Ontario Geological Survey
Permanent Link to this Record:
MDI42A08NW00141
Record Name(s) | V2 Occurrence - 1988, Gunnex Ltd. - 1960, Stroud Resources Inc. - 1984, Barymin Explorations Ltd. - 1972, Chevron Canada Resources Ltd. - 1986, Pancontinental Mining (Canada) Ltd. - 1981 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Developed Prospect Without Reported Reserves or Resources |
Date Created | 1992-Mar-04 |
Date Last Modified | 2023-Aug-25 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Hislop, Hislop, Hislop
Latitude: 48° 29' 31.45" Longitude: -80° 18' 10.23"
UTM Zone: 17 Easting: 551508.2 Northing: 5371228.7 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 42A08NW
Point Location Description: overburden occurrence
Location Method: Data Compilation
Access Description: A point 4.68 km north and 2.05 km west of the southeast corner of Hislop Township. The auriferous V2 Zone occurrence is in the central part of the northeast quarter of the north half of lot 3, concession III, Hislop Township, about 2.9 km northwest of the village of Holtyre. Access to within several hundred metres of the (overburden covered) occurrence area may be made via all weather north trending Hislop Road 2, located on the common boundary of lots 3 and 4, or an east trending road located on the common.
The area's exploration history is summarized in the report for the Gunnex deposit. (168) MDI42A08NW00104. 1974: Gunnex Ltd. - DD-32-8427 ft. 1980-81: Barymin Explroations and Pancontinental Mining (Canada) Ltd. - ground magnetics, IP and residtiviy, electromagnetic and lithogeochemical surveys; RC sampling; DD-14-1714 m. 1984: Stroud Resources Ltd. - property optioned. 1986-88: Chevron Canada Resources/ Stroud Resources: ground geophysics, geochemical survey; stripping; overburden and diamond drilling, IP survey; resistivity survey
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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KL-1009/63.5321/OM86-6-C-135 | 42A08NW0035 | 42A08NW0035 |
KL-1009/63.5155/OM-87-6-C-027 | 42A09SW0256 | 42A09SW0256 |
63.3930/OM9-PE7-C-80 | 42A08NW0062 | 42A08NW0062 |
63.5342/OM87-4-JV-349 | 42A09SW0255 | 42A09SW0255 |
63.3627 | 42A08NW0075 | 42A08NW0075 |
63.4999/OM86-6-JV-202 | 42A08NW0040 | 42A08NW0040 |
KL-1064/14 | 42A08NW0081 | 42A08NW0081 |
KL-1009/63.5200/OM86-6-P-181 | 42A08NW0007 | 42A08NW0007 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
Metamorphism Grade: Greenschist
Apr 08, 2016 (C Salo) - Geological mapping indicates bedrock in the deposit area is almost entirely glacial drift covered. Bedrock geology and structure in the area are complex and not well understood. Bedrock is interp. to consist mainly of weakly metamorphosed (greenschist or lower metamorphic facies except marginal to large felsic intrusive bodies, where amphibolite grade contact metamorphic aureoles may be developed) subaqueously deposited ultramafic to felsic volc., pyroclastic, and chemical and clastic interflow sedimentary rocks. In places these supracrustal rocks have been intruded by albite syenitic bodies of unspecified size and geometry, aplite dikes, and narrow (gener. no more than tens of metres in width) diabase dikes of the Matachewan swarm which usually strike north. Bedrock stratigraphy is rpted to strike SE, to dip steeply SW, and to face southwest, but Prest has postulated the presence in the area of isoclinal folding, suggesting that semiregional scale descript. of the deposit area's basement structure should be regarded with caution. Bedrock hosting the Creek Zone deposit is interp. by Johnstone and Trowell to be about 2.4 km SW of a relatively narrow Porcupine-Destor Fault Zone (PDFZ) while Jensen .the PDFZ to be much wider and closer to the deposit loc. than this. Bedrock hosting the deposit appears to be either: a) within a distinc. felsic marker horizon loc. near the top of the (Archean) Stoughton-Roquemaure Group which occurs south of the PDFZ and occupies part of the north limb of the east striking and east plunging Blake River Synclinorium; or b) within a lithologically and structurally complex bedrock assemblage which is spatially assoc. with the PDFZ and which is termed by Jensen and Langford the Porcupine-Destor Complex.
Rock Type | Rank | Composition | Texture | Relationship | Intermediate lava flow-unsubdivided | 1 | Andesite | Near |
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Syenite | 2 | Albite Intrusion | Host | |
Terrigenous-Clastic-Unsubdivided | 3 | Clastic Sediments | Host | |
Schist-Unsubdivided | 4 | Sericitic | Near | |
Vein | 5 | Quartz | Host | |
Felsic lava flow-unsubdivided | 6 | Rhyolite, Dacite | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Molybdenite | Economic | Ore | ||||
5 | Galena | Economic | Ore | ||||
6 | Specularite | Economic | Ore | ||||
8 | Hematite | Economic | Ore | ||||
1 | Chlorite | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue | ||||
3 | Fuchsite | Economic | Gangue | ||||
4 | Graphite | Economic | Gangue | ||||
5 | Quartz | Economic | Gangue | ||||
6 | Sericite | Economic | Gangue | ||||
7 | Serpentine | Economic | Gangue |
Apr 08, 2016 (A Wilson) - The highest assays returned from the drilling completed by Chevron were:0.406 oz/t Au over 1 m (DDH P-1); 3.07 oz/t Au over 0.8m (DDH P-21) and 0.955 oz/t Au over 1.0 m in DDH G-25.
Dec 07, 2005 (C Salo) - The V2 Zone occurrence is about 640 m northeast of the Gunnex deposit. It is reported to be: a) geologically similar to the Creek Zone deposit (described elsewhere in this compendium); b) to be spatially associated with the south southeast striking Gibson Fault about 1.86 km south southeast of the Hislop West Mine (also spatially associated with the Gibson Fault and described elsewhere in this compendium); and c) comprised at least in part of anomalously elevated gold tenors associated with visible (coarse grained native) gold (Stroud Resources Ltd. Annual Report 1988 dated May 18, 1989; Stroud Resources Ltd. news release dated June 4, 1989).
Rank | Characteristic |
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1 | Stratiform |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 396.24 |
File - Resident Geologist file KL-2179
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
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:
Map - Precambrian Geology of the Hislop Township Area
Publication Number: M2527 Scale: 1:20,000 Date: 2000
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological Compilation of the Lake Abitibi Area, Abitibi Greenstone Belt
Publication Number: P3398 Scale: 1:100,000 Date: 1999
Author: Ayer J.A., Berger B.R., Trowell N.F.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of Hislop Township
Publication Number: ARV65-05 Page: 38 Date: 1997
Author: Prest V.K.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Mineral occurrences, deposits, and mines of the Black River-Matheson area
Publication Number: OFR5735 Page: 1673-1677 Date: 1990
Author: Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geological Synthesis of the Highway 101 Area, East of Matheson, Ontario
Publication Number: OFR6091 Date: 2003
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
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