Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SW00343
Record Name(s) | Madsen Red Lake Gold Mines Ltd. (Pine Option) - 1987, Pine Option - 1987 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1996-Dec-28 |
Date Last Modified | 2022-Sep-01 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Fairlie
Latitude: 51° 2' 44.24" Longitude: -93° 56' 37.83"
UTM Zone: 15 Easting: 433836.661 Northing: 5655322.059 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SW
Point Location Description: N/A
Location Method: Data Compilation
1930s: Ground was originally staked by persons unknown (Fisher?). Limited prospecting and development. 1969: Ground was optioned to Madsen Red Lake Gold Mines Limited and Silvermaque Mining Limited by C. Fuller Pine of Balmertown who had staked the property earlier. 1970: Trenching, prospecting, EM and magnetometer surveys. 1971: One diamond drill hole completed.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (K R Kettles) - GEOLOGICAL DESCRIPTION: The occurence is located on the west boundry of the Dome Stock and is primarily underlain by augite diorite. To the northwest occur units of chemical metasediments (marble), clastic metasediments (greywackes to arkoses) and intermediate metavolcanics. Iron formation units are interlayered with the clastic sedimentary rocks. Metasedimentary and metavolcanic rocks are intruded by granitic dikes. From geophysical interpretation, the strike of the metasediments and metavolcanics appears to be NE-SW. This direction parallels the contact between the Dome Stock and other units to the northwest. DEPOSIT DESCRIPTION: Little information has been recorded about this occurence, other than the fact that gold seems to be located in units of chemical metasediment (marble). These units contain narrow beds of chert, which may be auriferous, and short sections where magnetite is disseminated. GEOPHYSICAL DESCRIPTION: A strong EM anomaly with an associated magnetic high was delineated northwest of the island. The anomaly is approximately 1300 m long, strikes NE-SW and is open ended to the northeast.
Rock Type | Rank | Composition | Texture | Relationship | Chert | 1 | Marble | Host |
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Sandstone | 2 | Greywackes To Arkoses | Clastic Metasediments | Adjacent |
Intermediate lava flow-unsubdivided | 3 | Near | ||
Ironstone-unsubdivided | 4 | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Magnetite | Economic | Ore | ||||
3 | Pyrite | Economic | Ore | ||||
1 | Carbonate | Economic | Gangue | ||||
Epidote | Alteration | Epidotization | 1 | Weak | Veins | ||
Silicate | Alteration | Silicification | 2 | Weak | Veins | ||
Carbonate | Alteration | Carbonatization | 3 | Weak | Veins |
Dec 07, 2005 (K R Kettles) - Several sections from drill core returned assays of up to 0.07 oz/ton (2.400 g/tonne) Au over 1 m intervals.
Dec 07, 2005 (K R Kettles) - Minor epidote is located in quartz diorite intrusions. Greywackes have been silicified to cherty greywackes. Carbonatization along fracture planes has been observed.
File - Resident Geologist's Files, Red Lake
Publication Number: RGF RL Date: 1971
Author: Harriman, F.G.
Publisher Name:
Location: Red Lake RGP
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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