Ontario Geological Survey
Permanent Link to this Record:
MDI32E13SE00008
| Record Name(s) | Getty DDH Dl-82-06 - 1982, Getty DDH Dl-83-38 - 1983 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1991-Feb-25 |
| Date Last Modified | 2022-Jul-15 |
| Created By | |
| Revised By |
Primary Commodities: Copper
Secondary Commodities: Zinc
Township or Area: Atkinson Lake Area
Latitude: 49° 50' 9.66" Longitude: -79° 33' 47.86"
UTM Zone: 17 Easting: 603312.431 Northing: 5521388.664 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 32E13SE
Point Location Description: Approx locn of drill collar on former claim P619063
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.
1975: Hudson Bay Exploration and Development Co. Ltd. - ground geophysics. 1981-83: Getty Canadian Metals Ltd. - airborne geophysics, ground geophysics, mapping, 1 ddh (236.5 m). 2007: Dentonia Resources Ltd. - airborne geophysics
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| T-2443 / 2.4292 | 32E13NE9322 | 32E13NE9322 |
| T-2443 / 2.4849 | 32E13SE0016 | 32E13SE0016 |
| T-2443 / 2.5578 | 32E13SE0013 | 32E13SE0013 |
| T-5819 / 2.40023 | 20000003683 | 20000003683 |
| T-1704 / 2.1976 | 32E13SE0032 | 32E13SE0032 |
| T-2443 | 32E13NE0045 | 32E13NE0045 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Neoarchean
| Rock Type | Rank | Composition | Texture | Relationship | Pyroxenite | 1 | Pyroxenite | Hanging Wall |
|---|---|---|---|---|
| Mafic massive flow | 2 | Massive | Hanging Wall | |
| Chert | 3 | Sulphide-Bearing | Host | |
| Mafic Tuff | 4 | Tuff | Footwall |
Dec 07, 2005 (A Wilson) - Elevated Cu values were recovered from a cherty, sulphide-rich conductive zone interbedded with mafic flows and tuffs. An ultramafic flow also returned slightly elevated Cu values.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Chalcopyrite | Economic | Ore | ||||
| 1 | Pyrrhotite | Economic | Gangue | ||||
| 2 | Pyrite | Economic | Gangue | ||||
| 3 | Molybdenite | Economic | Gangue |
Dec 23, 2010 (D Draper) - In hole DL-82-06, the 7.2m conductive zone returned averaged values of up to 3400 ppm Cu and 1600 ppm Zn over 1m. Follow-up hole DL-83-38, collared 212.5m grid north of -06, returned: 2800 ppm Cu over 0.5m from an upper unit of conductive, cherty, metasediments; 4200 ppm and 3500ppm Cu, each over 0.5m, from a lower unit of a similar zone; and 3900 ppm Zn over 0.5m in ultramafic intrusive. (T-2443)
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:
MonoMap - Geology of the Burntbush-Detour lakes area, District of Cochrane
Publication Number: R199 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:
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