Ontario Geological Survey
Permanent Link to this Record:
MDI41O15SE00010
Record Name(s) | McNeely-McCullough - 1984, McNeely-McCullogh - 1931 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1994-Jul-27 |
Date Last Modified | 2023-Mar-28 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Swayze
Latitude: 47° 50' 5.99" Longitude: -82° 37' 52.42"
UTM Zone: 17 Easting: 377931.809 Northing: 5299249.354 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41O15SE
Point Location Description: An old trench towards the eastern end of a series excavated in the thirties.
Location Method: Data Compilation
Access Description: Access is possible via a rough trail which extends from the old Kenty Mine Road to the former Swayze Townsite on the shore of Brett Lake. From a point near the lake, a skidder trail extends north and passes with a half kilometre of the prospect.
1932 Messrs McNeely and McCullough staked ground adjacent to the Kenty discovery and carried out a trenching and stripping program in the search for extensions to the Kenty gold mineralization. A number of narrow low grade showings were reported. 1976 Umex flew a regional magnetic survey and based on this work staked some claims which covered the prospect. No follow-up ground work is on file. 1982 The Canadian Nickel Company flew a regional electromagnetic, magnetic and radiometric survey which covered the prospect. As Caninco did not hold the ground, ground follow-up was directed else where. 1983 Swayze Resources carried out a geological mapping program and located the old trenches. In the following year a number of areas along the trend of the original trenches were stripped and some old trenches were resampled. Assays results varied from 0.1 g/t to 5.9 g/t Au (0.173 opt) and averaged 2.1 g/t. 1990 Messrs Troup and Otton re-evaluated the favourable rocks west of the Kenty Mine. Work consisted of rock, lake, stream, humus, and some till sampling. Except for two anomalous rock samples collected at the old trenches on the prospect (0.16 and 0.48 g/t Au), results for the other geochemical techniques were disappointing.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-1732 / 2.2145 | 41O15NE0012 | 41O15NE0012 |
T-3497 | 41O09NW0076 | 41O09NW0076 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Tectonic Assemblage: Halcrow-Swayze
Geological Age: Neoarchean Geochronological Age: 2700 MA Geochron. Age Ref.: GOO VOL 1
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Vein | Host |
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Mafic lava flow-unsubdivided | 2 | N/A | ||
Mylonite/Fault Gouge/Pseudotachylite | 3 | Shear Zone | Adjacent | |
Vein | 4 | Quartz | Contains | |
Feldspar Porphyry | 5 | Feldspar | Porphyry | Near |
Dec 07, 2005 (S Fumerton) - The mineralization occurs in a series of quartz veins / stockworks hosted in mafic metavolcanics. Other quartz veins and various trenches associated with the prospect generally follow a major contact between a felsic intrusive body to the south and the mafic volcanics but are slightly off-set to the north.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Gangue |
Dec 07, 2005 (S Fumerton) - Pyrite is associated with the auriferous trenches and locally forms up to 20%.
Dec 07, 2005 (A Wilson) - Assays from samples taken at the time of discovery returned low grade values. Swayze Resources resampled the trenches in 1983 and obtained values of 0.1 g/t Au to 5.9 g/t Au and averaged values of 2.1 g/t Au. Samples collected in 1990 from the same trenches returned values of 0.16 g/t Au and 0.48 g/t Au.
Rank | Classification |
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1 | Mesothermal |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | N/A | N/A |
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 41O-121 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
File - Resident Geologist file T-2784
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Swayze and Dore townships, Sudbury District
Publication Number: M2070 Scale: 1:31,680 Date: 1997
Author: Donovan J.F.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology of the Swayze gold area
Publication Number: ARV43-03.001 Page: 25-26 Date: 1998
Author: Rickaby H.C.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane
Publication Number: R157 Page: 188 Date: 1977
Author: Thurston P.C., Siragusa G.M., Sage R.P.
Publisher Name: Ontario Division of Mines
Location:
File - Resident Geologist files 1980, air photos
Publication Number: Date: 1996
Author:
Publisher Name:
Location: Timmins RGP office
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: 86-87 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: 215-216 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
Book - Swayze Township - unpublished GDIF
Publication Number: GDIF Date: 1988
Author: Resident Geologist Staff
Publisher Name:
Location: Timmins RGP office
Map - Geology, Swayze greenstone belt, Rollo Lake, Ontario
Publication Number: OF 3384b Scale: 1:50,000 Date: 1999
Author: Heather, K B; Shore, G T
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/210450
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