Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SW00230
Record Name(s) | Luxor DDH 65-2 - 1965, Martin-McNeeley - 1982 |
---|---|
Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1982-Aug-27 |
Date Last Modified | 2022-Nov-15 |
Created By | |
Revised By |
Primary Commodities: Copper, Gold, Silver
Secondary Commodities: Iron
Township or Area: McDonough
Latitude: 51° 6' 34.84" Longitude: -93° 52' 19.05"
UTM Zone: 15 Easting: 438960 Northing: 5662383 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SW
Point Location Description: DDH 65-2 from map in Assessment report 52N04SW0025
Location Method: Data Compilation
Access Description:
1934: Martin McNeeley Mines Ltd. carrie dout trenching and surface exploration. 1936: Luxor Red Lake Mines was incorporated to acquire the property formerly held by McNeely Red Lake Holdings Ltd. 1937: Trenching and pitting. 1 DDH totalling 84.4 m was drilled on claim KRL 2208. 1962: Luxor Red Lake Mines conducted EM and magnetometer surveys and drilled 3 DDH. 1965: Luxor Red Lake Mines drilled two diamond drill holes totalling 536.1 m. 1981-84: Bluestack Resources Ltd. optioned the property and carried out geophysical, geochemical, and geological surveys.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
14 | 52N04NW0041 | 52N04NW0041 |
OM92-111 | 52N04SW0025 | 52N04SW0025 |
63.4471 | 52N04NW0021 | 52N04NW0021 |
63.4118 | 52N04NW0012 | 52N04NW0012 |
2.4703 | 52N04NW0022 | 52N04NW0022 |
52N04NW0049 | 20000005533 | 20000005533 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Iron Formation | Oxide Facies | Host |
---|---|---|---|---|
Mafic lava flow-unsubdivided | 2 | Adjacent | ||
Quartz-Feldspar Porphyry | 3 | Quartz Feldspar Porphyry | Dikes | Intrudes |
Terrigenous-Clastic-Unsubdivided | 4 | Clastic Sedimentary Rocks | Adjacent | |
Sulphide Ironstone | 5 | Sulphide Facies | Up To 55% Pyrrhotite | Host |
Dec 07, 2005 (K R Kettles) - The occurrence is underlain by a sequence of clastic sedimentary rocks which are overlain by an interlayered sequence of mafic flows and oxide and sulphide facies iron formation. The clastic metasedimentary units have been intruded by several quartz-feldspar porphyry dykes. The area immediately west of the occurrence is underlain by a large feldspar and quartz-feldspar porphyry intrusion. High silver values occur in what appear to be skarn rocks. The skarn rocks consist mainly of oxide and sulphide iron formation which contain appreciable amounts of epidote and garnet.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Gold | Economic | Ore | ||||
2 | Silver | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Pyrrhotite | Economic | Ore | ||||
6 | Magnetite | Economic | Ore | ||||
Epidote | Alteration | Skarn | 1 | Strong | Massive | ||
Garnet | Alteration | Skarn | 2 | Strong | Replacement | ||
Chlorite | Alteration | Skarn | 3 | Strong | Network | ||
Silica | Alteration | Silicification | 4 | Medium | Veins | ||
Carbonate | Alteration | Carbonatization | 5 | Medium | Veins | ||
Tourmaline | Alteration | Tourmalinization | 6 | Medium | Veins |
Oct 31, 2014 (K R Kettles) - Sulphide facies iron formation units contain up to 55% py and po. High silver and copper values have been obtained from several of the sulphide facies iron formation units. One section of drill core 0.7 m in length returned assays of 0.04 oz/ton (1.371 g/tonne) Au, 0.95% Cu, and 0.86 oz/ton (29.485 g/tonne) Ag. A 0.24 m section of core returned assays of 0.06 oz/ton (2.057 g/tonne) Au, 3.50% Cu, and 1.12 oz/ton (38.399 g/tonne) Ag. 1965 Luxor DDH-65-2 returned an assay of 0.04 oz/t Au, 0.95% Cu, 0.86 oz/t Ag over 0.7 m; 0.06 oz/t Au, 3.5% Cu,1.12 oz/t Ag over 0.24 m, 29.32% Fe in skarn (417.8-452.4 ft)
Nov 15, 2022 (Therese Pettigrew) - Timiskaming conglomerates and greywackes are cut by granodiorite and quartz dykes, and quartz veins varying from 1-8 feet in width which contain pyrrhotite, chalcopyrite, pyrite, and small amounts of gold. Malachite and native copper occur in a weathered portion of the outcrop. The best intersection was between 717.7 and 718.5 feet in an inclined hole L-65-2 collared on KRL 2206. This interval, located below lake level on claim KRL 49364, contained narrow stringers of pyrrhotite and chalcopyrite in metasediment with cherty bands. Assays results are 3.50% Cu, 1.12 oz/t Ag, and 0.06 oz/t au. an assay of 29.3% Fe was obtained from 417.8-452.4 feet in siliceous skarn zones containing magnetite (SMDR 00542)
Dec 07, 2005 (K R Kettles) - The metasediments in the area contain many thin quartz-carbonate and quartz-tourmaline veins. The oxide facies iron formation (skarn rocks) have been highly altered, and contain up to 80% epidote, some garnets and chlorite.
Map - Geological series, McDonough Township, District of Kenora (Patricia Portion)
Publication Number: P1240 Scale: 1:12,000 Date: 1977
Author: Pirie J., Sawitzky E.
Publisher Name: Ontario Geological Survey
Location:
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 553-554 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
Part - Gold deposits in the vicinity of Red Lake
Publication Number: ARV44-06.001 Page: 24-25 Date: 1997
Author: Hurst M.E.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology and mineral deposits of the Red Lake area
Publication Number: ARV49-02 Page: 152-153 Date: 1998
Author: Horwood H.C.
Publisher Name: Ontario Dept. of Mines
Location:
We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral record please contact the Red Lake Resident Geologist District Office