Ontario Geological Survey
Permanent Link to this Record:
MDI42B01SW00011
Record Name(s) | C.E. O'Neil - 1983, Pinecone Point - 1983, O'Neil - 1933, Pinecone - 1982 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1992-Jul-25 |
Date Last Modified | 2022-Nov-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper
Township or Area: Horwood
Latitude: 48° 0' 50.58" Longitude: -82° 20' 5.85"
UTM Zone: 17 Easting: 400446.083 Northing: 5318724.002 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42B01SW
Point Location Description: Series of closely spaced north - south trenches on north shore of small peninsula.
Location Method: Field Visit with GPS
Access Description: The occurrence is located on the west shore of Horwood Lake and access is very easy via boat from a landing at the north end of Horwood Lake.
1933 The ground was originally staked by C.E. O'Neil who was exploring for gold mineralization hosted in a north south quartz vein. The work carried out consisted of extensive pitting and some gold values were reportedly obtained. 1974 Noranda Exploration carried out a detailed Vertical Loop EM and magnetic survey over the showing 1982 Gold Fields Mining Corporation carried out a ground VLF-EM and magnetic survey over the area and defined two northeast trending shear zones. This work was followed up with geological mapping program which defined two zones of carbonate alteration at Pinecone Point and a humus geochemical survey which also identified the same zones. 1987 St Joe Canada drilled six holes to follow up on the work by Goldfields, but their results were generally discouraging.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-2559, 2.4890 | 42B01SE0053 | 42B01SE0053 |
T-3195, 28 | 42B01SE0039 | 42B01SE0039 |
2.6982, T-2559 | 42B01SE0050 | 42B01SE0050 |
2.6980, T-2559 | 42B01SE0049 | 42B01SE0049 |
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
Dec 07, 2005 (S Fumerton) - There are some small folds in the quartz veins in the northern zone. These folds plunge down dip which is at a shallow angle to the north (10 degrees) compared to the reported steep dip to the whole zone.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Vein | Host |
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Mafic lava flow-unsubdivided | 2 | Basalt | N/A | |
Quartz-Feldspar Porphyry | 3 | Adjacent | ||
Vein | 4 | Quartz-Tourmaline | Contains |
Dec 07, 2005 (S Fumerton) - The rocks in the area are predominantly mafic flows which have been intruded by small stocks of diorite and numerous thin felsic sills. Associated with the dioritic rocks are two zones of carbonate alteration with minor quartz veining trending southeast. The southern zone also has some quartz - tourmaline veins and sericite alteration. The northern zone which was examined is hosted in fine grained mafic metavolcanics adjacent to a coarse grained flow.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Gangue | ||||
2 | Chalcopyrite | Economic | Gangue | ||||
3 | Tourmaline | Economic | Gangue | ||||
Tourmaline | Alteration | Tourmalinization | 1 | Weak | Veins | ||
Sericite | Alteration | Potassic | 2 | Replacement |
Dec 07, 2005 (S Fumerton) - Pyrite is disseminated throughout the alteration zones whereas the distribution of chalcopyrite is more irregular and tends to be concentrated into bands together with pyrite. Together both sulphides can form up to 5% of the rock but typically form less than 2% of the rock. The best gold values are associated with zones of increased deformation and alteration combined with quartz stringers but even so the gold values are still less than 1 g/tonne. The northern zone normally consists of a 10 to 20cm banded quartz vein which is very coarse grained but may be up to 1m thick. No sulphides were observed in the vein. In the mafic flows adjacent to the quartz veins pyrite is abundant especially where the veins are folded. This sulphide enrichment extends for 1m from the vein. There are two types of pyrite, a coarser subhedral variety and a finer disseminated anhedral variety.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Gold | Unknown | .03 | ppm | |||
Gold | Unknown | .1 | ppm | |||
Gold | Unknown | .51 | ppm | |||
Silver | Unknown | ppm | BDL | |||
Silver | Unknown | ppm | BDL | |||
Silver | Unknown | ppm | BDL |
Rank | Classification |
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5 | Mesothermal |
Rank | Characteristic |
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5 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Tabular | 50 | 2 | 120 | 90 | N/A | N/A |
Date: Jul 24, 1992
Geologist: S Fumerton
Notes: A set of trenches along northern zone were examined and sampled.
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:
Book - FINACIAL SURVEY OF MINES 1947, P241
Publication Number: N/A Date: 1947
Author:
Publisher Name:
Location: Timmins RGP
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
Part - Geology of the Horwood Lake area
Publication Number: ARV46-02 Page: 29-30 Date: 1997
Author: Harding W.D.
Publisher Name: Ontario Dept. of Mines
Location:
File - Resident Geologist files 1946, air photo
Publication Number: Date: 1996
Author:
Publisher Name:
Location:
MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane
Publication Number: R157 Date: 1977
Author: Thurston P.C., Siragusa G.M., Sage R.P.
Publisher Name: Ontario Division of Mines
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: 105 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: 611-613 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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