Ontario Geological Survey
Permanent Link to this Record:
MDI000000002076
Record Name(s) | New Dogpaw - 2003 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2017-Apr-21 |
Date Last Modified | 2022-Jan-30 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Dogpaw Lake Area
Latitude: 49° 21' 49.09" Longitude: -93° 52' 55.33"
UTM Zone: 15 Easting: 435957 Northing: 5468255 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F05SW
Point Location Description: precise
Location Method: Based on Assessment
Access Description: Via Dogpaw Lake by boat
2003: Cunniah Lake Inc. compiled information on the property. 2003-4: Endurance Gold Corp. conducted prospecting, geological mapping, sampling, and airborne geophysics and discovered the New Dogpaw and Starlyght showings. 2008: Metals Creek Resources Corp. acquired the property and conducted prospecting and geological mapping. 2013: Metals Creek conducted prospecting and sampling. Refer to Kenora assessment file 2.55671 52F05SW, QQQQ-12, Metals Creek Resources for extensive exploration history of Dogpaw Lake and Flint Lak area.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52F05SW, QQQQ-12 | 20000014323 | 20000014323 |
52F05SW, MMMM-2, 2.27990 | 52F05SE2006 | 52F05SE2006 |
2.7902 | 52F05SW0061 | 52F05SW0061 |
Province: Superior
Subprovince: Wabigoon
Belt: Kakagi-Rowan Lakes
Geological Age: Precambrian
May 16, 2017 (C Ravnaas) - “The Flint Lake Property’s outer boundary incorporates, to the northeast of the Pipestone-Cameron Fault, a portion of the Rowan Lake Volcanics. The Rowan Lake Volcanics consist predominantly of massive and pillowed basaltic flows, with coarser gabbroic portions.” (Kenora AF 52F05SW, QQQQ-11, 2.55671, Metals creek Resources, pg.6).
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 |
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Felsic Tuff | 2 | Felsic Ash Tuff |
May 16, 2017 (C Ravnaas) - The 6.8 meter wide zone exists as a strongly to intensely silicified and sericite altered felsic ash tuff with cleavage related iron carbonate and 2-8% disseminated pyrite. This zone is hosted within a much wider sheared to strongly foliated system of deformation that strikes in a similar direction to the nearby Gauthier Occurrence (1100 dipping 75 0 north). The showing lies 170 meters across strike (southwest) of a theoretical strike extension of the Gauthier Occurrence (Kenora AF 52F05SW, MMMM-2, 2.27990, Cunniah Lake Inc.)
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore |
Aug 28, 2017 (C Ravnaas) - Eight grab samples were collected by Cunniah Lake Inc in 2003 from the New Dogpaw showing returning values from 12 to 23,421 ppb Au. Subsequently seven channel cuts were sawn across the 6.8 meters (AFRI 2.27990, Cunniah Lake Inc.) Metals Creek crab sample DHJ-13-006 assayed 2.07 g/t Au, grab sample DHJ-13-007 assayed 1.849 g/t Au, both samples described as: “New Dogpaw Showing; felsic to intermediate tuff; sericite rich; 3-5% fine pyrite disseminated throughout.” (AFRI 2.55671, Metals Creek Resources, Appendix I).
MonoMap - Geology of the Cedartree Lake area, District of Kenora
Publication Number: R134 Scale: Date: 1976
Author: Davies J.C., Morin J.A.
Publisher Name: Ontario Division of Mines
Location:
Mono - Structural and metallogenetic studies in the Flint-Cameron lakes area, District of Kenora
Publication Number: OFR5682 Scale: Date: 1988
Author: Buck S.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology Kakagi-Rowan Lakes Area
Publication Number: P3594 Scale: 1:50,000 Date: 2007
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
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