Ontario Geological Survey
Permanent Link to this Record:
MDI000000001621
| Record Name(s) | Dome Exploration DDH 83B-2 - 1975 |
|---|---|
| Related Record Type | |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 2013-Sep-05 |
| Date Last Modified | 2022-Sep-15 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper, Zinc
Township or Area: Rennie
Latitude: 48° 22' 37.18" Longitude: -84° 0' 25.2"
UTM Zone: 16 Easting: 721621 Northing: 5362532 UTM Datum: NAD83
Resident Geologist District: Sault Ste. Marie
NTS Grid: 42B05NW
Point Location Description: drill collar for 83B-2
Location Method: Based on Assessment
Access Description: The site is accessible via the Renabie Road.
1975: Dome Exploration Limited – airborne geophysics, DD-1-526 ft. 1984: R.J. McGowan – airborne geophysics. 2007-2008: Chalice Diamond Corporation – airborne geophysics, prospecting, sampling.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| Stover 0026 / 63.2278 | 42C08SE0004 | 42C08SE0004 |
| Meath 0019-A1 | 42C08NE0028 | 42C08NE0028 |
| WP Meath.20/ 2.34531 | 20000002017 | 20000002017 |
| WP Stover.21 / 2.41485 | 20000004162 | 20000004162 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Michipicoten
Tectonic Assemblage: Catfish
Geological Age: Neoarchean
Sep 09, 2013 (A Wilson) - The Baltimore Lake Deformation Zone (BLDZ) is located in northwestern Stover Township where it is defined by by a 1.2 km wide, SE-trending zone of folding, transposition and shearing. The BLDZ can be traced fro approximately 6 km southeastward across Stover Township. The BLDZ is characterized by rootless isoclinal folds of bedding/schistosity, sinistral and dextral shear folds, transposition and ductile shear zones axial planar to the folds.
| Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Host |
|---|---|---|---|---|
| Intermediate lava flow-unsubdivided | 2 | Dacitic | Adjacent |
Sep 09, 2013 (A Wilson) - Diamond drilling intersected a sequence of andesite, dacite, gabbro and iron formation. The iron formation is described as fine-grained, dark grey in colour and sulphidic in composition. Graphitic schist also was observed in narrow stringers within dacite.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Pyrrhotite | Economic | Ore | ||||
| 2 | Pyrite | Economic | Gangue |
Sep 09, 2013 (A Wilson) - A 5 foot length of core assayed 0.30 dwt/t Au, 0.04% Cu and 0.15% Zn.
| Rank | Characteristic |
|---|---|
| 1 | Sheared |
File - Resident Geologist files Resident Geologist files Rennie-0010-A1
Publication Number: Date:
Author:
Publisher Name:
Location: SSM RGP office
Map - Rennie Township, District of Sudbury
Publication Number: P0404 Scale: 1:15,840 Date: 1997
Author: Riley R.A.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Glasgow, Meath, and Rennie townships, Algoma and Sudbury districts
Publication Number: M2210 Scale: 1:31,680 Date: 1971
Author: Riley R.A.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Map - Chapleau-Foleyet, geological compilation series, Algoma, Cochrane and Sudbury districts
Publication Number: M2221 Scale: 1:253,440 Date: 1976
Author: Thurston P.C., Sage R.P., Siragusa G.M.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Geology of Glasgow, Meath, and Rennie townships, districts of Algoma and Sudbury
Publication Number: R090 Date: 1971
Author: Riley R.A.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
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