Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52N04SW00348

Record: MDI52N04SW00348

General

Mineral Record Identification
Record Name(s) Altura Gold Mines Ltd. - 1936, DST Quality Control Entry - 1997
Related Record Type Simple
Related Record(s)
Record Status Developed Prospect Without Reported Reserves or Resources
Date Created 1997-Feb-08
Date Last Modified 2022-Aug-05
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Fairlie

Latitude: 51° 4' 46.08"    Longitude: -93° 56' 55.81"

UTM Zone: 15    Easting: 433535.003   Northing: 5659090.005    UTM Datum: NAD83

Resident Geologist District: Red Lake

NTS Grid: 52N04SW

Point Location Description: Shaft

Location Method: Data Compilation



Exploration History

1936: Trenching and diamond drilling by Jomac Gold Syndicate. 1937: Altura Gold Mines Ltd. sunk shaft to 85 m and level stations established on the 40 m, 75 and 125 m levels, 125 m of drifting on 75 m level and 450 m of underground drilling. Ceased operations in November 1937.


Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Red Lake

Geological Age: Archean  

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Sandstone 1 Quartzites, Grewackes Adjacent
Siltstone 2 Slate Adjacent
Conglomerate 3 Adjacent
Diorite 4 Diorite Dikes Intrudes
Quartz-Feldspar Porphyry 5 Quartz Porphyry Dikes Intrudes
Lamprophyre-Unsubdivided 6 Dikes Intrudes
Vein 7 Quartz Veins And Lenses Host

Lithology Comments

Dec 07, 2005 (A Mitchell) - The claims are underlain by an NE-SW striking, moderately to vertically dipping, intercalated sequence of slates, quartzites, greywackes and conglomerates. Dikes of quartz porphyry, diorite, and lamprophyre intrude the sedimentary rocks. A 5 m to 12 m wide band of slate, containing lenses of quartzite is the locus for the quartz veins. The quartz is clear to bluish in colour and granular. Tourmaline is present along the margins of the veins.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GoldEconomicOre
2PyriteEconomicOre
3PyrrhotiteEconomicOre
4SphaleriteEconomicOre
5ChalcopyriteEconomicOre
6GalenaEconomicOre
1QuartzEconomicGangue
2TourmalineEconomicGangue

Mineralization Comments

Dec 07, 2005 (A Mitchell) - Work has outlined a zone approximately 25 m long, 2 m wide and extending to a depth of 75 m containing auriferous quartz veins. Most of the zone is comprised of a large quartz vein approximately 20 m long and 2 m wide. The other veins are considerably smaller and pinch out along strike and with depth. The quartz lens is reported to have assayed 0.685 oz/ton at surface and 0.15 oz/ton across 1 m at the 450 m level.



Mineral Record Details

Classification
RankClassification            
1 Hydrothermal
Characteristics
Rank Characteristic            
1 Vein

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Vein

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 25 2 75 45

Site Visit Information

Date: Feb 08, 1997

Geologist: A Mitchell

Notes: N/A



References

Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2

Publication Number: OFR5558 Page: 434-435  Date: 1987

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

Publisher Name: Ontario Geological Survey

Location:


Part - Geology and mineral deposits of the Red Lake area

Publication Number: ARV49-02 Page: 74-75  Date: 1998

Author: Horwood H.C.

Publisher Name: Ontario Dept. of Mines

Location:


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