Ontario Geological Survey
Permanent Link to this Record:
MDI41O15SE00023
Record Name(s) | Kenty K87-1 - 1991 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1993-Jul-09 |
Date Last Modified | 2022-May-09 |
Created By | |
Revised By |
Primary Commodities: Gold, Silver
Township or Area: Rollo
Latitude: 47° 50' 53.57" Longitude: -82° 37' 21.19"
UTM Zone: 17 Easting: 378611.915 Northing: 5300704.43 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41O15SE
Point Location Description: Collar for hole K84-1 transferred from a company grid map onto a 1:50,000 topographic map
Location Method: Data Compilation
Access Description: Access to the area is via the old Kenty Mine which is at the end of a gravel road which branches off the Dore Main Haul road 60km south of Highway 101. From the Kenty Mine a kilometre long winter trail has been established to the general area of the drill hole.
Circa 1930s A number of old exploration pits and trenches occur in the general area, presumably excavated during the general activity following the discovery of the Kenty Mine. 1972 Claw Lake Molybdenum Mines flew a magnetic survey over a number of claim blocks, one of which included this showing. No follow up work was reported. 1976 Umex commissioned a regional airborne magnetic survey which covered the area but no ground follow-up was carried out in the vicinity of the showing. 1983 Kenty Resources carried out a soil geochemical survey (Au, Ag, Cu, and Zn) following the release of a government airborne geophysical survey. A number of anomalous values in excess of 1 g/t Au were obtained in this survey. This work was combined with geological mapping and IP geophysical surveying and a number of targets were drill tested, 463m in 5 holes. One hole from this program intersected a number of intervals greater than 1 g/t Au over a 20m interval. 1985 Kenty Resources together with a number of other companies commissioned an airborne magnetic and VLF electromagnetic survey which covered the area. This was followed up two years later with another small drill program ( 472m in 7 holes) and an IP geophysical survey on the western part of the property. Results of the second drill program were not encouraging.2009 Red Pine Exploration Inc. performs an aerial electromagnetic, aerial magnetic and aerial radiometric surveys (T-5962 / 2.42363). 2010 Red Pine Exploration performs an aerial electromagnetic, induced polarization and aerial magnetic surveys (T-6230 / 2.46831).
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-1732 / 2.2145 | 41O15NE0012 | 41O15NE0012 |
T-2731 / 2.6132 | 41O15SE0023 | 41O15SE0023 |
T-2731 / 2.6434 | 41O15SE0021 | 41O15SE0021 |
T-5962 / 2.42363 | 20000000248 | 20000000248 |
T-6230 / 2.46831 | 20000006503 | 20000006503 |
T-2157 / 2.736 | 41O16SE0031 | 41O16SE0031 |
T-1732 | ||
T-2731 / 2.6471 | 41O15SE0022 | 41O15SE0022 |
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) - A number of small folds occur in the sedimentary sequence.
Rock Type | Rank | Composition | Texture | Relationship | Claystone | 1 | Argillite | Graphitic | Host |
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Sandstone | 2 | Arenite | Host |
Dec 07, 2005 (S Fumerton) - The mineralization is hosted in an argillaceous arenaceous sequence of rocks. The sediments are bedded on a metre scale with a number of graphitic slip planes. The sedimentary sequence is about 500m thick and separates mafic volcanics to the south from a narrow lens of felsic volcanics to the north. There are a number of small mafic dykes that cut the sedimentary sequence and one is near the reported mineralized interval.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Gangue | ||||
Graphite | Alteration | Graphitic | 1 | Weak | Disseminated |
Dec 07, 2005 (S Fumerton) - Pyrite occurs in scattered seams and disseminated euhedral grains forming up to 10% of the rock. Locally there is a stockwork of small quartz carbonate veins within the graphitic argillite. Lower gold values are generally associated with reduced sulphide concentrations. Near the contacts of a mafic dykes there may be an increase in the gold content. Minor silver values are associated with the gold mineralization.
Dec 07, 2005 (A Wilson) - Assays reportedly ran 0.89 g/t Au and 0.91 g/t Ag.
Rank | Classification |
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1 | Igneous Contact |
Rank | Characteristic |
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1 | Disseminated |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 2 | N/A | N/A |
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:
Core - Resident Geologist Core Library
Publication Number: Drill Core Date: 1996
Author:
Publisher Name:
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: 192-193 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
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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