Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI000000000900

Record: MDI000000000900

General

Mineral Record Identification
Record Name(s) McFaulds West (McF-06-70) - 2006
Related Record Type
Record Status Occurrence
Date Created 2010-Oct-15
Date Last Modified 2022-Jan-05
Created By N Bennett
Revised By N Bennett

Commodities

Primary Commodities: Copper



Location

Township or Area: BMA 526 863

Latitude: 52° 42' 30.74"    Longitude: -86° 36' 34.88"

UTM Zone: 16    Easting: 526370   Northing: 5839920    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 43D10

Point Location Description: Drill collar located with GPS from 2006 Spider/KWG JV drill program.

Location Method: Based on Assessment

Access Description: Located 30km west of McFaulds Lake; 585km NW of Timmins; 80km east of Webequie; 110km north of Martin Falls. Access to McFaulds Lake camp by fixed wing (float, ski) and then Helicopter to the property.



Exploration History

2006-2008: KWG Resources Inc. - airborne geophysics, ground geophysics, DD-1-300 m. 2011: UC Resources Ltd. - airborne graviometer survey


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.33950 20000001940 20000001940
2.48617 20000006568 20000006568
2.38108 20000002923 20000002923

Geology

Province: Superior

Subprovince: Sachigo

Terrane: North Caribou

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Intermediate lava flow-unsubdivided 1 Contains
Terrigenous-Clastic-Unsubdivided 1 Banded Pyrite-Chert-Tuff Intervals Host

Lithology Comments

Aug 05, 2014 (A Wilson) - This hole cut an intermediate to felsic fragmental succession containing two significant intervals of banded sulphides, between 55 meters and 58 meters as well as one further down the hole starting at 194 meters. Host rocks exhibited sericitic alteration, garnet grains and intermittent presence of sulphides (mostly pyrite) and magnetite. The drill hole terminated in garnet-biotite schist.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
2ChalcopyriteEconomicOre
1PyriteEconomicGangue

Mineralization Comments

Aug 05, 2014 (A Wilson) - An upper massive pyrite band (2.8 m) between 55.6 and 58.4 m corresponds with the location of the northern conductor. A second, narrower (0.46m), sulphide-chert horizon at 194.14 m appears to be the strike extension of a second conductor. Assays ranged from 0.242% Cu over 1.6 m, 0.535% Cu over 1.2 m and 0.615% Cu over 0.2 m


Oct 15, 2010 (N Bennett) - The hole intersected sulphide mineralization that is indicative of distal mineralization to classic VMS style mineralization over 3m from 55.6m to 58.6m averaging 0.384% Cu.



Mineral Record Details

Classification
RankClassification            
1 VMS Base Metal
Characteristics
Rank Characteristic            
2 Disseminated
1 Massive

References

Mono - Mineral Deposits of Northern Ontario, North of Latitude 49 30'

Publication Number: OFR6242 Scale:     Date: 2009

Author: Stott G.M., Josey S.D.

Publisher Name: Ontario Geological Survey


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


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Ministry Contact Information

For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office