Ontario Geological Survey
Permanent Link to this Record:
MDI32E04SW00020
Record Name(s) | South Dyke - 1959, Pegmatite - 2 - 1995 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Prospect |
Date Created | 1995-May-12 |
Date Last Modified | 2023-Aug-16 |
Created By | |
Revised By |
Primary Commodities: Lithium
Secondary Commodities: Beryllium, Gallium, Rubidium, Tantalum, Niobium
Township or Area: Steele
Latitude: 49° 1' 47.5" Longitude: -79° 55' 40.17"
UTM Zone: 17 Easting: 578374 Northing: 5431329 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 32E04SW
Point Location Description: Sample from Assessment report 20000016979
Location Method: Data Compilation
Access Description: The property is accessed by the Trans-limit road from Cochrane and a southern branch leading to the former railway station of Eades near the north shore of Lake Abitibi. A 3.8 km bush road from the branch road to Eades leads directly to the property.
1959: Discovered during ODM mapping by S.B. Lumbers. 1962-1963: Prospecting by Canadian Johns-Manville. Three samples, totaling 171 pounds sent to Mineral Science Division of the Federal Department of Mines and Technical Surveys. Analyses identified spodumene, beryl, pollucite and columbite-tantalite. 1971-1974: Prospecting, mapping, stripping, trenching and drilling by L. Darby. 1975: Dex Ltd. evaluated the property for the production of phlogopite to supply paint and electrical industries. 1989-1990: Prospecting and sampling by G. O'Reilly (no assessment work filed). 1991: Prospecting, mapping, ground magnetic survey and sampling by J. Burns. 1996-1998: Prospecting and sampling by G. O'Reilly. Samples were collected by the OGS for evaluation in 1998. 2017: Power Metals drilled 50 DDH totalling 5405.8 m into the Main, North, and South Dykes.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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KL-0644 | 32E04SW0008 | 32E04SW0008 |
2.14451 | 32E04SW0003 | 32E04SW0003 |
2.49595 | 20000006869 | 20000006869 |
2.23394 | 32E04SW2003 | 32E04SW2003 |
Province: Superior
Subprovince: Opatica
Geological Age: Archean
Dec 07, 2005 (D Guidon) - The property is near the contact of the Case Batholith to the north and the Scapa Metasediments to the South. The batholith has a mapped and inferred extent in excess of 5000 square kilometres. It is unkown if this is a single or series of intrusions. The intrusion is mainly quartz monzonite, but near its contacts, it grades to a granodiorite. A wedge of metasediments (Scapa Metasediments) cross Steele Township along the southern contact of the batholith. They vary in thickness from 0.5 km on the west to greater than 5 km on the east. A set of 3 subparallel pegmatite dikes strike obliquely to the batholoith/sediment contact. The maximum known dimensions of the largest dike are 420 m long by 30 m wide. Each of the dikes is complexly zoned.
Rock Type | Rank | Composition | Texture | Relationship | Pegmatite | 1 | Spodumene | Host |
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Granodiorite | 2 | Hanging Wall | ||
Schist-Unsubdivided | 3 | Qtz-Feldspar-Biotite | Metasediment | Near |
Dec 07, 2005 (D Guidon) - The following has been condensed from a report by J. Burns (1991, assessment file KL-3240). The Scapa Metasediments trend in a southeast direction and dip southward between 60 and 70 degress. Bedding varies from crude to well defined with individual beds ranging between 1 and 2 cm in thickness. In the area of the property, the unit is fine grained and schistose. Quartz, eldspar and biotite are the main minerals with occasional garnets. Stuarolite is common in some beds. Granodiorite is the dominant phase of the batholith near its contact. It is grayish-pink, massive, medium to coarse grained and equigranular. The pegamtites are zoned. The border phase is rarely more than 2 m thick and composed of quartz, feldspar and muscovite. The average grain size of the coarse grained zone is 1-2 cm. Spodumene concentrations are greatest in theos zone and may be as hight as 15-20% of the rock. Crystals average 3-7 cm. In the very coarse zone, quartz, feldspar and muscovite range from 2-5 cm. Spodumene crystals are fewer in number but may be 50 cm long and 5-7 cm in diameter. In the quartz core, grain size is in excess of 5 cm and is composed of mainly quartz with feldspar and spodumene. Spodumene crystals are up to 90 cm in length. Property visit by J. Selway The main outcrop of the south dike consists of the following zones: 1. Aplite border zone; 2. Quartz+coarse green muscovite zone with minor oxide minerals and local beryl; 3. Albite+coarse muscovite+quartz zone with local abundant apatite (up to 20 volume %) and minor beryl and oxide minerals; 4. layered aplite with green muscovite and/or garnet, and minor oxide minerals and apatite; 5. K-feldspar+green muscovite+quartz zone; 6. blocky albitized K-feldspar+quartz+beryl (up to 9cm long).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Beryl | Economic | Ore | ||||
2 | Pollucite | Economic | Ore | ||||
3 | Tantalite | Economic | Ore | ||||
4 | Spodumene | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Feldspar | Economic | Gangue | ||||
4 | Muscovite | Economic | Gangue | ||||
5 | Garnet | Economic | Gangue | ||||
6 | Apatite | Economic | Gangue | ||||
7 | Zircon | Economic | Gangue | ||||
8 | Sphalerite | Economic | Gangue | ||||
9 | Pyrochlore | Economic | Gangue | ||||
10 | Molybdenite | Economic | Gangue |
Dec 07, 2005 (D Guidon) - The above minerals were identified in a report by E.H. Nickel of the Department of Mines and Technical Surveys in 1963 (see assessment file KL-0644). Pollucite was found in a coarse pegmatitic sample. Columbite-tantalite was found in both aplitic and pegmatitic phases of the samples submitted. Spodumene is found in all phases. Property visit by J. Selway albite (aplite), quartz, muscovite, K-feldspar, beryl, spessartine garnet, fluorapatite, columbite-tantalite.
