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Ontario Geological Survey
Permanent Link to this Record:
MDI52O09SE00005
Record Name(s) | Pickwick - 1936, Tarp Lake E - 1983 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1983-Dec-28 |
Date Last Modified | 2022-Mar-02 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Connell
Latitude: 51° 31' 27.2" Longitude: -90° 2' 34.25"
UTM Zone: 15 Easting: 705134.8 Northing: 5712268.92 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O09SE
Point Location Description: Precise
Location Method: Conversion from MDI
1936: Pickwick Gold Mines Ltd. was organized and carried out prospecting. 1937: Diamond drilling by Pickwick Gold Mines. 1960: Geophysical surveys by Success Mines.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52O09SE-017A | 52O09SE0131 | 52O09SE0131 |
52P12SW0017B1 | 52P12SW0562 | 52P12SW0562 |
52O09SE0046A1 | 52O09SE0060 | 52O09SE0060 |
52O09SE-012A | 52O09SE0407 | 52O09SE0407 |
52O09SW0012 | 52O09SW0511 | 52O09SW0511 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Pickle Lake
Geological Age: Mesoarchean
Dec 22, 2006 (Mark Puumala) - The geology of the Pickle Crow area is described in MDI52O09SE00007.
Rock Type | Rank | Composition | Texture | Relationship | Ironstone-unsubdivided | 1 | Adjacent |
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Quartz Porphyry | 2 | Adjacent | ||
Mylonite/Fault Gouge/Pseudotachylite | 3 | Shear Zone | Contains | |
Vein | 4 | Contains |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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5 | Chalcopyrite | Economic | Ore | ||||
10 | Pyrite | Economic | Ore | ||||
15 | Pyrrhotite | Economic | Ore |
Dec 22, 2006 (Mark Puumala) - The Pickwick occurrence is located in an area of limited bedrock exposure immediately north of the Kawinogans River. Diamond drilling in 1937 by Pickwick Gold Mines (AFRI# 52O09SE0131) is reported to have encountered significant gold mineralization in three diamond drill holes (P-12, 16 and 18). Mineralization was reported to occur in quartz veins within sheared and silicified metavolcanic rocks and banded iron formation. The most significant drill intersections were reported from ddh P-16, where up to 0.1 oz/ton Au was reported over 1.5 m in silicified metavolcanics containing a 4 cm wide quartz vein. The quartz vein is reported to have been mineralized with trace pyrite. This drill hole also reportedly encountered 0.08 oz/ton Au in a 1.2 m wide section of banded iron formation. This iron formation horizon reportedly contained up to 3% pyrrhotite. Early diamond drill results from the Pickwick property reportedly contained higher gold values. However, Thomson (1937) reported that re-assaying of the anomalous intersections returned insignificant gold values, and that the original results for ddh P-1 and 2 should be disregarded.
Rank | Classification |
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1 | Lode (Gold) |
2 | Vein |
Rank | Characteristic |
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1 | Vein |
Part - The Crow River area
Publication Number: ARV47-03.001 Scale: Date: 1997
Author: Thomson J.E.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Scale: Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office