Ontario Geological Survey
Permanent Link to this Record:
MDI42C08SE00088
| Record Name(s) | Canreos-Armistice Showing #4 - 1989 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 2001-May-11 |
| Date Last Modified | 2022-Nov-02 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Bruyere
Latitude: 48° 16' 17.72" Longitude: -84° 12' 33.11"
UTM Zone: 16 Easting: 707077 Northing: 5350252 UTM Datum: NAD83
Resident Geologist District: Sault Ste. Marie
NTS Grid: 42C08SE
Point Location Description: Chip samples from sheared quartz on east shore of island in Emily Bay
Location Method: Based on Assessment
Access Description: Access to the site is most easily made by boat from Missinabie via Emily Bay.
1974: Umex: airborne geophysics. 1983: Hemgold Resources - airborne geophysics. 1985: Kingswood Exploration Ltd. - airborne geophysics. 1987: Tenoga Consultants Ltd. - airborne geophysics. 1989: Shelagh Resources/Belmoral Mines/Canreos/Armistice JV - mapping, sampling.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| WP Bruyere.6/2.11094 | 42C08SW0089 | 42C08SW0089 |
| Aguonie 0027A1 | 42C08SE0674 | 42C08SE0674 |
| Jacobson 0019A1 / 63.1263 | 42C08SW0089 | 42C08SW0089 |
| Bruyere 0022/ 2.7968 | 42C08SE0023 | 42C08SE0023 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Michipicoten
Geological Age: Archean
Dec 07, 2005 (A Wilson) - The Emily Bay Deformation Zone (EBDZ) is located on the west side of Dog Lake in southern Riggs Township. The EBDZ is a 500 m wide, east-northeast trending zone of intense ductile shearing and weakly to strongly strained rocks. The EBDZ can be traced up to 4 km to the southwest of Dog Lake but cannot be traced to the eastern side of Dog Lake. The EBDZ is localized within massive to pillowed mafic metavolcanic rocks that are deformed to chlorite-calcite and chlorite-iron carbonate schists within several discrete ductile shear zones. These shear zones are NE-trending and vay in width from 1 m to greater than 30 m. A second set of narrow, brittle to ductile, NW-trending shear zones is observed in the vicity of this showing.
| Rock Type | Rank | Composition | Texture | Relationship | Granitoid-Unsubdivided | 1 | Felsite Dike | Massive | Host |
|---|---|---|---|---|
| Vein | 2 | Quartz | Host | |
| Mafic pillowed flow | 3 | Basaltic | Pillowed | Near |
Dec 07, 2005 (A Wilson) - The occurrence consists of two bands of sheared felsite and quartz within a massive felsite dike. The felsite dike intrudes pillowed mafic basalts.
Oct 20, 2014 (A Wilson) - Chip samples taken from the sheared felsite and quartz ranged from trace to 0.006 oz/t Au over 3 feet.
| Rank | Characteristic |
|---|---|
| 1 | Sheared |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Regular | 20 | 60 |
File - Resident Geologist files WP Riggs.25
Publication Number: Date:
Author:
Publisher Name:
Location: SSM RGP office
Map - Geological compilation series, Wawa sheet, districts of Algoma and Sudbury
Publication Number: P0640 Scale: 1:126,720 Date: 1997
Author: Leahy E.J., Rupert R.J., Giblin P.E., Giguere J.F.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Map - Precambrian Geology Compilation Series - White River Sheet
Publication Number: M2666 Scale: 1:250,000 Date: 2001
Author: Santaguida F.
Publisher Name: Ontario Geological Survey
Location:
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