Ontario Geological Survey
Permanent Link to this Record:
MDI000000001504
Record Name(s) | Kimberley Quartz - 1995 |
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Related Record Type | |
Related Record(s) | |
Record Status | Prospect |
Date Created | 2012-Oct-17 |
Date Last Modified | 2022-Jul-15 |
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Revised By |
Primary Commodities: Quartz
Township or Area: Kimberley
Latitude: 47° 52' 15.58" Longitude: -80° 36' 21.64"
UTM Zone: 17 Easting: 529463 Northing: 5302037 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 41P15SE
Point Location Description: Field Visit/GPS point by McAuley, J. 1996
Location Method: Data Compilation
Access Description: The property is accessed by travelling north on Hwy 65 from Elk Lake for a distance of 26.6 Km or south from the intersection Hwy 65 and Hwy 66 east of Matachewan for 27.2 Km to a logging road to the ewst. Follow the logging road for 0.3 Km and then turn left (south) and follow a subsidiary logging road for 6.5 Km and turn to the right(west) onto another logging road which leads to the property. The vein traverse this road 0.8 Km from the last turn.
1995, OGS, Geology, Sampling (5 samples), 2001, Oconnor, T.A. Stripping. 2007, Oconnor, T. A. Sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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KL-4942; 2.21446 | 41P15SE2010 | 41P15SE2010 |
KL-5780; 2.35112 | 20000002181 | 20000002181 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Geological Age: Neoarchean
Oct 17, 2012 (Nazha Sabiri) - The claim area is underlain by Neoarchean granodiorite. The quartz begins as a narrow stringer on the flank of the main vein and gradually becomes more massive. Other thins veinlets, veins and stockwork of quartz extending into the granitoid are present and tend to be parallel to the main quartz vein. The vein seems to be continued to the North East in claim 1211565 and to the South West in claims 1206317 and 1206318. Great White Minerals operated a quarry in these claims. Exploration shaft 1.5 m deep was found beside the quartz vein in claim 1211565.
Rock Type | Rank | Composition | Texture | Relationship | Granodiorite | 1 | Foliated To Massive | Host |
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Monzonite | 2 | Monzonite | Host |
Oct 17, 2012 (Nazha Sabiri) - Marginal to the vein, the granitoid exhibits strong shearing with a well developed schistosity. Fine- to- medium grained, massive to weakly foliated granodiorite and quartz manzonite. The quartz veins locally have a vuggy texture and 1% rusty sulphides are locally present. Chloritic and saussuritic thins smears material is also present on some fractures surfaces. Dessiminated iron staining is located along grain boundaries and fractures surfaces , these fractures and joints on the granodiorite are oriented 095/65 and 000/90. Prominent fractures are oriented 130o/90o and 150/90. Porphyritic to glomeroporphyritic mafic dikes are also present north of the quartz vein in the western part of the claim.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Quartz | Economic | Ore |
Rank | Classification |
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1 | Decorative Aggregate |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 400 | 10 |
Mono - An Evaluation of Potential High-Purity Silica Sources: Preliminary Site Investigation, Volumes 1 and 2
Publication Number: OFR5948 Page: 62-63 Date: 1996
Author: McAuley J.B.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Central Abitibi Greenstone Belt: Kapuskasing Structural Zone to the Quebec Border
Publication Number: P3565 Scale: 1:250,000 Date: 2005
Author: Ayer J.A., Berger B.R., Hall L.A.F., Houlé M.G., Johns G.W., Josey S.D., Madon Z.B., Rainsford D.R.B., Trowell N.F., Vaillancourt C.
Publisher Name: Ontario Geological Survey
Location:
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For detailed information regarding this mineral record please contact the Kirkland Lake Resident Geologist District Office