Ontario Geological Survey
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MDI52N04NW00013
| Record Name(s) | Harvey J Showing - 1991 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 1991-Mar-11 |
| Date Last Modified | 2022-Jun-28 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: McDonough
Latitude: 51° 8' 19.54" Longitude: -93° 48' 56.38"
UTM Zone: 15 Easting: 442936.708 Northing: 5665572.036 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04NW
Point Location Description: N/A
Location Method: Conversion from MDI
Prior to 1936: The property was held by the Prospector's Investment Group. 1936: C.Harvey acquired the claims(?). Surface work.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Amphibolite
Dec 07, 2005 (K R Kettles) - GEOLOGICAL DESCRIPTION: The occurrence is underlain by a thick sequence of mafic metavolcanic flows. The flows vary from massive and coarse grained to pillowed. Stratigraphic tops are to the west. Foliation strikes NE-SW and dips approximately 80 deg. southeast. A thick unit of metasedimentary rocks overlies the mafic volcanics. The basal part of the sedimentary sequence is primarily composed of garnetiferous conglomerate. DEPOSIT DESCRIPTION: A quartz vein striking S34 deg. E and dipping 15 deg. to 60 deg. to the west hosts the gold mineralization. The vein has been exposed over a length of 27 m.
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz Vein | Host |
|---|---|---|---|---|
| Mafic lava flow-unsubdivided | 2 | Flows | Massive To Pillowed | Adjacent |
| Conglomerate | 3 | Conglomerate | Garnetiferous | Adjacent |
Dec 07, 2005 (K R Kettles) - The occurrence is underlain by a thick sequence of mafic metavolcanic flows. The flows vary from massive and coarse grained to pillowed. Stratigraphic tops are to the west. Foliation strikes NE-SW and dips approximately 80 deg. southeast. A thick unit of metasedimentary rocks overlies the mafic volcanics. The basal part of the sedimentary sequence is primarily composed of garnetiferous conglomerate. A quartz vein striking S34 deg. E and dipping 15 deg. to 60 deg. to the west hosts the gold mineralization. The vein has been exposed over a length of 27 m.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| Garnet | Alteration | Hydrothermal | 1 |
Dec 07, 2005 (K R Kettles) - MDI1 DATA: GRADE: ASSAYS UP TO 0.03 OPT AU FROM VEIN A quartz vein striking S34 deg. E and dipping 15 deg. to 60 deg. to the west hosts the gold mineralization. The vein has been exposed over a length of 27 m. Assays of up to 0.03 oz/ton (1.029 g/tonne) Au have been reported from the vein.
Dec 07, 2005 (K R Kettles) - The conglomerate in the area is garnetiferous.
File - Resident Geologist files AF RL 1947 McDonough #15
Publication Number: AF RL 1947 Date: 1947
Author: Thompson, R.
Publisher Name:
Location: Red Lake RGP
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 576 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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