Ontario Geological Survey
Permanent Link to this Record:
MDI43F03SW00001
Record Name(s) | Kyle Lake No. 5 - 1996, Kwg DDH Dr96-62 - 1996 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2001-Feb-05 |
Date Last Modified | 2022-Oct-06 |
Created By | |
Revised By |
Primary Commodities: Kimberlite, Diamond
Township or Area: BMA 531 852
Latitude: 53° 4' 23.65" Longitude: -85° 15' 43.71"
UTM Zone: 16 Easting: 616425.998 Northing: 5881829.002 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 43F03SW
Point Location Description: exact
Location Method: Based on Assessment
Access Description: Via helicopter from Attawapiskat.
1988: B.P. Resources Canada/Selco - airborne geophysical survey. 1992-93: K.W. G. Resources Inc/Spider Resources Inc./Blue Falcon Mines Ltd. - airborne survey, ground geophysical surveys. 1995-96: KWG Resources Inc. - ground geophysical surveys, 2 DD (684.14 m). 2006: KWG Resources Inc. & Spider Resources Inc. - ground geophysics. 2006: Renforth Resources Inc. - sampling
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-5396 | 20000001565 | 20000001565 |
T-3865 | 43F03SE0001 | 43F03SE0001 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Geological Age: Archean
Oct 20, 2009 (A Wilson) - Proterozoic kimberlites have been found within the Sachigo Subprovince. The distribution of these intrusions appears to be random but restricted to the Sachigo. The age of these intrusions makes them coeval with the Mid continent Rift (Lake Superior Basin) and the tectonic and/or alkalic rock magmatism along the Kapuskasing Structural Zone and the Grenville Front.
Rock Type | Rank | Composition | Texture | Relationship | Lamproite-Unsubdivided | 1 | Lamproite | Host |
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Limestone | 2 | Hanging Wall |
Oct 20, 2009 (A Wilson) - The Kyle No. 5 intrusion has been identifed as a lamproite not a true kimberlite. The drill log identifies it as a diatreme facies rock overlain by limestone and underlain by granitic gneiss. The intrusion is assumed to be Proterozic since it lies beneath Paleozoic rocks and has a similar magnetic expression comparable to those found associated with Proterozoic kimberlite.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Diamond | Economic | Ore |
Oct 20, 2009 (A Wilson) - 35, 6-m samples, weighing a total of 606.5 kg were submitted to Lakefield Research for diamond analysis by causitc fusion. Only one micro diamond, weighing 12,054 oct, was recovered from a sample taken near the middle of the body.
Rank | Classification |
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2 | Diamond |
1 | Diatreme |
Rank | Characteristic |
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1 | Intrusive |
File - Resident Geologist files T-3569
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Known Kimberlites of Eastern Ontario
Publication Number: P3321 Scale: 1:50,000 Date: 1995
Author: Zalnieriunas R.V., Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Kimberlites of the Attawapiskat Area, James Bay Lowlands, Northern Ontario
Publication Number: OFR6019 Page: 28 Date: 2000
Author: Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
Book - KWG Annual Information Form, 2002
Publication Number: KWG info Date: 2003
Author:
Publisher Name:
Location: Timmins RGP files
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-East Sheet
Publication Number: P3598-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
Publication - Press Releases - Renforth Resources Inc.
Publication Number: Date: 2006
Author: Renforth Resources Inc.
Publisher Name:
Location: Timmins RGO files
Publication - Technical Report on the Kyle Kimberlite Project, Porcupine Mining District - prepared for Renforth Resources Inc. and Spider Resources Inc.
Publication Number: NI-43-101 rpt Date: 2007
Author: H. Lahti and B. H. Newton
Publisher Name:
Location: Timmins RGO files
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