Ontario Geological Survey
Permanent Link to this Record:
MDI000000001099
Record Name(s) | Junction Shear - 2011 |
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Related Record Type | |
Related Record(s) | |
Record Status | Prospect |
Date Created | 2011-Mar-17 |
Date Last Modified | 2022-Jan-30 |
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Revised By |
Primary Commodities: Gold
Township or Area: Moss
Latitude: 48° 29' 55.59" Longitude: -90° 46' 52.17"
UTM Zone: 15 Easting: 663909 Northing: 5374117 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52B07NW
Point Location Description: Located from Noranda assessment work and confirmed with Google Earth
Location Method: Other
Access Description: The showing is located about 120 km west of Thunder Bay and is accessible by a logging road called Swamp Road 16 km west of Kashabowie, going south of Highway 11. The Swamp Road must be followed for 19 km until a left tum on Nelson Lake Road for another 10 km.
1956: Ray Smith and Red Sanderson discovered copper mineralization 137 m northwest of the north western corner ofHamlin Lake. Noranda Mines Limited and Prospector Airways Company Limited jointly optioned 31 claims from Ray Smith north of Hamlin Lake. 1957: Noranda Exploration optioned a 31 claim block from Smith and Sanderson which covered the Ray Smith and Junction Shear showings. 1984: OreQuest Consultants Ltd. obtained 2 samples from 2 of the Noranda trenches over the Ray Smith occurrence which yielded 620 and 10 ppb Au. 1985: Kennco Exploration completed magnetometer and V.L.F.-E.M. surveys,geological mapping and Humus sampling. 1987: Grand Portage Resources completd trenching and and IP survey. 1988: Grand Portage Resources completed a two DDH prograam totalling 284 m. 2004: East West Resources completed geological mapping and prospecting of airborne EM anomaly targets develop from a VTEM survey flown earlier in the year.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52B07NW0042 | 52B07NW0042 | 52B07NW0042 |
25 | 52B07NW0031 | 52B07NW0031 |
52B07NW2010 | 52B07NW2010 | 52B07NW2010 |
2.9890 | 52B07NW0074 | 52B07NW0074 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Shebandowan
Geological Age: Archean
Dec 14, 2016 (Andrew Tims) - Bedrock consists of sheared and altered felsic-intermediate metavolcanics and chert-magnetite iron formation dipping steeply northward. Alteration/mineralization are focused about a series of banded chert magnetite iron formations hosted within intermediate to felsic metavolcanics that have been altered to chloritized quartz porphyritic tuffs and chlorite-sericite schists. Shearing has resulted in a pyrite chert-chlorite-magnetite breccia from highly deformed iron formation.
Rock Type | Rank | Composition | Texture | Relationship | Felsic lava flow-unsubdivided | 1 | Host |
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Ironstone-unsubdivided | 2 | Host |
Dec 14, 2016 (Andrew Tims) - Initial sampling of a gossan zone just north of the Wawiag River - Deatys Creek junction yielded 0.239 and 0.720 oz./ton Au from composite grabs. Trenching returned values up tol 1.44 g/t Au over 4.40 metres and 2.2 g/t gold over 4.0 metres. 8.6 g/t Au over 0.55 meters
MonoMap - Geology of the Moss Lake area, District of Thunder Bay
Publication Number: R085 Scale: Date: 1970
Author: Harris F.R.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Precambrian Geology of the Wye and Hamlin Lakes Area
Publication Number: P2511 Scale: 1:20,000 Date: 2009
Author: Hart T.R., Metsaranta D.-A.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology and Mineral Potential, Greenwater Lake Area, West-Central Shebandowan Greenstone Belt
Publication Number: R296 Scale: Date: 1997
Author: Osmani I.A.
Publisher Name: Ontario Geological Survey
Location:
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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office