Ontario Geological Survey
Permanent Link to this Record:
MDI52E11NE00067
Record Name(s) | Electrum Prospect W Zone - 1983, San Antonio (Fault Zone) - 1983, West Zone - 1983 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1983-Dec-20 |
Date Last Modified | 2022-Mar-02 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper
Township or Area: Ewart
Latitude: 49° 42' 41.48" Longitude: -95° 7' 2.23"
UTM Zone: 15 Easting: 347360 Northing: 5508708.99 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E11NE
Point Location Description: AFRI 52E11NE9222 p. 8
Location Method: Conversion from MDI
1930: Gold was discovered in the High Lake area by C. Alcock. 1953: San Antonio Gold Mines Ltd. explored and drilled 24 holes across the property. 1960: Electrum Lake Gold Mines Ltd. drilled 70 holes across the property (11 holes totalling 1399 ft in the W Zone) and performed geological mapping, magnetic and EM surveys. 1965-66: Mag and IP surveys by Steep Iron Mines Ltd. 1983: Barrier Reef Resources Ltd. optioned the property and conducted geological mapping, geochemical soil sampling, magnetometer and VLF electromagnetic surveys. 1984: Barrier assigned its rights in the High Lake Property to a subsidiary company Francis Resources Ltd. 1985: Francis Resources was merged with Northcal Resources Ltd. to form Calnor Resources Ltd. 1986: Calnor Resources Ltd. drilled 22 DDH totalling 7594 ft. 1987: Laramide Service Corp. conducted a trenching, mapping and sampling program. 2006: mining lease owned by Canadian Star Minerals Ltd. 2011: Canadian Star transferred the adjacent claims to International Millennium Mining Corp.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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63.5114 | 52E11NE9032 | 52E11NE9032 |
63.1996 | 52E11NE9069 | 52E11NE9069 |
33 | 52E11NE9222 | 52E11NE9222 |
Province: Superior
Subprovince: Wabigoon
Belt: Lake of the Woods
Geological Age: Archean
Mar 10, 2015 (C Ravnaas) - The area is underlain by the High Lake porphyritic granodioritie stock, which intrudes Archean mafic metavolcanic rocks. The stock has been interpreted to be two intrusions (1965, Colvine 1979).
Rock Type | Rank | Composition | Texture | Relationship | Mylonite/Fault Gouge/Pseudotachylite | 1 | Shear Zone | Contains |
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Vein | 2 | Host | ||
Granodiorite | 3 | Porphyritic | Contains |
Mar 10, 2015 (Therese Pettigrew) - The High Lake stock is generally referred to as a porphyritic granodiorite. Typically this rock is grey weathering and massive, containing about 60% plagioclase, 30% quartz and up to 10% biotite. Greyish quartz-eyes and coarse, euhedral microcline crystals (up to 4 cm long) are frequently present (AFRI 52E11NE9222).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore | ||||
5 | Tourmaline | Economic | Ore | ||||
6 | Plagioclase | Economic | Gangue | ||||
7 | Quartz | Economic | Gangue | ||||
8 | Biotite | Economic | Gangue |
Mar 10, 2015 (C Ravnaas) - At the W zone, visible gold can be found on surface in a number of places, especially associated with pyrite-bearing, quartz-tourmaline veins, and had also been reported in drill cores (Davies and Smith, 1988).GRADE: HIGHEST ASSAY - 0.04 OPT AU + 0.06% CU.
Mar 10, 2015 (Therese Pettigrew) - Gold is found in zones of shearing within clean, uncontaminated High Lake granodiorite. It is associated with pyrite-filled fractures and with pyrite-bearing quartz tourmaline veins (AFRI 52E11NE9222). The mineralization occurs within highly sheared and silicified porphyry with lenses and irregular masses of vein quartz accompanied by minor pyrite, black tourmaline and carbonate. Visible gold is reported in some of the old trenches. The shearing strikes at the regional trend of N60E, but it is offset by other shears striking N10E to N30E with the result that the overall trend of the mineralized zone is N35E. Unlike the other zones on the property, the W Zone shows reasonable continuity and it has been traced by trenching over a strike length of over 700 feet. Samples collected from trenches assayed 0.04 opt Au over 2.58 feet in TR-8, 0.12 opt Au over 6.0 feet in TR-6 and 0.39 opt au over 5.5 feet in TR-7. A total of 56 samples were taken from 17 trenches. Individual samples ranged from trace to a maximum of 0.66 opt Au over a width of 2.5 ft in TR-7 (AFRI 52E11NE9032).
Rank | Classification |
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1 | Lode (Gold) |
1 | Vein |
Rank | Characteristic |
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1 | Sheared |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 214 | 3 | 26 | 35 |
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
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Electrum W Zone | 1987 | Unclassified | 12200 | AFRI 52E11NE9032, p. 21 | average width of 9.50 feet using a tonnage factor of 11.50 cubic feet per ton | Gold 0.16 Ounce per Ton |
Electrum A, B, C, P, R and W Zones | 1987 | Unclassified | 100005 | AFRI 52E11NE9032, p. 21 | average width of 8.73 feet | Gold 0.33 Ounce per Ton |
MonoMap - Geology of High Lake-Rush Bay area, District of Kenora
Publication Number: R041 Scale: Date: 1997
Author: Davies J.C.
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 - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River
Publication Number: MDC016 Scale: Date: 1976
Author: Beard R.C., Garratt G.L.
Publisher Name: Ontario Division of Mines
Location:
Map - Ewart-Forgie area, Kenora District
Publication Number: M2069 Scale: 1:31,680 Date: 1997
Author: Davies J.C.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Precambrian Geology of the Lake of the Woods Area-North Sheet
Publication Number: P2675 Scale: 1:50,000 Date: 2009
Author: Ayer J.A.
Publisher Name: Ontario Geological Survey
Location:
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