Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI000000002070

Record: MDI000000002070

General

Mineral Record Identification
Record Name(s) Central Zone - 1987
Related Record Type
Related Record(s)
Record Status Developed Prospect With Reported Reserves or Resources
Date Created 2017-Mar-03
Date Last Modified 2022-May-17
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Dome, Heyson

Latitude: 51° 0' 57.8"    Longitude: -93° 50' 41.93"

UTM Zone: 15    Easting: 440729   Northing: 5651950    UTM Datum: NAD83

Resident Geologist District: Red Lake

NTS Grid: 52N04SW

Point Location Description: DDH HLD004 from Assessment report 20000014412

Location Method: Data Compilation

Access Description: The Property partly covers the community of Red Lake and is easily accessed, year round via provincial Highway 105 and Highway 618, which transects the southern part of the Property. Various secondary dirt roads and trails provide access to the remainder of the property.



Exploration History

1987-88: Lac Minerals (later Barrick Gold Corp.) carried out geological mapping, geophysical surveys, and drilled 9 DDH totalling approximately 5000 m. 2016: Premier completed 96 DDH totalling 45,881 m; four trenches exposing 6488 m2 were completed with 338 channel samples taken. A phase one 6 sample composite was run in a metallurgical testing. A follow-up phase 2 metallurgical test involved 4 samples for heap leaching potential.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.57108 20000014412 20000014412
27399 20000017046 20000017046

Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Red Lake

Geological Age: Archean  



Geology Comments

Nov 30, 2020 (Andrew Tims) - Gold mineralization is represented by the Central Sector, which hosts the Laverty Dyke. The Central Sector is in the southern part of the Dome Stock where a series of conjugate structures occur within a roughly circular, silicic-altered, pseudo-breccia zone that is enveloped by a broader calcitic-altered zone. The sub-vertical Laverty Dyke strikes north-northwest across the Central Sector, which is characterized by wide-spread gold mineralization. The conjugate structures and their subordinate fracture system are occupied by gold-bearing quartz+/-tourmaline veins and veinlets, typically less than 2 cm wide. Gold is associated with quartz±tourmaline veins in felsic intrusions. These are characteristically small, narrow, laterally extensive, fault-fill and extensional veins, within and proximal to felsic and intermediate intrusions and dykes.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Granodiorite 1 Contains
Vein 2 Quartz Host

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicOre
2ChalcopyriteEconomicOre
3GoldEconomicOre
1QuartzEconomicGangue
2TourmalineEconomicGangue

Mineralization Comments

Nov 30, 2020 (Andrew Tims) - The Central Zone, which hosts the Laverty Dyke, and is characterized by wide-spread gold mineralization. The Central Zone is in the southern part of the Dome Stock where a series of conjugate structures occur within a roughly circular, silicic-altered, pseudo-breccia zone that is enveloped by a broader calcitic-altered zone. The conjugate structures and their subordinate fracture system are occupied by gold-bearing quartz+-tourmaline veins and veinlets. The Laverty Dyke is characterized by widespread persistent mineralization associated with silicification, weakly disseminated sulphides and variably distributed quartz veinlets.


Nov 30, 2020 (Therese Pettigrew) - A hole drilled by Lac Minerals in 1987 returned up to 1.49 g/t Au over 48.7 m and 0.95 g/t Au over 32 m. The ore host is a locally silicified and mineralized Dome Stock Granodiorite. Visible gold is common in glassy-blue quartz veinlets. In intercepts with the typical strong silica alteration with chalcopyrite, occasional visible gold was intersected. The Dome Stock granodiorite remains open to exploration to both the north and east. Central zone highlight intercepts include 0.94 g/t Au - 305.5m incl. 1.61 g/t Au - 122.5m in HLD004, 0.80 g/t Au over 246.7 m (including. 2.16 g/t Au - 25.0 m) in HLD003, 0.98 g/t Au over 118.0 m (including. 3.08 g/t Au - 14.0 m) in HLD005, 0.79 g/t Au over 172.5 m (including 1.25 g/t Au over 50.8 m) in HLD011, 1.06 g/t Au over 93.0 m and 1.04 g/t Au over 10.0 m in HLD012 and 0.84 g/t Au across 101.0 m in HLD030 (Assessment report 20000014412). Drill core from the Central zone shows visible gold in glassy blue quartz-carbonate ± tourmaline ± pyrite ± chalcopyrite veins with silicified, sericitized and/or potassic altered granodiorite. Trace molybdenite has also been observed in drill core. Significant mineralization also occurs within the north-northeast trending Laverty dyke (Assessment report 20000017046).



Mineral Record Details

Classification
RankClassification            
1 Lode (Gold)
Characteristics
Rank Characteristic            
1 Disseminated
Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
Central Zone 2017 Indicated Mineral Resource 31613000 2017 NI 43-101 Technical Report: Hasaga Project p. 95 31,613,000 tonnes @ 0.79 g/t for 803,900 oz contained Au Gold 0.79 Grams per Tonne
Central Zone 2017 Inferred Mineral Resource 23733000 2017 NI 43-101 Technical Report: Hasaga Project p. 95 23,733,000 tonnes @ 0.76 g/t for 582,700 oz contained Au Gold 0.76 Grams per Tonne

References

Publication - Greenstone-hosted Quartz-Carbonate Vein Deposits, in Goodfellow, W.D., ed., Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods. pp. 49-73

Publication Number: Sp No. 5 Date: 2007

Author: Dubé, B. and Gosselin, P.

Publisher Name: Geological Association of Canada, Mineral Deposits Division

Location: GAC Website


Map - Howey-Hasaga area, Dome and Heyson townships, Red Lake area, District of Kenora (Patricia Portion), Ontario

Publication Number: ARM49E Scale: 1:3,600    Date: 1998

Author: Horwood H.C.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Geology, Red Lake greenstone belt, western Superior Province, Ontario

Publication Number: OF 4594 Scale: 1:50,000    Date: 2004

Author: Sanborn-Barrie, Skulski, T; Parker, J

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/215568


Publication - Technical Report: Hasaga Project

Publication Number: 2017 NI 43-101 Date: 2017

Author: Jourdain, V., Langton, J., Ladidi, A.

Publisher Name: MRB & Associates for Premier Gold Mines

Location: SEDAR


MonoMap - Geology of the northern part of Heyson Township, District of Kenora

Publication Number: R056 Page: 37-38  Date: 1968

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Precambrian Geology, Dome Township

Publication Number: OFM0231 Scale: 1:12,000    Date: 1993

Author: Atkinson B.T.

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian Geology, Red Lake

Publication Number: P3227 Scale: 1:50,000    Date: 1993

Author: Atkinson B.T., Stone D.

Publisher Name: Ontario Geological Survey

Location:


Report an Error

We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.


Terms of Use

Please review our Terms of Use agreement for this data product.


Ministry Contact Information

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