Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42B01SW00014

Record: MDI42B01SW00014

General

Mineral Record Identification
Record Name(s) Kerr-Addison (Main Showing) - 1983, Lefever - 1948, Kerr-Addison Main Showing - 1960
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1992-Jun-30
Date Last Modified 2022-Nov-03
Created By
Revised By

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Silver



Location

Township or Area: Horwood

Latitude: 48° 1' 44.54"    Longitude: -82° 19' 29.73"

UTM Zone: 17    Easting: 401222.976   Northing: 5320377.088    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 42B01SW

Point Location Description: The point located is a small outcrop above water level at the south end of a grassy flooded area

Location Method: Data Compilation

Access Description: The showing is located 89km west southwest of Timmins and access is possible with a vehicle and a boat via Highway 101 to the Horwood Lake - Groundhog Lake turn-off. From this point an access road to Horwood Lake extends 11km south and then the showing is another 8km boat trip to an island east southeast of Blueberry Island.



Exploration History

1935 The showing was originally staked by P.H. Silams. 1947 H. Logan mapped and sampled the showing. During this work values up to $166/ton were reported. 1948 J. Lefever drilled a number of holes over a three year period and intersected some quartz veining. 1959 J. Lefever drilled additional holes. 1960 Kerr Addison carried out a magnetic survey which included the occurrence and drilled 7 holes. This work returned high gold and silver values over narrow widths and limited lateral extent. 1980 Raise Contracting / Ingamar Exploration carried out a magnetic and VLF-EM survey which covered the occurrence, then subsequently re-examined the surface exposures. 1986 Pelangio Larder Mines carried out a VLF-EM survey over the property. In the next three years Pelangio repeated the VLF survey together with an IP and magnetic survey, and then mapped the property. Following this work two short holes were drilled and 12 auriferous zones were intersected up to 1.5m thick with a maximum grade of 19 g/t over 30cm but otherwise values were less than 5 g/t over 30cm.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-1976, 2.3366 42B01SE0059 42B01SE0059
T-2712, 2.10441 42B01SE0045 42B01SE0045
T-2737, 2.5107 42B01SE0054 42B01SE0054
T-2123, 12 42B01SW8531 42B01SW8531
17, T-2123 42B01SE0069 42B01SE0069
2.11166, T-2712 42B01SE0042 42B01SE0042
30, T-2712 42B01SE0037 42B01SE0037
2.12547, T-2712 42B01SE0035 42B01SE0035

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Swayze

Geological Age: Neoarchean   Geochronological Age: 2700 MA   Geochron. Age Ref.: GOO VOL 1

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (S Fumerton) - To the west of the showing the existence of a major north south fault has been inferred to underlie the axis of Horwood Lake.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 Quartz-Carbonate Vein Host
Diorite 2 Diorite N/A
Mafic Tuff 3 Basalt Tholeiitic Fe, Tuff N/A
Gabbro 4 Gabbro Adjacent
Vein 5 Quartz-Carbonate Contains

Lithology Comments

Dec 07, 2005 (S Fumerton) - The occurrence is hosted in a medium grained diorite which is part of a sequence of Fe tholeiitic flows and tuffs which trend northeast. A strong carbonate alteration zone occurs in outcrop but has not been delineated in drill core and appears to be north of most quartz carbonate veins tested by drilling.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
5PyrrhotiteEconomicOre
10PyriteEconomicOre
15ChalcopyriteEconomicOre
20GoldEconomicOre
25SilverEconomicOre

Mineralization Comments

Dec 07, 2005 (S Fumerton) - Mineralization occurs as disseminated sulphides in a number of parallel quartz carbonate veins. These veins pinch and swell and are known to be up to 50cm thick but normally are up to 10 - 15cm thick. The veins have been traced laterally up to 60m. Typically the gold values are low but a section in one vein has consistently returned values between 14 and 118 g/t.



Assay Samples

Assay Samples
CommodityAnalytical MethodDigestion Method ResultUnitLimitQualifier
GoldUnknown7.78ppm
SilverUnknown.35ppm

Mineral Record Details

Classification
RankClassification            
5 Mesothermal
Characteristics
Rank Characteristic            
5 Vein

Mineral Zones - Size and Shape

Rank: 5       Structure Type: Fault

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Tabular 150 1 100 90 N/A N/A

Site Visit Information

Date: Jun 30, 1992

Geologist: S Fumerton

Notes: The showing has been flooded when the lake was damned. None of the early work is apparent though it would appear than a zone of strong carbonate alteration presently outcropping on a small island to the north east was not drill tested in the past.



References

Map - Horwood Lake, Sudbury District

Publication Number: M2329 Scale: 1:31,680    Date: 1975

Author: Breaks F.W.

Publisher Name: Ontario Division of Mines

Location:


Publication - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario

Publication Number: GSC OF 1087 Date: 1985

Author: Rose, D.G.

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/129999


File - Resident Geologist files 1946, air photo

Publication Number: Date: 1996

Author:

Publisher Name:

Location:


Part - Geology of the Horwood Lake area

Publication Number: ARV46-02 Page: Date: 1997

Author: Harding W.D.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of the Horwood Lake Area, Sudbury District

Publication Number: R169 Page: 48  Date: 1978

Author: Breaks F.W.

Publisher Name: Ontario Geological Survey

Location:


Mono - Gold deposits of Ontario, part 2, part of District of Cochrane, districts of Muskoka, Nipissing, Parry Sound, Sudbury, Timiskaming, and counties of southern Ontario

Publication Number: MDC018 Page: 66-67  Date: 1979

Author: Gordon J.B., Lovell H.L., de Grijs J.W., Davie R.F.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Mineral Prospects of the Swayze Greenstone Belt (Volume 1, Parts of NTS 41 O and Volume 2, Parts of NTS 41 P, 42 A and 42 B)

Publication Number: OFR5912 Page: 605-606  Date: 1995

Author: Fumerton S.L., Houle K.A.

Publisher Name: Ontario Geological Survey

Location:


Book - Horwood Township - unpublished GDIF

Publication Number: GDIF Date: 1990

Author: Resident Geologist Staff

Publisher Name:

Location: Timmins RGP


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