Ontario Geological Survey
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MDI53A12SE00004
Record Name(s) | Schryburt Lake - 1961 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1985-Jun-20 |
Date Last Modified | 2023-Jun-09 |
Created By | |
Revised By |
Primary Commodities: Niobium, Phosphate
Secondary Commodities: Uranium
Township or Area: Schryburt Lake Area
Latitude: 52° 36' 12.21" Longitude: -89° 37' 12.15"
UTM Zone: 16 Easting: 322577.22 Northing: 5831376.44 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 53A12SE
Point Location Description: Precise
Location Method: Data Compilation
Access Description: Schryburt Lake is located approximately 128 km northeast of Pickle Lake and is accessible by float-equipped aircraft.
1960: 30 claims staked by Many Lakes Exploration Company. 1961: Many Lakes Exploration Company Ltd. conducted mapping, prospecting, trenching, sampling, and a ground magnetic survey. 1976: OGS staff mapped the complex. 1975-77: International Minerals & Chemical Corp. conducted geological mapping, soil sampling, and drilled 6 vertical reverse circulation holes totaling 292.6 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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53A12SE0010 | 53A12SE0001 | 53A12SE0001 |
63.3423 | 20000019638 | 20000019638 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Domain: Island Lake
Geological Age: Archean Geochronological Age: 1145 +/- 74 Ma Geochron. Age Ref.: Sage, 1983
Rock Type | Rank | Composition | Texture | Relationship | Carbonatite-Unsubdivided | 1 | Is |
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Granitoid-Unsubdivided | 2 | Adjacent |
Sep 12, 2019 (Therese Pettigrew) - Samples collected from the pits and trenches indicate the complex is composed predominantly of calcitic carbonatite. Subvertical bands of nearly pure sovite alternate with bands of silicocarbonatite. One pit exposed a coarse-grained dolomite dike. In the carbonate, very pronounced bands of nearly pure actinolite, apatite, magnetite, biotite-phlogopite, or pyrrhotite alternate with pink to pink-white carbonate. The rocks are highly variable in colour, texture, and grain size, but generally could be classified as equigranular and medium-grained. One outcrop of granitic rock in the northeast corner of the complex is strongly fenitized and extensively cut by carbonate dikes (Sage, 1983).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrochlore | Economic | Ore | ||||
2 | Apatite | Economic | Ore | ||||
3 | Magnetite | Economic | Ore | ||||
4 | Perovskite | Economic | Ore | ||||
5 | Fluorite | Economic | Ore | ||||
6 | Vermiculite | Economic | Ore | ||||
1 | Calcite | Economic | Gangue |
Sep 12, 2019 (Therese Pettigrew) - The complex is principally carbonatite and varies from nearly pure calcite to almost pure apatite with bands of massive magnetite several feet in thickness. Pyrochlore is present as an accessory mineral (Ferguson 1971). Samples from trenches done in 1961 by Many Lakes Exploration returned assays of up to 1.82% Nb2O5 from a grab sample and 0.40% Nb2O5 over 8 feet from a channel sample. Many Lakes Exploration Co. Ltd. took 55 samples, 43 of which assayed below 0.1% niobium oxide, 8 between 0.1 and 0.3%, and 4 between 0.3 and 1.82%. Perovskite is the chief source of the lower niobium values, the higher values occurring in pyrochlore associated with apatite-rich samples. Pyrochlore was present in a magnetite-rich sample from trench 21 of Many Lakes Exploration Ltd. Radioactivity was 8 to 9 times background within the bottom of the trench and the soil consisted of medium-grained, disaggregated carbonatite composed of magnetite and carbonate grains. A coherent sample was collected from a pit within the trench at a depth of approximately 1.5 metres. In thin section pyrochlore is present as dark brown, subhedral grains. It is present as isolated grains within carbonate and as grains perched on the edge of ,magnetite grains. One of the larger grains contains inclusions or blebs of carbonate. Cracks commonly radiate out from this grain. A sample of the soil, assayed for uranium and niobium, returned 0.039% U3O8 and 0.08% niobium. International Minerals and Chemical Corp. drilled 6 vertical reverse circulation holes. This drilling encountered residual apatite accumulations only in hole SC-1. Within this hole 9.0 meters (30 feet) of apatite-rich residual soil returned an average assay of 17.5% P2O5, with values up to 19.6% P2O5 over 5 feet (Sage, 1983). Thin sections prepared from resistant nodules of carbonatite recovered from the carbonatite soils indicate that the rocks of the intrusion have a high carbonate content. The samples contain 10-100% carbonate, trace to 35% magnetite, trace to 0.4% zircon, trace to nearly 14% apatite, from less than 1 to more than 28% biotite, 0 to more than 26% clinopyroxene, and from 0 to more than 13% olivine. Generally minor amounts of arfvedsonite, actinolite, brown alteration, perovskite, nepheline, cancrinite, serpentine, quartz and orthoclase were identified in one or more thin sections. The nepheline noted in one section is well zoned and the zircons in one section were also zoned. The pyroxene in one section is zoned from a light brown core to a grey rim. Olivine in the same section as the zoned pyroxene is very fresh, but was serpentinized in other thin sections (Thurston et al, 1979).
Article - Carbonatite-alkalic complexes
Publication Number: MP067.013 Date: 1997
Author: Sage R.P.
Publisher Name: Ontario Division of Mines
Location:
Map - Geological series, Schryburt Lake carbonatite complex, District of Kenora (Patricia Portion)
Publication Number: P2236 Scale: 1:15,840 Date: 1979
Author: Sage R.P., Wright W.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of the Schryburt Lake carbonatite complex
Publication Number: OFR5413 Date: 1984
Author: Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of carbonatite-alkalic rock complexes in Ontario: Schryburt Lake carbonatite complex, District of Kenora
Publication Number: S050 Date: 1988
Author: Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of Winisk Lake area, District of Kenora, Patricia Portion
Publication Number: R193 Page: 123-129 Date: 1980
Author: Thurston P.C., Sage R.P., Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
Map - Geophysical series, Obabigan Lake, Kenora District, Ontario, airborne magnetic, total field
Publication Number: M00938G Scale: 1:63,360 Date: 1998
Author: Geological Survey of Canada, Ontario Dept. of Mines
Publisher Name: Geological Survey of Canada, Ontario Dept. of Mines
Location: https://doi.org/10.4095/110384
Mono - Uranium and thorium deposits of northern Ontario
Publication Number: MDC025 Page: 79 Date: 1984
Author: Robertson J.A., Gould K.L.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Columbium (niobium) deposits of Ontario
Publication Number: MDC014 Page: 48 Date: 1971
Author: Ferguson S.A.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
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