Ontario Geological Survey
Permanent Link to this Record:
MDI52K06SW00004
Record Name(s) | Aerobus Lake - 1955, Anomaly 8 - 2008 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1986-Oct-10 |
Date Last Modified | 2022-Feb-24 |
Created By | |
Revised By |
Primary Commodities: Uranium
Township or Area: Aerobus Lake Area
Latitude: 50° 21' 33.14" Longitude: -93° 20' 52.76"
UTM Zone: 15 Easting: 475247 Northing: 5578628 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52K06SW
Point Location Description: Location of Sample 244262 from AFRI 20000003744
Location Method: Conversion from MDI
Access Description: Access is by provincial highways 17 and 105 and the Timber Point Camp road. A boat launch at the Timber Point Camp provides access to the showing on Aerobus Lake. There is a network of logging roads that can be used once across the lake.
1955: 9 X-ray DDH totalling 188.4 m were drilled by S. Duggan and C. St. Paul. 1983: Noranda Exploration Company Ltd. flew an airborne magnetic survey. 1986: trenching was conducted. 2008: Delta Uranium conducted prospecting and airborne magnetic, radiometric, and VLF-EM surveys.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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10 | 52K06SW0001 | 52K06SW0001 |
2.40155 | 20000003744 | 20000003744 |
2.5956 | 52K05NE0001 | 52K05NE0001 |
Province: Superior
Subprovince: Winnipeg River
Terrane: Winnipeg River
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Granite | 1 | Contains |
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Terrigenous-Clastic-Unsubdivided | 2 | |||
Pegmatite | 5 | Contains |
Mar 14, 2018 (Therese Pettigrew) - The regional geology of the Aerobus Lake property is dominated by massive medium-grained granodiorite to granite and a gneissic tonalite suite, with minor paragneiss, migmatites and metasedimentary rocks, as well as a foliated tonalite suite. In the area of Anomaly 8, the rocks are medium-grained granite with small patches of coarser-grained pegmatite throughout and many small biotite-schist xenoliths. The higher scintillometer readings are found along the contacts with the granite and schist (AFRI 20000003744).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Biotite | Economic | Gangue | ||||
2 | Quartz | Economic | Gangue | ||||
3 | Feldspar | Economic | Gangue |
Mar 14, 2018 (Therese Pettigrew) - Grade - best assays: 0.05% U3O8 over 1.7 m, 0.07% U3O8 over 1.35 m (from DDH) and 5156 U3O8 ppm, 2501 U3O8 ppm, 2478 U3O8 ppm, 3339 U3O8 ppm (grab samples). Prospecting several of the airborne radiometric anomalies has confirmed the presence of uranium mineralization. Samples collected by OGS staff in 1975 assayed 0.03% and 0.006% U3O8 (Beard and Scott, 1975). During the 2008 radiometric survey, the highest outcrop reading noted was 40,600 cps in an old pit close to the uranium showing. This outcrop assayed up to 5156 ppm U3O8 (AFRI 200000037440). Uranium mineralization is found in medium- to coarse-grained quartz monzonite near the contact with quartz-feldspar-biotite metasediments. Yellow staining is common (Robertson and Gould, 1983).
Mono - Uranium and thorium deposits of northern Ontario
Publication Number: MDC009 Scale: Date: 1968
Author: Robertson J.A.
Publisher Name: Ontario Dept. of Mines
Location:
Article - Kenora District
Publication Number: MP023.002 Scale: Date: 1997
Author: King H.L.
Publisher Name: Ontario Dept. of Mines
Location:
Article - 1975 report of the Northwestern Regional Geologist and Kenora Resident Geologist
Publication Number: MP064.001 Scale: Date: 1997
Author: Beard R.C., Scott W.R.
Publisher Name: Ontario Division of Mines
Location:
Mono - Uranium and thorium deposits of northern Ontario
Publication Number: MDC025 Scale: Date: 1984
Author: Robertson J.A., Gould K.L.
Publisher Name: Ontario Geological Survey
Location:
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