Ontario Geological Survey
Permanent Link to this Record:
MDI42A03SE00016
Record Name(s) | O'Connor Claim10247 - 1923, D. Jones Property - 1989, Flinsky Property - 2001, Warford Property - 2011 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2005-Jun-08 |
Date Last Modified | 2023-Mar-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Cleaver
Latitude: 48° 7' 44.52" Longitude: -81° 2' 46"
UTM Zone: 17 Easting: 496569 Northing: 5330643 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 42A03SE
Point Location Description: approximate location of vein
Location Method: Based on Assessment
Access Description: Located in the south-west of Cleaver Township, approximately 40 km south-east of Timmins, the property is reached by the Langmuir and Nighthawk Timber road network.
1924: D. O’Connor - discovery, stripping, sampling, shaft sinking/pitting. 1965: B.W. Lang - ground geophysics. 1989: D. Jones - geological mapping, sampling.1991: Bruce and Beth Durham - line cutting, prospecting, geological mapping; IP, magnetic and VLF-EM surveying; hand and mechanical trenching; 2001-2002: W. Flinsky and N. Pryor - stripping, trenching, prospecting, sampling. 2008: Klondike Silver Corp. - airborne geophysics. 2011-2012: V. Warford - prospecting.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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Kl-1568/63.1868 | 42A03NE0043 | 42A03NE0043 |
KL-5192/2.25136 | 42A03NE2007 | 42A03NE2007 |
KL-6547/2.49487 | 20000006849 | 20000006849 |
KL-6703/2.52814 | 20000007462 | 20000007462 |
KL3245/63.6281/OP91-700/OP91-701 | 42A03NE8452 | 42A03NE8452 |
KL-1322/2.12916 | 42A03NE1030 | 42A03NE1030 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
Mar 09, 2010 (J Suma-Momoh) - No indication of local fold structures. All carbonate and related altered zones strike between N20E and N40E, and dip sub-vertically to as shallow as 55 degrees east.
Rock Type | Rank | Composition | Texture | Relationship | Mafic massive flow | 1 | Tholeiitic Basalt | Massive, Fine- To Medium-Grained; Pillowed. | Adjacent |
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Granitoid-Unsubdivided | 2 | Felsic Dykes | Fine-Grained, Weathered To A Pinkish-Tan Colour; | Adjacent |
Syenite | 3 | Pinkish-White Whethered; Medium-Grained; Massive | Contains | |
Vein | 4 | Quartz | Host |
Oct 08, 2014 (A Wilson) - The original description of the property indicated that there were four, pyrite-bearing quartz vein systems striking 035° and dipping steeply west.
Mar 09, 2010 (J Suma-Momoh) - More than 70 % of outcrops located in the area are basaltic in composition. The mafic volcanics vary from medium green, chloritic and slightly soft, to dark green-black, slightly silicified to amphibolitized. Pillow shapes indicate a north to north-east strike, with tops facing south-east; they average 30 cm thick by 60 to 80 cm in length. These rocks are intruded by a variety of felsic intrusives and late diabase dykes.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic And Alteration | Gangue | Pyritic | 1 | Unknown | Disseminated |
1 | Gold | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Bornite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Gangue | ||||
3 | Arsenopyrite | Economic | Gangue |
Oct 08, 2014 (J Suma-Momoh) - At least 38 samples (outcrop, grab and trench samples) have been assayed. Only one (sample OP-15: hematite-bearing, reddish-altered, chloritic shear material) returned 0.046 oz/t. At a distance of about 32 km northwest from the given UTM co-ordinates, a large northeast trending quartz vein occurs; visible gold has been found within the vein. About 30 m from the northern tip of the vein is a shaft, and along the strike of the quartz vein and shaft are at least four trenches.
Oct 08, 2014 (J Suma-Momoh) - Alteration within the mafic volcanic rocks seems to be confined to north-northeast trending zones, several metres long and several meters wide. These zones consist of (a) massive, moderate to strongly carbonatized, with local silicification, disseminated pyrite mineralization, minor green mica, and frequent quartz stringers and (b) sheared zones with carbonate, chlorite, sericite, abundant disseminated pyrite, minor green mica and sub-parallel quartz veins and lenses that swell to widths of several meters in places.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Gold | Unknown | .046 | oz/t |
Rank | Classification |
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1 | Vein |
Rank | Characteristic |
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1 | Vein |
File - Resident Geologist file KL-2144
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Precambrian Geology, Cleaver and Hincks Townships
Publication Number: OFM0236 Scale: 1:20,000 Date: 1994
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Part - Notes on gold in McNeil and other townships
Publication Number: ARV33-03.003 Page: 39-40 Date: 1998
Author: Hopkins P.E.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Peterlong Lake
Publication Number: M2345 Scale: 1:50,000 Date: 1978
Author: Pyke D.R.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of the Peterlong Lake area, districts of Timiskaming and Sudbury
Publication Number: R171 Date: 1978
Author: Pyke D.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Precambrian Geology of McNeil, Robertson, Hincks and Cleaver Townships
Publication Number: OFR5931 Page: 61 Date: 2002
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Matachewan Area, Abitibi Greenstone Belt
Publication Number: P3527 Scale: 1:100,000 Date: 2003
Author: Ayer J.A., Trowell N.F., Josey S.D., Nevills M., Valade L.
Publisher Name: Ontario Geological Survey
Location:
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