Ontario Geological Survey
Permanent Link to this Record:
MDI52K13NW00026
| Record Name(s) | Halden Red Lake Mines Ltd - 1944, Madsen-Hall Group - 1943 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1991-Mar-11 |
| Date Last Modified | 2022-Aug-05 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Heyson
Latitude: 50° 57' 6" Longitude: -93° 53' 2.12"
UTM Zone: 15 Easting: 437911.574 Northing: 5644821.977 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52K13NW
Point Location Description: N/A
Location Method: Conversion from MDI
Halden Red Lake Gold Mines Ltd. was incorporated around 1944 to acquire the property formerly known as the Madsen-Hall Group. Only preliminary prospecting and surface work was performed before 1946. 1946: X-ray drilling was completed but no record of footage are recorded. 1947: diamond drilling was performed, with seven deep holes being completed. The company's charter was cancelled in 1958. 1974: the property was included in a larger group of claims staked by Bob Mykyiuk.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Amphibolite
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Stringers And Veins | Host |
|---|---|---|---|---|
| Intermediate lava flow-unsubdivided | 2 | Near | ||
| Quartz-Feldspar Porphyry | 3 | Quartz, Quartz-Feldspar | Adjacent | |
| Granite | 4 | Near |
Dec 07, 2005 (K R Kettles) - The northwestern portion of the property is underlain by the Faulkenham Lake granite stock. The dominant rock type of the property is intermediate volcanic rocks. These units have been intruded by dikes of quartz porphyry, quartz-feldspar porphyry and granite. Some of the quartz porphyry dikes have been sheared, and are well mineralized with quartz stringers and veinlets. In the southwest corner of the property, there is a small area of metasediments.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue |
Dec 07, 2005 (K R Kettles) - The auriferous structure is comprised of shear zones in units of quartz porphyry. These shear zones contain quartz veinlets and stringers over widths of up to 1.5 m. Three, and possibly four parallel shear zones are present. The mineralized structure extends for about 600 m in length and averages 60 m in width. The best mineralization was intersected around the 180 m to 210 m level. The number 4 drill hole completed in 1947 returned the best results. Values of 0.38 oz/ton (13.028 g/tonne) Au over 0.98 m, and 0.23 oz/ton (7.886 g/tonne) over 0.76 m have been reported. Other recorded results from different drill holes ranged from 0.01 oz/ton (0.343 g/tonne )Au to 0.07 (2.400 g/tonne) Au.
File - Resident Geologist files AF RL 1947 Heyson #15
Publication Number: AF RL 1947 Date: 1947
Author:
Publisher Name:
Location: Red Lake RGP
File - Resident Geologist files AF RL 1988 Heyson #94
Publication Number: AF RL 1988 Date: 1988
Author:
Publisher Name:
Location: Red Lake RGP
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 505-506 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
File - Resident Geologist's Files, Red Lake
Publication Number: RGF RL Date: 1974
Author: Mykytiuk, B.
Publisher Name:
Location: Red Lake RGP
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