Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SE00154
Record Name(s) | Duluth Red Lake Gold Mines DDH#K-69-1 - 1969, DDH K-69-1 - 1969, Kostynuk Group - 1969 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1991-Mar-12 |
Date Last Modified | 2022-May-06 |
Created By | |
Revised By |
Primary Commodities: Gold, Silver
Township or Area: Balmer
Latitude: 51° 3' 53.47" Longitude: -93° 42' 10.97"
UTM Zone: 15 Easting: 450736.63 Northing: 5657271.94 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SE
Point Location Description: DDH K 69-1 in SE corner of Property 13 map P1976A
Location Method: Data Compilation
Access Description: 10 km NE of Red Lake, accessible by road from Balmertown to Nungessor road for 3 km and turning east onto gravel and dirt logging roads.
1945: Duluth Red Lake Gold Mines:surface trenching, stripping, geological and geophysical surveys and about 900 m of diamond drilling. 1956-1962: Dickenson Mines Ltd. drilled 5 holes for a total of 613 m. 1969: Cochenour Willans Gold Mines performed geophysical surveys , and drilled 2 holes totalling 216 m. 1975: Dome Exploration Canada Ltd. performed ground magnetometer and electromagnetic surveys, and completed 6 diamond drill holes totalling 1102.27 m. 2005 Gold Corp completed a 6 hole drill program totalling 1,995 m on the property. The drill results returned low gold values over narrow intervals.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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BLAMG 0311 | 20000013634 | 20000013634 |
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) - The occurrence is situated in an east-west striking band of mafic volcanics which is underlain to the north and overlain to the south by sequences of intercalated clastic and chemical sedimentary rocks. Rock units dip 50 to 60 degs south.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 2 | Quartz-Carbonate | Stringers | Host |
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Mafic lava flow-unsubdivided | 3 | Altered | Contains | |
Terrigenous-Clastic-Unsubdivided | 4 | Intercalated | Intercalated | Adjacent |
Nov 12, 2014 (K R Kettles) - Anomalous gold values occur in zones of altered mafic metavolcanic containing numerous quartz-carbonate stringers and occassional narrow stringers of massive sulphides. Two relatively short, weak anomalies with an associated magnetometer anomaly of 1500 gammas are situated above the anomalous zones.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Galena | Economic | Ore | ||||
2 | Sphalerite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Pyrrhotite | Economic | Ore | ||||
6 | Silver | Economic | Ore | ||||
7 | Gold | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue | ||||
Carbonate | Alteration | Carbonatization | 1 | Unknown | Disseminated | ||
Silica | Alteration | Silicification | 2 | Unknown | Stockwork |
Feb 24, 2012 (K R Kettles) - Anomalous gold values occur in zones of altered mafic metavolcanic containing numerous quartz-carbonate stringers and occassional narrow stringers of massive sulphides. Two relatively short, weak anomalies with an associated magnetometer anomaly of 1500 gammas are situated above the anomalous zones. Assays of core samples from this hole (# K-69-1)returned interesting silver values but only trace amounts of gold. 10 intersections are mention with the following range of assays: 10.37 to 10.74 m - 0.14 opt Ag; 59.96 to 60.60 m - 0.22 opt Ag; 76.25 to 76.86 m - 5.00 opt Ag; 93.21 to 94.43 m - 0.18 opt Ag; 95.65 to 97.39 m - 3.92 opt Ag; 98.39 to 99.31 m - 0.50 opt Ag; 99.77 to 101.26 m - 0.32 opt Ag; 103.55 to 103.85 m - 0.88 opt Ag; 108.12 to 110.41 m - 0.74 opt Ag; 116.05 - 118.10 - 0.60 opt Ag. 2005: Gold Corp completed a 6 hole drill program, best assay returned 1810 ppb Au over 0.3 m.
Dec 07, 2005 (K R Kettles) - The mafic metavolcanics have been silicified and carbonatized, and are locally biotitic and garnetiferous.
File - Red Lake Resident Geologists Files 1969 Balmer #41
Publication Number: AF RL 1969 Date: 1969
Author: Chastko, L.C.
Publisher Name:
Location: Red Lake RGP
Map - Geological series, Balmer Township, District of Kenora (Patricia Portion)
Publication Number: P1976A Scale: 1:12,000 Date: 1978
Author: Pirie J., Grant A.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of Balmer Township
Publication Number: ARV60-10 Page: 44 Date: 1997
Author: Chisholm E.O.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 198-199 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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