Ontario Geological Survey
Permanent Link to this Record:
MDI42E12SW00008
Record Name(s) | Long Lac Superior - 1936 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1983-Sep-06 |
Date Last Modified | 2022-Jun-20 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Summers
Latitude: 49° 37' 32.11" Longitude: -87° 59' 25.63"
UTM Zone: 16 Easting: 428468 Northing: 5497474 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42E12SW, 52H09SE
Point Location Description: Plugger hole locations from map in Assessment report 42E12NW0123
Location Method: Data Compilation
1910: Claims were staked by H. Murphy and P.J. McDevitt adjoining the Leitch property to the north. 1934: A second group of claims was staked by G. Maki, L. Farrow, and J. Farrow. 1936: Drilling, blasting, trenching and sampling was performed on several of the claims by H.G. Waring and the Long Lac Superior Syndicate. 1944-1979: Various claims were staked, leased, cancelled, restaked etc. 1982-84: A group of 22 claims were staked by J. McMahon, M. Rentz, and W. Cox, including the old Murphy showings, south of the Leitch property. Geological mapping, trenching, and sampling was conducted over a flagged grid. 1988: Nipigon Gold Resources Ltd. drilled 3 DDH and conducted airborne magnetometer and EM surveys as well as stripping, trenching, mapping, and sampling. 1993: B. Kowalski carried out prospecting, samples from plugger holes, mapping, and a VLF-EM survey. 2008: Kodiak Exploration Ltd. carried out prospecting and sampling. 2012-13: R. Cote carried out prospecting, mapping, trenching, and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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OP93-689 | 42E12NW0123 | 42E12NW0123 |
2.14532 | 42E12SW0040 | 42E12SW0040 |
2.53415 | 20000008634 | 20000008634 |
2.54930 | 20000008190 | 20000008190 |
2.15318 | 42E12SW8102 | 42E12SW8102 |
2.7650 | 42E12SW0073 | 42E12SW0073 |
Province: Superior
Subprovince: Wabigoon
Belt: Beardmore-Geraldton
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Sandstone | 1 | Greywacke | Contains |
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Ironstone-unsubdivided | 2 | Contains | ||
Vein | 3 | Quartz | Host |
Oct 15, 2019 (Therese Pettigrew) - The showing area is hosted by greywackes that are fine-grained sugary in texture and are massive. The general strike and dip of the greywackes was determined to be 090/80S. A number of narrow quartz veinlets and stringers occur in the unit. The greywackes appear sheared toward the contact with the iron formations. In the massive sequence of greywackes are iron formations. The iron formations are oxide facies and contain up to 15% sulphides. Sugary and glassy quartz veinlets cross-cut the iron formations. The iron formations strike 090 however were determined to be overturned in the sequence 85N (Assessment report 42E12NW0123).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Bornite | Economic | Ore | ||||
5 | Arsenopyrite | Economic | Ore | ||||
6 | Galena | Economic | Ore | ||||
7 | Magnetite | Economic | Ore |
Nov 04, 2019 (Therese Pettigrew) - In 1936, Long Lac Superior Syndicate uncovered a few quartz veins near the east boundary of claim 19913. No assays were reported (Laird, 1937). The best sample collected by Nipigon Gold in 1982 returned 0.01 oz/t Au (0.34 g/t Au) from a greyish-white quartz vein along and iron formation and greywacke (Assessment report 42E12SW0040). A number of large stripped areas expose folded and locally sulphidized banded iron formation. Grab samples of sulphidized (=20% fine-grained pyrite) magnetite banded iron formation with minor quartz veinlets returned up to 0.02 ounce Au per ton (Resident Geologist’s Files, Thunder Bay North District, Thunder Bay; Smyk et al., 2007). Seventy-six dust samples were collected carefully into bags from the plugger holes. The depth of the plugger holes was 1.5 feet. These samples were taken along the iron formation, particularly where sulphides were apparent. Dust taken from plugger holes in magnetite-hematite-jasper iron formation. Sugary to glassy quartz veinlets cross-cut the iron formation. The veins are 2 to 5 inches in width. The iron formation contains sulphides of pyrite, pyrrhotite, chalcopyrite, bornite, minor arsenopyrite and galena as fine disseminations 1 mm in diameter and massive veinlets. The sulphides occur in varying amounts from 1 to 15% concentrations. The results from the program revealed that gold occurs along the drag folds or in the noses of the folds of the iron formation. Samples 32, 34, 54, and 66 from the 1993 plugger hole program returned assays of 4.368 ppm Au, 2.46 ppm Au, 1.671 ppm Au, and 4.858 ppm Au respectively (Assessment report 42E12NW0123).
Map - Summers Township, District of Thunder Bay
Publication Number: P0602 Scale: 1:15,840 Date: 1998
Author: Mackasey W.O.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Report of Activities 2006, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6201 Page: 20-21 Date: 2007
Author: Smyk M.C., White G.D., Puumala M.A., Magee M.A., Komar C.L.
Publisher Name: Ontario Geological Survey
Location:
Part - The western part of the Sturgeon River area (Sturgeon R.-Beardmore section)
Publication Number: ARV45-02.002 Page: 105-106 Date: 1998
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
File - Resident Geologist Mineral Deposit Files
Publication Number: Min Dep Date: 1996
Author:
Publisher Name:
Location: Thunder Bay RGP
Book - GDIF 42E12NW (unpublished)
Publication Number: GDIF Date: 1988
Author: Ontario Geological Survey
Publisher Name: Ontario Geological Survey
Location:
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