was concentrated on the extension of the Jubilee vein, and an ore shoot 2.7 metres wide and 97.0 metres long was reported to average 0.37 oz. Of gold per ton. In the autumn of 1937, a mining plant was installed and underground work begun. A two compartment shaft was sunk to 76.2 metres with levels at 125 ft. and 250 ft. Drifting was carried out on the 250 ft. level. /the results of this work was probably not encouraging since the mining plant was moved to the Big Master property in 1939. The assets of Selby Lake Mines Ltd., were taken over by Kenwest Gold Mines, Ltd., and operations thereafter were confined to the Big Master property. (Historical File F07NE00010, EMR#502600, Kenora Resident Geologist Office) Early Precambrian greenstones, contain horizons of porphyritic lavas which occur locally in the flows and may be traced for considerable distances along the strike. A narrow band of agglomerate and tuff occurs along the shore line of Upper Manitou Lake. The lavas have been intruded by felsite dykes. These rock assemblages belong to Superior Structural Province. A number of NE - striking quartz veins were found. They are mostly quartz lens located along zones of shearing in the volcanics. The main vein, near the lake shore on claim K 919, lies along a sheared zone that follows the contact between a felsite dike and metabasalt. The sheared zone was exposed in trenches for a distance of 135 m, attaining a width of 1.6 - 2.4 m. It contains quartz lenses and stringers banded by graphite and chlorite schist. The vein material ranges from a few cm to about 2.4 m. An ore shoot 2.7 m wide and 97 m long was reported to average 12.7 g/ t (0.37 oz/ton ) Au. (Historical File F07NE00010, SMDR#001418, Kenora Resident Geologist Office)



Mineral Record Details

References

Part - Some gold deposits near Goldrock, Upper Manitou Lake

Publication Number: ARV47-06.001 Scale:     Date: 1997

Author: Thomson J.E.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay

Publication Number: MDC013 Scale:     Date: 1971

Author: Ferguson S.A., Groen H.A., Haynes R.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Mono - Geology of the Boyer Lake-Meggisi Lake area, District of Kenora

Publication Number: OFR5263 Scale:     Date: 1979

Author: Blackburn C.E.

Publisher Name: Ontario Geological Survey

Location:


Mono - Feasibility of small scale gold mining in northwestern Ontario (parts of the districts of Kenora, Rainy River, and Thunder Bay), volume 1, text, volume 2, appendices

Publication Number: OFR5332 Scale:     Date: 1981

Author: Neilson J.N., Bray R.C.E.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of the Boyer Lake-Meggisi Lake area, District of Kenora

Publication Number: R202 Scale:     Date: 1981

Author: Blackburn C.E.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office