Ontario Geological Survey
Permanent Link to this Record:
MDI52O11SW00003
Record Name(s) | Dougie Lake West - 1979, Semia Lake-Kenlew - 1979, McVicar Lake G, 1 - 1979 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1979-Sep-25 |
Date Last Modified | 2022-May-27 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: McVicar Lake Area
Latitude: 51° 31' 5.07" Longitude: -91° 24' .45"
UTM Zone: 15 Easting: 611004.485 Northing: 5708652.654 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O11SW
Point Location Description: Precise
Location Method: Conversion from MDI
1950: Chellow Gold Mines Ltd. Conducted geological mapping, trenching and diamond drilling in the Lower McVicar Lake area. 1959-1961: Kenlew Mines Ltd conducted geological mapping, stripping, trenching and diamond drilling in the lower McVicar Lake area and the area to the east of McVicar Lake. 1968-1969: New Jersey Zinc Exploration Company (Canada) Limited conducted geological mapping, geophysics, trenching and limited diamond drilling for VMS mineralization in the area north of north of McVicar Lake. 1971: Hoey Syndicate conducted geological mapping, trenching and geophysics for Cu-Ni-PGE mineralization in the lower half of the McVicar Lake area. 1977-1981, 1987, 1991 Cominco Ltd conducted extensive airborne geophysical surveys as well as diamond drilling over the McVicar Lake and Andy lake areas, well as limited diamond drilling in McVicar and Cannon Lake areas for gold and base metals. 1985-1994 Utah Mines, later BHP-Utah Mines, and then simply BHP conducted extensive grid mapping, geophysics and diamond drilling on the area surrounding McVicar Lake resulting in the discovery of the Altered Zone and Lower McVicar Lake structural zones and several associated gold showings. Utah Mines also conducted extensive work in the western Lang Lake area. 2001-2003 Prospector Consolidated Inc and Continuum Resources Ltd, conducted extensive trenching and limited diamond drilling for gold on the old BHP-Utah Mines property in the McVicar Lake area.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52O11SW0021 | 52O11NE0001 | 52O11NE0001 |
52O11SW0020 | 52O11NE0003 | 52O11NE0003 |
52O11SW-25 | 52O11SW0033 | 52O11SW0033 |
52O11SW-41 | 52O11SW0029 | 52O11SW0029 |
52O11SW-43 | 52O11SW0021 | 52O11SW0021 |
52O11SW0013B1 | 52O11SW0055 | 52O11SW0055 |
13, 52O11SW0014A1 | 52O11SW0069 | 52O11SW0069 |
2.27178 | 52O11SW2003 | 52O11SW2003 |
2.18309 | 52O11SW2001 | 52O11SW2001 |
63.5247 | 52O11SE0080 | 52O11SE0080 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Lang Lake
Geological Age: Neoarchean
Mar 28, 2007 (Mark Puumala) - Stott and Corfu (1991) describe the Lang Lake greenstone belt as being dominated by tholeiitic basalt flows and calc-alkalic pyroclastic deposits, with the eastern portion of the belt containing a significant clastic metasedimentary sequence that also includes iron formation horizons. The supracrustal rocks of this belt have been provisionally assigned to the Confederation Assemblage by Stott and Corfu (1991) based on a single age determination from a dacitic tuff in the lowermost (i.e., interpreted to be oldest) portion of the supracrustal rock sequence. The entire belt has been isoclinally folded into an east-trending and east-plunging syncline (Thomas 1988). Thomas (1988) also indicates that the belt contains two significant intrusions, including an east-west trending mafic stock in the Sor-McVicar Lakes area, and a later north-south trending felsic intrusion in the Shonia-McVicar Lakes area. The mafic intrusion has a number of Cu-Ni-PGE occurrences that have been documented near its northern contact, while the felsic intrusion hosts several gold occurrences. The dominant structural feature in the area is the Bear Head Fault Zone, which is located immediately to the southwest. This is an approximately northwest-southeast striking, regional-scale, dextral shear zone that has been classified by Stott and Corfu (1991) as a transcrustal megafault. This fault zone extends approximately 515 km from Lake Winnipeg to the northern boundary of the Meen-Dempster Greenstone Belt (Osmani and Stott 1988). Two additional WNW-ESE trending deformation zones referred to as the Lower McVicar Fault and Altered Zone Fault (McKay 2004) are also present in the area and are associated with a number of gold occurrences. Fumerton (1997) suggests a relationship between the Altered Zone Fault and the axial plane of the regional syncline. Fumerton (1997) indicates that supracrustal rocks between the Bear Head and Lower McVicar Faults have been folded into sigmoidal S-folds, and that a number of splay faults also exist in this area. The geometry of these structures has been interpreted as being consistent with a dextral sense of displacement.
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Basalt | Adjacent |
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Intermediate lava flow-unsubdivided | 2 | Andesite | Adjacent | |
Mylonite/Fault Gouge/Pseudotachylite | 3 | Shear Zone | Contains | |
Vein | 4 | Host |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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5 | Arsenopyrite | Economic | Ore | ||||
10 | Chalcopyrite | Economic | Ore | ||||
15 | Pyrite | Economic | Ore | ||||
20 | Pyrrhotite | Economic | Ore | ||||
25 | Sphalerite | Economic | Ore | ||||
Sericite | Alteration | Sericitization | 1 |
Mar 28, 2007 (Mark Puumala) - The Dougie Lake West occurrence is described by Leonard (1986) as a mineralized shear zone from which Pickle-Patricia Explorers and Kenlew Mines are reported to have obtained assay values of up to 2 oz/ton Au in the early 1960s. The mineralized shear is reported to be an approximately 1.5 m wide zone in intermediate metavolcanics that strikes approximately 120 degrees. The shear contains a massive to moderately laminated milky white quartz vein that contains minor disseminated pyrite. A 30 to 40 cm wide zone of massive pyrite was also reported to occur in contact with the vein (Leonard 1986). Pickle-Patricia Explorers DDH log KL-4 (AFRI# 52O11SW0069) indicates that gold mineralization at depth occurred in a smoky grey quartz vein mineralized with wispy greenish sericite, acicular arsenopyrite (up to 2%), pyrite (up to 3%) and pyrrhotite (trace). This vein was reported to occur within an approximately 1.5 m wide section of shear zone material mineralized with pale green sericite, arsenopyrite and pyrite. The sheared material occurs within material logged as mafic metavolcanics. The most favourable reported assay from DDH KL-4 was 0.11 oz/ton Au.
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Vein |
Book - AF SL 1986 52O11SW-0039-C1
Publication Number: N/A Date: 1996
Author:
Publisher Name:
Location:
Book - AFRO 1962, MCVICAR LAKE AREA, DHR 1
Publication Number: N/A Date: 1996
Author:
Publisher Name:
Location:
Article - Uchi subprovince
Publication Number: SV04-01.006 Page: 145-236 Date: 1997
Author: Stott G.M., Corfu F.
Publisher Name: Ontario Geological Survey
Location:
Article - Regional-scale shear zones in Sachigo Subprovince and their economic significance
Publication Number: MP141.006 Page: 53-67 Date: 1997
Author: Osmani I.A., Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
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