Ministry of Energy, Northern Development and Mines
Permanent Link to this Record: MDI52A15SW00009Deposit Name(s) | New Senator-rouyn Ltd - 1966 |
---|---|
Related Deposit Type | None |
Deposit Status | occurrence |
Date Created | 1992-Mar-27 |
Date Last Modified | 2020-Feb-24 |
Created By | Q Unknown |
Revised By | T Pettigrew |
Primary Commodities: molybdenum, copper
Secondary Commodities: silver, tin, tungsten
Township or Area: Dorion
Latitude: 48° 45' 58.02" Longitude: -88° 46' 25.69"
UTM Zone: 16 Easting: 369656 Northing: 5402974 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52A15SW
Point Location Description: Sample 383105 from Assessment report 20000003571
Location Method: data compilation
Sources Map Scale: 1:25 000
Access Description: The property is accessible by highway and logging road by proceeding east on the Trans-Canada Highway 11/17 to the Ouimet Canyon Road, travelling northwest and west for 16.7 km along the Ouimet Canyon Road and several logging roads
1966: New Senator-Rouyn Ltd. conducted mapping, trenching, and sampling. 1984: Golden Tiger Mining Exploration Company Inc. carried out VLF-EM and magnetic surveys, and sampling. 2004-08: K. Fenwick and K. Bjorkman carried out prospecting and sampling. 2008: Magma Metals (Canada) Ltd. optioned the property from K. Fenwick and K. Bjorkman and carried out prospecting, trenching, mapping, and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
52A15/SW-012 | ||
2.7398 | 52A15SW0001 | Open |
2.39561 | 20000003571 | Open |
Province: Superior
Subprovince: Quetico
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship |
---|---|---|---|---|
felsic intrusive | 1 | granite | ||
schist | 2 | |||
pegmatite | 3 | host | ||
vein | 4 | quartz | host |
02/24/2020 (T Pettigrew) - The southern portion of the property is primarily underlain by strongly deformed quartz-biotite schist and gneiss, derived from turbiditic wacke and siltstone. These rocks are crosscut by strongly boudinaged leucogranitic pegmatite, fine- to coarse-grained granite and granodiorite dykes, and very fine to fine-grained pinkish aplite dykes. Strongly deformed, often narrow quartz stringers, veinlets, and veins are very common. The northern portion of the property is underlain by weakly foliated quartz monzonite. All observed rock-types are locally crosscut by north trending, medium- to locally coarse-grained diabase dykes of mid- to late-Proterozoic age (Assessment report 20000003571).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Habit Description |
---|---|---|---|---|---|---|---|
1 | molybdenite | economic | ore | ||||
2 | chalcopyrite | economic | ore |
02/24/2020 (T Pettigrew) - A short distance south of the contact between the metasedimentary rocks and the quartz monzonite there occurs a zone, striking at approximately 260°, where the pegmatite dykes and quartz veins often contain localized concentrations of finely disseminated to coarsely blebby molybdenite and sometimes chalcopyrite. The chalcopyrite is most commonly observed within quartz veins (Assessment report 20000003571). The pegmatites contain visible molybdenum and have returned assays of up to 0.33% MoS2 over 4.3’ at the No. 1 Showing, 0.28% MoS2 over 3.5’ at the No. 2 showing, 0.56% MoS2 over 6’ at the No. 3 showing, 0.30% MoS2 over 4’ at the No. 4 showing, and 1.78% MoS2 and 0.46% Cu over 2’ at the No. 5 showing (Thunder Bay Assessment files). Samples taken by Golden Tiger in 1984 did not return significant gold values. Sample 44 returned 0.125% Mo, 0.08% Cu, and 0.01 opt Ag (Assessment report 52A15SW0001). Samples collected by K. Fenwick and K. Bjorkman returned up to 473 ppm W, 6007 ppm Sn, 0.397 ppm Re, and over 1 % Mo. Samples collected by Magma Metals returned up to 19,200 ppm Mo and 6320 ppm Cu. Sample 312067 returned 34.9 ppm Ag, >10,000 ppm Mo, and 637 ppm Cu. Most samples returned less than 10 ppm Ag (Assessment report 20000003571).
We are continuously updating the Mineral Deposit Inventory. 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 deposit please contact the Thunder Bay South Resident Geologist District Office