Ontario Geological Survey
Permanent Link to this Record:
MDI32E13SE00019
| Record Name(s) | Kesagami DDH 12-2 - 1959, Loon Group - 1959, Westmin Vandette Group - 1989 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1985-Aug-19 |
| Date Last Modified | 2023-Jul-11 |
| Created By | |
| Revised By |
Primary Commodities: Zinc
Secondary Commodities: Copper
Township or Area: Atkinson Lake Area
Latitude: 49° 51' 46.91" Longitude: -79° 38' 24.46"
UTM Zone: 17 Easting: 597733.027 Northing: 5524288.645 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 32E13SE
Point Location Description: Drill collar at L4N 1+80E on former claim L68901
Location Method: Based on Assessment
Access Description: Access to the property is by fixed wing aircraft from Cochrane, or by all terrain vehicle from the Detour Lake Mine site. Detour Lake Mine is accessible by an all-season road from Cochrane.
1959: Kesagami Syndicate - 1 ddh (225 ft). 1982-84: Getty Canadian Metals Ltd. - airborne geohysics, mapping, 1989-90: Westmin Mines Ltd. - ground geophysics, mapping. 2007: Dentonia Resources Ltd. - airborne geophysics
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| T-5819 / 2.40023 | 20000003683 | 20000003683 |
| T-2443, 2.4292 | 32E13NE9322 | 32E13NE9322 |
| 14 | 32E13SE0050 | 32E13SE0050 |
| T-3351, 2.13390 | 32E13SE0003 | 32E13SE0003 |
| 2.4613, T-2443 | 32E13NE0081 | 32E13NE0081 |
| 2.5306, T-2443 | 32E13NE0074 | 32E13NE0074 |
| 33, T-2443 | 32E13SE0022 | 32E13SE0022 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Neoarchean
| Rock Type | Rank | Composition | Texture | Relationship | Intermediate Tuff | 1 | Tuff | Hanging Wall |
|---|---|---|---|---|
| Ironstone-unsubdivided | 2 | Ampholitized | Hanging Wall | |
| Feldspar Porphyry | 3 | Feldspar | Near | |
| Mudstone | 4 | Graphitic Argillite | Host |
Dec 07, 2005 (A Wilson) - Diamond drilling intersected a sequence of intermediate flows and tuffs, overlying argillite and quartzite. The units are intruded by narrow feldspar porphyry dikes. The main conductor is described as a graphtic zone.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Sphalerite | Economic | Ore | ||||
| 1 | Pyrite | Economic | Gangue | ||||
| 2 | Pyrrhotite | Economic | Gangue |
Dec 07, 2005 (A Wilson) - The best assay returned 0.73% Zn, 0.09% Cu over 5 ft.
File - Resident Geologist file T-3786
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Burntbush-Detour lakes, Cochrane District
Publication Number: M2453 Scale: 1:100,000 Date: 1982
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Burntbush-Detour Lakes Area, Abitibi Greenstone Belt
Publication Number: P3609 Scale: 1:100,000 Date: 2009
Author: Ayer J.A., Chartrand J.E., Duguet M., Rainsford D.R.B., Trowell N.F.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of the Burntbush-Detour lakes area, District of Cochrane
Publication Number: R199 Page: 71-72 Date: 1982
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
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