Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52N04NE00060

Record: MDI52N04NE00060

General

Mineral Record Identification
Record Name(s) Duluth Red Lake Gold Mines Occurrence - 1987, Balmer Twp #7 Occurrence - 1987
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1997-Jan-11
Date Last Modified 2022-Sep-27
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Balmer

Latitude: 51° 4' 19.66"    Longitude: -93° 41' 22.55"

UTM Zone: 15    Easting: 451686.628   Northing: 5658071.942    UTM Datum: NAD83

Resident Geologist District: Red Lake

NTS Grid: 52N04NE

Point Location Description: Precise/DDH

Location Method: Data Compilation



Exploration History

1945: Duluth Red Lake Gold Mines incorporated to develop the property. Early development work included surface trenching, stripping, geological and geophysical surveys and about 900 m of diamond drilling. 1956 to 1962: 5 holes drilled for a total of 613 m. In 1957 Dickenson Mines owned the property. 1969: Cochenour Willans Gold Mines performed geophysical surveys, and drilled 2 holes totalling 216 m. 1975: Dome Exploration Canada performed ground magnetometer and electromagnetic surveys, and drilled 6 holes totalling 1102.27 m.


Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Red Lake

Geological Age: Archean  

Metamorphism Type: Regional

Metamorphism Grade: Amphibolite



Geology Comments

Dec 07, 2005 (K R Kettles) - The occurrence is situated in an east west striking band of altered 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.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 Quartz Stringers Host
Mafic lava flow-unsubdivided 2 Basalt Adjacent

Lithology Comments

Dec 07, 2005 (K R Kettles) - Occurrence is in an E-W band of basalts which are silicified, carbonatized and are garnitierous and biotite-rich. They are overlain and underlain with sequences of intercalated clastic and chemical sedimentary rocks.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GoldEconomicOre
2PyriteEconomicOre
3PyrrhotiteEconomicOre
1QuartzEconomicGangue
SilicaAlterationSilicification1
CarbonateAlterationCarbonatization2
GarnetAlterationSkarn3

Mineralization Comments

Dec 07, 2005 (K R Kettles) - Anomalous gold values occur in highly silicified units of basalt with up to 25% quartz occurring as thin stringers. Two drill holes #75-1 and #75-2 intersected narrow zones of mineralization. Hole #75-1: 0.40 dwt/ton Au from 116.91 to 117.21 m. Hole #75-2: 0.40 dwt/ton Au from 143.05 to 143.23 m. The intersections were probably from different zones.



Alteration Comments

Dec 07, 2005 (K R Kettles) - The basalts have been silicified, carbonatized, depleted in Na2O, and are garnitiferous. The altered basalts have been described as being brown in color suggesting they also contain appreciable biotite. They have also undergone enrichment in CO2, SiO2, and K2O.




Mineral Record Details

References

Part - Geology of Balmer Township

Publication Number: ARV60-10 Date: 1997

Author: Chisholm E.O.

Publisher Name: Ontario Dept. of Mines

Location:


File - 1976, Resident Geologist's Files, Red Lake

Publication Number: AF RL 1976 Date: 1976

Author: Sanderson, W.L.

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: 157-158  Date: 1987

Author: Durocher M.E., Burchell P.S., Andrews A.J.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Red Lake Resident Geologist District Office