Ontario Geological Survey
Permanent Link to this Record:
MDI000000000122
Record Name(s) | Inco DDH 25068 - 1965 |
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Related Record(s) | |
Record Status | Occurrence |
Date Created | 2006-Jul-28 |
Date Last Modified | 2022-Nov-07 |
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Revised By |
Primary Commodities: Nickel, Gold
Township or Area: Aubin
Latitude: 48° 53' 19.9" Longitude: -81° 28' 15.47"
UTM Zone: 17 Easting: 465475.999 Northing: 5415208.002 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A14NW
Point Location Description: Approximate: Collar location scaled from drill plan, measurements transferred to GIS map
Location Method: Based on Assessment
1963-1966, Abitibi-Canico JV: Inco options properties in 10 twps from Abitibi Price 1963-1964, Abitibi-Canico JV: Amag, AEM (T-3529, 63.4838) 1964-66, Inco: Ground geophysics, drilling, assays (T-3213) 1980-1981, Hudbay Mining Limited JV with Abitibi Price: Amag, AEM (T-3534, 63.4810) 1983-1985, Chevron Canada Resources: Regional compilation (T-3539, T-3529) 1989, Rio Algom Exploration: Options Abitibi Price property, begins 10-twp Abitibi-Timmins project 1990-1991, Rio Algom: Compilation and reinterpretation of previous work; mapping; overburden (sonic) drilling (T-3573; T-3425)
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-3213 / 63.4811 | 42A13NE0006 | 42A13NE0006 |
T-3529 / 63.4838 | 42A14SE0106 | 42A14SE0106 |
Rock Type | Rank | Composition | Texture | Relationship | Peridotite | 1 | Peridotite | Contains |
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Intermediate lava flow-unsubdivided | 2 | Contains | ||
Ultramafic lava flow-unsubdivided | 3 | Pyroxenite | Adjacent |
Jul 28, 2006 (D Draper) - Hole drilled to 854ft, bearing north, dipping -50 deg, in tuff, chert and intermediate metavolcanics to 314ft, serpentinized peridotite to 690ft and then pyroxenite (or mafic metavolcanics--file log unclear) to 841ft. Hole bottomed in tuff.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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Serpentine | Alteration | Serpentinization | 1 | ||||
Magnesite | Alteration | 2 | |||||
Talc | Alteration | 3 |
Jul 28, 2006 (D Draper) - Assays of core returned 0.09% - 0.21% Ni in peridotite from 427ft to 674ft. The peridotite is described as magnetic, serpentinized and carrying stringers and veinlets of magnesite and talc. Only one reference in log to sulphides within zone of Ni assays (occ. visible specks of sulphide--unspecified) . A 1-foot sample of the brecciated tuff unit @ 196.4ft assayed 0.024 opt Au. The unit was mineralized with 3% po, disseminated py, tr cpy and possibly sphalerite. This same sample returned the highest copper assay for the hole, at 0.15% Cu. (AF T-3213)
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