Mineral Deposit Inventory for Ontario

Ministry of Energy, Northern Development and Mines

Permanent Link to this Record: MDI000000000152

Deposit: MDI000000000152

General

Mineral Deposit Identification
Deposit Name(s) Kl-35 - 1987
Deposit Status occurrence
Date Created 2006-Oct-05
Date Last Modified 2019-Sep-27
Created By M A Puumala
Revised By T Pettigrew

Commodities

Primary Commodities: gold

Location

Township or Area: North Bay Area

Latitude: 51° 45' 36.23"    Longitude: -88° 32' 10.64"

UTM Zone: 16    Easting: 393973   Northing: 5735469    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 52P15SE

Point Location Description: Location obtained from map in assessment file 52P16SW0002

Location Method: data compilation

Exploration and Mining History

1971: Cominco conducted AEM and MAG surveys. 1986-88: Noramco Exploration Inc. conducted AVLF-EM and MAG surveys, IP, and ddh (including 1 DDH on this occurrence). 2004: prospecting, geological mapping, diamond drilling and assaying by Slam Exploration on claims owned by William E. Brereton.

Assessment Work on File

Assessment Work on File
Office File Number   Online Assessment File Identifier   Online Assessment File Directory  
63.5246     52P16SW0002     Open
2.30147     20000000510     Open

Geology

Province: Superior

Subprovince: Uchi

Belt: Miminiska-fort Hope

Geological Age: Mesoarchean   

Tectonic Assemblage: Unnamed Assemblage Equivalent To Pickle Crow

Structure
Structure Name Scale Strike Dip Trend Plunge
Stratigraphy And Foliation local 45

Geology Comments

10/05/2006 (M A Puumala) - The Keezhik Lake area gold occurrences are located within the northern portions of the Miminiska-Fort Hope Greenstone Belt. This portion of the belt has been interpreted by Stott and Corfu (1991) to be underlain by the rocks of three separate supracrustal rock assemblages. The northernmost assemblage is dominated by mafic volcanic flows containing a banded iron formation marker unit. This assemblage is interpreted to be overlain by a southward facing sequence of massive to pillowed mafic volcanics that also contains a well-defined iron formation marker unit. A third assemblage consisting of mafic volcanics, felsic pyroclastic rocks and a quartz porphyry intrusion overlies the second unnamed assemblage. The Keezhik Lake gold occurrences are located near the boundary between the second and third assemblages. A wide variety of lithologies have been mapped in this area, including mafic metavolcanics, mafic to ultramafic intrusive rocks (gabbro and pyroxenite), banded iron formation, intermediate to felsic pyroclastic rocks with thin interbedded sedimentary layers, and quartz/quartz-feldspar porphyry intrusions (Arnold and MacTavish, 2005). Gold occurrences appear to be hosted within all of these lithologies, with the most significant known occurrence (KL-12) being found in a quartz porphyry stock The Keezhik Lake gold occurrences are located in an area of significant lithologic and structural complexity. The most significant structure that has been mapped in the area is a syncline that is shown by Arnold and MacTavish (2005) to be located immediately to the north of Keezhik Lake. The orientation of stratigraphy and foliation are variable throughout the area and appear to generally parallel the northern margin of the quartz-feldspar porphyry intrusion. A number of faults that cross-cut and offset stratigraphy have also been interpreted to be present throughout the area. The majority of these faults strike approximately north-south and northwest-southeast

Mineral Deposit Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
mafic metavolcanics 1 adjacent
iron formation 2 near
porphyry 3 near
vein 4 quartz-carbonate host

Mineralization

Deposit Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Habit Description
1 pyrite economic ore
2 gold economic ore

Mineralization Comments

09/27/2019 (T Pettigrew) - DDH KL-35 returned 5.01 ppm Au over 0.8 m from chemical metasediments in bedded chert with quartz-tourmaline-carbonate veining, and 2.40 ppm Au over 0.8 m from mafic metavolcanics with shearing and carbonate-quartz veining (Assessment report 52P16SW0002).

Mineral Deposit Details

Deposit Classification
Rank Classification            
1 vein
2 lode (gold)
Deposit Characteristics
Rank Characteristic            
1 vein

References

Publication - Mineral Occurrences and Prospects in the Fort Hope-Winisk Area, p. 92-94

Publication Number: OFR5926    Date: 1995

Author: Mason, J.K. and White, G.D.

Publisher Name: OGS


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Ministry Contact Information

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