Jul 13, 2022 (Therese Pettigrew) - Samples collected by J. Burns in 1991 returned up to 0.24% Li2O, 40 ppm Ta, and 223 ppm Cs (Assessment report 32E04SW0003). Sampling by P. Hermeston returned up to 191 ppm Li, 0.06 ppm Ta, 10.15 ppm Ga, 329 ppm Rb, and 22.1 ppm Cs (Assessment report 20000006869). The Case Lake pegmatite swarm consists of five dykes: 1. North Dyke – 12 m thick and > 100 m strike length; 2. Main Dyke (also known as Central Dyke) – 35 m thick and > 600 m strike length; 3. South Dyke – 10 m thick and > 250 m strike length; 4. East Dyke – 19 m wide and > 1200 m strike length; 5. Northeast Dyke – 10 m wide and > 75 m length. The North, Main and South dykes are hosted by a tonalite laccolith offshoot from the Case Batholith and they strike at 60 to 70° and dip 40 to 60°. Spodumene is absent in the beryl-type South Dyke (Assessment report 20000016979).
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Cesium | Unknown | 223 | ppm | |||
Lithium | Unknown | .11 | % | |||
Tantalum | Unknown | 40 | ppm | |||
Yttrium | Unknown | 270 | ppm |
Rank | Classification |
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1 | Pegmatite |
Rank | Characteristic |
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2 | Layered |
1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Irregular | 250 | 10 |
Date: Jul 28, 1999
Geologist: D Guidon
Notes: Property visited on September 23, 1998 with G. O'Reilly. South dike not eamined
File - Resident Geologist files KL-0668, KL-2653, KL-3240, KL-4462
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Steele, Bonis and Scapa townships, District of Cochrane
Publication Number: M2018 Scale: 1:31,680 Date: 1997
Author: Lumbers S.B.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Burntbush-Detour lakes, Cochrane District
Publication Number: M2453 Scale: 1:100,000 Date: 1982
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of Steele, Bonis, and Scapa townships, District of Cochrane
Publication Number: R008 Page: 45-46 Date: 1997
Author: Lumbers S.B.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Burntbush-Detour lakes area, District of Cochrane
Publication Number: R199 Page: 65-66 Date: 1982
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
File - Res/Reg Property Visit Report KL #165
Publication Number: PV 165 Date: 1980
Author: Lovell, H.L.
Publisher Name:
Location: Kirkland Lake RGP office
Mono - Fertile Peraluminous Granites and Related Rare-Element Mineralization in Pegmatites, Superior Province, Northwest and Northeast Ontario: Operation Treasure Hunt
Publication Number: OFR6099 Date: 2003
Author: Breaks F.W., Selway J.B., Tindle A.G.
Publisher Name: Ontario Geological Survey
Location:
Article - Fertile and Peraluminous Granites and Related Rare-Element Pegmatite Mineralization, Superior Province, Northeastern Ontario
Publication Number: OFR6100.006 Date: 2002
Author: Breaks F.W., Selway J.B., Tindle A.G.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of Field Work and Other Activities, 2001
Publication Number: OFR6070 Page: 23 Date: 2001
Author: Baker C.L., Kelly R.I., Parker J.R.
Publisher Name: Ontario Geological Survey
Location:
Article - The western Abitibi subprovince in Ontario
Publication Number: SV04-01.011 Date: 1997
Author: Jackson S.L., Fyon J.A.
Publisher Name: Ontario Geological Survey
Location:
Journal - Orbicular Rocks: A Review; In: Geological Society of America Bulletin, vol. 77
Publication Number: GSAB.v77 Page: 409 Date: 1966
Author: Leveson, D.J.
Publisher Name: Geological Society of America
Location:
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