Ontario Geological Survey
Permanent Link to this Record:
MDI52C10NE00062
Record Name(s) | Bull -Price - 1990, Dinosaur - 1990, Bull-Sterling - 9999, J.O. 15 - 9999 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1990-Dec-08 |
Date Last Modified | 2022-Mar-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper, Silver
Township or Area: Bad Vermilion Lake Area
Latitude: 48° 42' 50.26" Longitude: -92° 33' 9.92"
UTM Zone: 15 Easting: 532899.404 Northing: 5395755.407 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52C10NE
Point Location Description: Claim J.O. 15 near the eastern boundary of Map 334A, 1.5km north of the Seine River.
Location Method: Data Compilation
Access Description: The property is accessible by water through the Seine River System, with launching sites on Shoal Lake. Then via foot trail to the property. The property is also accessible by all terrain vehicle and then foot a foot trail from bush roads off the Shoal Lake Road. (Schnieders and Dutka 1985).
1895: Bull Price property, stripping and test pitting (FF682 and 685). 1935: Owned by Mrs. A. Liezert. 1937: Doc Smylie did exploration to the southwest of the Dinosaur property. 1,300 man days of work and 5 x-ray drill holes were reported. 1980: Property visited by Greenwich Lake Exploration Co. Ltd. 1981: D. Levere owns patented claims J.O. 13, J.O. 14 and P669. Did minor stripping, trenching and sampling.
Province: Superior
Subprovince: Wabigoon
Belt: Fort Frances-Mine Centre
Geological Age: Archean
Dec 07, 2005 (P Hinz) - The area is underlain by intermediate to felsic metavolcanics which have undergone intensive alteration, including silicification and sericitization. Silicified sericite schist is present along strike from intermediate flows and tuffs. The sericite-chloritoid schists display no preserved primary textures, but are likely the altered equivalents of the intermediate metavolcanics. Gabbro, quartz-feldspar and feldspar porphyries, sills and dikes intrude the metavolcanics, with the felsic porphyry apparently being a later intrusive event. Diabase dikes appear to be the latest intrusive event. Shallow water metasediments unconformably over-lie the Bad Vermilion intrusion and consist of conglomerate, sandstone, siltstone and ironstone, believed to be derived from a volcanic source area (Woods et al., 1980). (Schnieders and Dutka 1985).
Rock Type | Rank | Composition | Texture | Relationship | Schist-Unsubdivided | 1 | Sericite | Host |
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Dec 07, 2005 (P Hinz) - Quartz veins hosted by silicified sericite schist are present on the Dinosaur property. Early reports indicated that small lenses of quartz porphyry were present, with the borders altered and sheared to sericite schist. In the area of the Dinosaur occurrence, the metavolcanic belt is approximately 1.5 to 2.0 kilometres wide and consists primarily of intermediate flows and pillowed flows. The sericite schist may represent the altered equivalent of the intermediate metavolcanics.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
2 | Gold | Economic | Ore | ||||
3 | Malachite | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Tourmaline | Economic | Ore | ||||
1 | Ankerite | Economic | Gangue | ||||
2 | Limonite | Economic | Gangue | ||||
3 | Tourmaline | Economic | Gangue | ||||
4 | Sericite | Economic | Gangue | ||||
5 | Chlorite | Economic | Gangue | ||||
Sericite | Alteration | Sericitization | 1 | Replacement |
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Gold | Unknown | .01 | oz/T |
Part - Second report on the gold fields of western Ontario
Publication Number: ARV05.002 Scale: Date: 1998
Author: Coleman A.P.
Publisher Name: Ontario Bureau of Mines
Location:
Mono - Property visits and reports of the Atikokan economic geologist, 1979-1983, Atikokan geological survey
Publication Number: OFR5539 Scale: Date: 1985
Author: Schnieders B.R., Dutka R.J.
Publisher Name: Ontario Geological Survey
Location:
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