Ontario Geological Survey
Permanent Link to this Record:
MDI52J13NE00007
Record Name(s) | Capital Lithium Mines 34 Claim Group - 1957, Root Lake Pegmatite Group - 2003 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 2003-Mar-05 |
Date Last Modified | 2023-May-12 |
Created By | |
Revised By |
Primary Commodities: Lithium
Secondary Commodities: Rare Earth Elements
Township or Area: Root Lake Area
Latitude: 50° 54' 23.14" Longitude: -91° 38' 42.69"
UTM Zone: 15 Easting: 595255.53 Northing: 5640293.7 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52J13NE
Point Location Description: DDH 5 location from assessment file map, hole collar not visible
Location Method: Based on Assessment
Access Description: Area is accessed by logging roads that extend along the north side of Root Lake from the Rawhide Road.
1956-57: Ground MAG survey followed by 5 diamond drill holes for 3240 feet by Capital Lithium Mines. 2011: Pierre Gagne Contracting conducted an airborne aeromag survey. 2012: Golden Dory Resources Corp. carried out prospecting and soil sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.49486 | 20000006839 | 20000006839 |
63.857 / 52J13NE0012 | 52J13NE0010 | 52J13NE0010 |
52J13NE0016 | 52J13NE0004 | 52J13NE0004 |
2.53411 | 20000008632 | 20000008632 |
Province: Superior
Subprovince: English River
Geological Age: Neoarchean
Aug 28, 2007 (Mark Puumala) - Blackburn et al. (1999) report that the Capital Lithium Mines occurrences are based on reported diamond drill intersections of white, muscovite-bearing pegmatites containing abundant tourmaline during a 1957 exploration program. The "34 claim group" occurrence is based on reports of beryl crystals (up to 3 mm) in two diamond drill holes, while the "5 claim group" occurrence is based on reports of spodumene in a single drill hole. Reconnaissance sampling of surface exposures of a number of pegmatites in the area of the Capital Lithium Mines occurrences that was reported by Hinz et al. (1999) did not report any significant assay results.
Jun 08, 2021 (Therese Pettigrew) - The Root Lake property straddles the Uchi and English River Subprovinces of the Superior Province of Northwest Ontario. The main mineralized zone lies within unsubdivided metavolcanic and clastic sedimentary rocks of the Birch-Uchi Greenstone Belt and to a lesser extent mafic metavolcanic rocks of the English River Subprovince.
Rock Type | Rank | Composition | Texture | Relationship | Pegmatite | 1 | Host |
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Terrigenous-Clastic-Unsubdivided | 2 | Adjacent | ||
Mafic lava flow-unsubdivided | 3 | Adjacent |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Beryl | Economic | Ore | ||||
2 | Tourmaline | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore | ||||
5 | Chalcopyrite | Economic | Ore | ||||
6 | Bornite | Economic | Ore | ||||
1 | Feldspar | Economic | Gangue | ||||
2 | Quartz | Economic | Gangue | ||||
3 | Muscovite | Economic | Gangue |
Jun 08, 2021 (Therese Pettigrew) - The five holes drilled in 1957 by Capital Lithium Mines intersected numerous, white, muscovite--bearing pegmatites with abundant tourmaline. Two of the holes, numbers 2 and 5, intersected pegmatites reported to contain green beryl crystals up to 3 mm in size. Abundant, disseminated sulphides (estimated up to 7%) were encountered, predominantly consisting of pyrite and pyrrhotite, but chalcopyrite and bornite were reported, particularly in holes 1 and 3 (bornite was reported from hole 1 only) (Hinz et al., 2000). Spodumene (lithium silicate) crystals (locally up to 50 cms in length) are exposed in a 9.14 metre wide medium to very coarse grained pegmatite dike, in association with feldspar, quartz, mica and tourmaline. Tourmaline is most common at or near the dike contacts. It is believed the associated rare metals including Ta and Nb are closely linked to the presence of tourmaline. Li ranged from detection limit of 2 ppm to 145 ppm in sample 791166 located in the south east corner of claim 4250499. The sample is described as a feldspar-rich rock with traces of pyrite. Rare earth element results were converted to oxides and results were also given as total rare earth oxides (TREO) and listed in Appendix 6. TREO values ranged from 10 to 250 ppm in the central part of claim 4251419. The sample is described as a biotite-rich pegmatite with an unidentified purple mineral located in outcrop (Assessment report 20000008632).
Rank | Classification |
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1 | Pegmatite |
Rank | Characteristic |
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1 | Intrusive |
Map - Root Lake sheet, Kenora District
Publication Number: M2156 Scale: 1:31,680 Date: 1969
Author: Clifford P.M.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Report of Activities 1999, Resident Geologist Program, Red Lake Regional Resident Geologist Report: Red Lake-Kenora Districts
Publication Number: OFR6003 Page: 25-26 Date: 2000
Author: Hinz P., Storey C.C., Gosselin S.D.M., Blackburn C.E., Kosloski L.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 1998, Resident Geologist Program, Red Lake Regional Resident Geologist Report: Red Lake and Kenora Districts
Publication Number: OFR5987 Page: 25-37 Date: 1999
Author: Blackburn C.E., Hinz P., Storey C.C., Kosloski L., Ravnaas C.
Publisher Name: Ontario Geological Survey
Location:
Mono - An evaluation of the industrial mineral potential of parts of the districts of Kenora and Rainy River
Publication Number: OFR5718 Date: 1990
Author: Storey C.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Fertile Peraluminous Granites and Related Rare-Element Mineralization in Pegmatites, Superior Province, Northwest and Northeast Ontario: Operation Treasure Hunt
Publication Number: OFR6099 Page: 32-33 Date: 2003
Author: Breaks F.W., Selway J.B., Tindle A.G.
Publisher Name: Ontario Geological Survey
Location:
Publication - Geology of Canadian Lithium Deposits; Geological Survey of Canada, Economic Geology Report 21
Publication Number: Econ Geol 21 Page: 64-65 Date: 1965
Author: Mulligan, R.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/102454
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