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Ontario Geological Survey
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MDI52B09SE00029
| Record Name(s) | Creek Zone - 1986, Jalna Resources West - 1984, QUARTZITE Mine - 1896 |
|---|---|
| Related Record Type | Partial |
| Related Record(s) | |
| Record Status | Prospect |
| Date Created | 1991-Mar-23 |
| Date Last Modified | 2024-Aug-13 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver
Township or Area: Duckworth
Latitude: 48° 31' 14.2" Longitude: -90° 2' 41.56"
UTM Zone: 15 Easting: 718200 Northing: 5378384 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52B09SE
Point Location Description: General
Location Method: Data Compilation
Access Description: Access to the property is relatively simple, from Highway #11, enter the Shebandowan turn-off and keep going on the paved road leading to the former Inco Shebandowan Mine. About 2 kilometres from the highway, a main logging gravel road, the Duckworth road, heading south, gives a good access to the claims.
see MDI52B09SE00029
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2012889 | 52B09SE0011 | 52B09SE0011 |
| 2.7577 | 52B09SE0045 | 52B09SE0045 |
| 22 | 52B09SE0016 | 52B09SE0016 |
| 2.12580 | 52B09SE0015 | 52B09SE0015 |
| 63.4618 | 52A12SE8102 | 52A12SE8102 |
| 2.8204 | 52B09SE0040 | 52B09SE0040 |
| 20000021037 | 20000021037 | |
| 20000021480 | 20000021480 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Shebandowan
Geological Age: Archean
Aug 18, 2016 (Andrew Tims) - The old ,Quartzite mine, a long known gold prospect consisting of auriferous, siliceous, pyritic schist which isexposed on the shores of Gold Creek very complex due to episodes of fracturing, brecciation, veining, and redeposition of breccia as well as several stages of volcanism and magmatic intrusion, all of which occurred before the superposition of a strong, penetrative, steeply plunging, stretching lineation and minor late tectonic adjustments. The original lithology was a pyroclastic or volcaniclastic unit. The most intensely sericitized rocks in this zone occur as septa of lineated sericite schist within and surrounding fractured tourmaline-quartz alteration zones.
| Rock Type | Rank | Composition | Texture | Relationship | Felsic lava flow-unsubdivided | 1 | Host |
|---|
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Pyrite | Economic | Ore |
Aug 18, 2016 (Andrew Tims) - A base metal bearing quartz vein reported values up to 35.65 g/t Au (1.04 oz/t) and 295 g/t Ag (8.6 oz/t). The vein, which is described in the section on mineralization, was intersected at a depth of 18 meters below surface, but contained only 0.77 g/t Au over l meter.
Mono - Property visits and reports of the Atikokan economic geologist, 1979-1983, Atikokan geological survey
Publication Number: OFR5539 Page: 208 Date: 1985
Author: Schnieders B.R., Dutka R.J.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geological setting of gold mineralization in the western part of the Shebandowan Greenstone belt, District of Thunder Bay, northwestern Ontario
Publication Number: OFR5636 Date: 1987
Author: Chorlton L.B.
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