Ontario Geological Survey
Permanent Link to this Record:
MDI52N04NE00016
| Record Name(s) | DDH G-82-2 - 1982, Dickenson Mines Ltd. - 1987, Marshall Red Lake Mines Ltd. - 1987 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 1991-Mar-13 |
| Date Last Modified | 2022-Jun-28 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Bateman
Latitude: 51° 9' 17.63" Longitude: -93° 40' 58.67"
UTM Zone: 15 Easting: 452236.692 Northing: 5667272.014 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04NE
Point Location Description: Point 175m south and 170 m west of # 2 post claim KRL19642 on map P.1569A
Location Method: Conversion from MDI
The claim group was originally held by Marshall Red Lake Mines Ltd. and was staked sometime prior to 1946. 1946: Ground magnetometer survey. 1962: Three holes totalling 518.50 m were drilled on the Marshall Red Lake property. Dickenson Mines Ltd. (Goldquest Exploration) acquired the ground around 1981. 1981: Horizontal loop E.M. survey completed. 1982: Four holes were drilled totalling 479.16 m.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Amphibolite
Dec 07, 2005 (K R Kettles) - GEOLOGICAL DESCRIPTION: The area is primarily underlain by massive and pillowed mafic metavolcanic rocks. Locally, these flows have been sheared, with the shear zones striking approximately N20deg.E. Southeast of the occurrence, iron formation units have been detected by geophysical methods. The shear zones in the area are mineralized with quartz and carbonate veins and minor sulphides, as well as being enriched in biotite. DEPOSIT DESCRIPTION: The occurrence is located in a mineralized shear zone within massive mafic volcanic rocks. The zone is characterized by moderate to strong shearing and weak brecciation with 5 to 10% quartz-calcite veining and minor pyrrhotite and pyrite. The zone has an estimated width of 1-3 m. GEOCHEMICAL DATA: The enrichment in biotite along the shear zones suggests potassic metasomatism.
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz-Carbonate | Veinlets | Host |
|---|---|---|---|---|
| Mafic lava flow-unsubdivided | 2 | Flows | Pillowed To Massive | Adjacent |
| Mylonite/Fault Gouge/Pseudotachylite | 3 | Shear Zone | Host | |
| Ironstone-unsubdivided | 4 | Iron Formation | Near |
Dec 07, 2005 (K R Kettles) - The area is primarily underlain by massive and pillowed mafic metavolcanic rocks. Locally, these flows have been sheared, with the shear zones striking approximately N20deg.E. Southeast of the occurrence, iron formation units have been detected by geophysical methods. The shear zones in the area are mineralized with quartz and carbonate veins and minor sulphides, as well as being enriched in biotite. The occurrence is located in a mineralized shear zone within massive mafic volcanic rocks. The zone is characterized by moderate to strong shearing and weak brecciation with 5 to 10% quartz-calcite veining and minor pyrrhotite and pyrite. The zone has an estimated width of 1-3 m.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Pyrrhotite | Economic | Ore | ||||
| 2 | Pyrite | Economic | Ore | ||||
| 3 | Chalcopyrite | Economic | Ore | ||||
| 4 | Gold | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| 2 | Calcite | Economic | Gangue | ||||
| Biotite | Alteration | Unknown | 1 | Strong | Replacement | ||
| Quartz | Alteration | Silicification | 2 | Weak | |||
| Carbonate | Alteration | Carbonatization | 3 | ||||
| Chlorite | Alteration | Chloritic | 4 |
Dec 07, 2005 (K R Kettles) - MDI1 DATA: GRADE 1982 DDH G-82-2: ONLY LOW GOLD VALUES, HIGHEST 0.07 OPT AU/0.6 M Only low gold values were returned from drill core assays, the highest being 0.07 oz/ton (2.400 g/tonne)Au over 0.6 m.
Dec 07, 2005 (K R Kettles) - The mafic metavolcanic rocks have locally been carbonatized and silicified, and contain abundant biotite and lesser amounts of chlorite.
File - Resident Geologist files AF RL 1981 Bateman #50
Publication Number: AF RL 1981 Date: 1981
Author:
Publisher Name:
Location: Red Lake RGP
Map - Geological series, Bateman Township, District of Kenora (Patricia Portion)
Publication Number: P1569A Scale: 1:12,000 Date: 1978
Author: Pirie J., Grant A.
Publisher Name: Ontario Geological Survey
Location:
File - Resident Geologist files AF RL 1982 Bateman #49
Publication Number: AF RL 1982 Date: 1982
Author: Sannes, D.L.
Publisher Name:
Location: Red Lake RGP
File - Resident Geologist files AF RL 1982 Bateman #66
Publication Number: AF RL Date: 1982
Author:
Publisher Name:
Location: Red Lake RGP
File - Resident Geologist files AF RL 1983 Bateman #61
Publication Number: AF RL 1983 Date: 1983
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: 321-322 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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