Ontario Geological Survey
Permanent Link to this Record:
MDI52E11NE00075
| Record Name(s) | Electrum (P Zone) - 1953, Electrum (Fault Zones) - 1953, High Lake Property - 1986 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Prospect |
| Date Created | 2002-Sep-11 |
| Date Last Modified | 2022-May-17 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Ewart
Latitude: 49° 42' 48.98" Longitude: -95° 6' 38.28"
UTM Zone: 15 Easting: 347846 Northing: 5508927 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E11NE
Point Location Description: Au symbol on west boundary of leased claim K20695 on map 2069 (Davies 1965), AFRI 52E11NE9222 p. 8
Location Method: Conversion from MDI
Access Description: The occurence can be accessed by driving 2.8km south from the intersection of the Shoal Lake Road and Highway 17 to the High Lake Road. Take the High Lake Road east to the gate. The prospect is located near the west boundary of claim K20695 approcimately 1km southwest of west end of Electrum Lake and 1.9km south of Baubee Lake.
1930: Gold was discovered in the High Lake area by C. Alcock. 1953: Examined by San Antonio Gold Mines Ltd. Five holes drilled in the fault zone (P zone). 1960: fourteen holes drilled on the P zone by Electrum Lake Gold Mines Ltd. Electrum also 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 (1 DDH totalling 500 ft on the P Zone). 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 |
|---|---|---|
| 63.5114 | 52E11NE9032 | 52E11NE9032 |
| 63.1996 | 52E11NE9069 | 52E11NE9069 |
| 33 | 52E11NE9222 | 52E11NE9222 |
Province: Superior
Subprovince: Wabigoon
Belt: Lake of the Woods
Geological Age: Archean Geochronological Age: 2.728 GA Geochron. Age Ref.: SMITH 1987
Metamorphism Type: Contact
Metamorphism Grade: Amphibolite
Dec 07, 2005 (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). The P zone is close to a prominent linear feature, which trends about 065. (Davies and Smith 1988) Davies (1965, p32) states, Visible gold shears along the north side of this lineation suggested that the linear feature may be a fault zone, which acted as a favourable structure for mineralizing solutions.
| Rock Type | Rank | Composition | Texture | Relationship | Mylonite/Fault Gouge/Pseudotachylite | 1 | Shear Zone | Contains | Host |
|---|---|---|---|---|
| Vein | 2 | Host | ||
| Granodiorite | 3 | Porphyritic | Contains |
Dec 07, 2005 (C Ravnaas) - Visible gold is associated with sheared quartz-feldspar porphyry. There are no strong shears, but more fractures. Thin quartz veins, in places containing tourmalinem, are also more abundant in the highly altered rock (Davies 1965).
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 |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Pyrite | Economic | Ore | ||||
| 3 | Tourmaline | Economic | Ore | ||||
| 4 | Plagioclase | Economic | Gangue | ||||
| 5 | Quartz | Economic | Gangue | ||||
| 6 | Biotite | Economic | Gangue | ||||
| Hematite | Alteration | Hematization | 1 | Extreme | Replacement |
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). A total of 1,924 feet was drilled by Electrum Lake Gold Mines in 14 holes, but only three holes have good mineralized intersections: E-34: 0.21 opt Au from 36.0-56.5 m; E-60: 0.117 opt Au from 131.0-146.0 m; E-63: 0.674 opt Au from 134-146.5 m. These three intersections are on three adjacent sections and do not line up, likely indicating en echelon zones. Assuming that the mineralization extends for 60 feet along dip and halfway to adjacent sections there are 10,000 tons at 0.29 opt Au with an average width of 12.96 feet using a tonnage factor of 11.50 cubic feet per ton (AFRI 52E11NE9032).
Dec 07, 2005 (C Ravnaas) - Iron oxide stains is present throughout most of the rocks, giving it a red to reddish-brown colour. Sulphides (pyrite and some chalcopyrite) are present on fractures surfaces, but in more strongly hematized portions sulphides are disseminated. Where the porphyry is stained, pyrite is less abundant, and large feldspar phenocrysts are typically white or partially pink. Gold is clearly associated with the more highly altered porphyry.
| Rank | Classification |
|---|---|
| 1 | Lode (Gold) |
| 1 | Vein |
| Rank | Characteristic |
|---|---|
| 1 | Sheared |
Date: Sep 11, 2002
Geologist: C Ravnaas
Notes: There are several mineral occurrences in the area all related to High Lake Stock. These include the Electrum (A-D) Prospect, Electrum (Arsenic Zone) Occurrence, Purdex (A-D) Occurrence, High Lake and Evenlode Occurrence.
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| P Zone | 1987 | Unclassified | 10000 | AFRI 52E11NE9032, p. 16 | average width of 12.96 feet using a tonnage factor of 11.50 cubic feet per ton | Gold 0.29 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 |
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:
MonoMap - Geology of High Lake-Rush Bay area, District of Kenora
Publication Number: R041 Page: 42-43 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 Page: 143 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 Page: 15 Date: 1976
Author: Beard R.C., Garratt G.L.
Publisher Name: Ontario Division of Mines
Location:
Mono - The geological setting of gold occurrences in the Lake of the Woods area
Publication Number: OFR5695 Page: 108-109 Date: 1988
Author: Davies J.C., Smith P.M.
Publisher Name: Ontario Geological Survey
Location:
Article - Geology of the High Lake area, Ewart Township, District of Kenora
Publication Number: MP137.010 Date: 1997
Author: Smith P.M.
Publisher Name: Ontario Geological Survey
Location:
Thesis - Mineralization of the High Lake Pluton and Adjacent Country Rocks
Publication Number: MSc Thesis Date: 1976
Author: Pedora, J.M.
Publisher Name: University of Manitoba
Location: Kenora RGP
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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