Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42A08NW00141

Record: MDI42A08NW00141

General

Mineral Record Identification
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
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

Commodities

Primary Commodities: Gold



Location

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.



Exploration History

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


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
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

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Abitibi

Geological Age: Archean  

Metamorphism Grade: Greenschist



Geology Comments

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.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Intermediate lava flow-unsubdivided 1 Andesite Near
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

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GoldEconomicOre
2PyriteEconomicOre
3ChalcopyriteEconomicOre
4MolybdeniteEconomicOre
5GalenaEconomicOre
6SpeculariteEconomicOre
8HematiteEconomicOre
1ChloriteEconomicGangue
2CarbonateEconomicGangue
3FuchsiteEconomicGangue
4GraphiteEconomicGangue
5QuartzEconomicGangue
6SericiteEconomicGangue
7SerpentineEconomicGangue

Mineralization Comments

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).



Mineral Record Details

Characteristics
Rank Characteristic            
1 Stratiform

Mineral Zones - Size and Shape

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 396.24

References

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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For detailed information regarding this mineral record please contact the Kirkland Lake Resident Geologist District Office