Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI41O15SE00023

Record: MDI41O15SE00023

General

Mineral Record Identification
Record Name(s) Kenty K87-1 - 1991
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

Commodities

Primary Commodities: Gold, Silver



Location

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.



Exploration History

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).


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
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

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) - A number of small folds occur in the sedimentary sequence.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Claystone 1 Argillite Graphitic Host
Sandstone 2 Arenite Host

Lithology Comments

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.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicGangue
GraphiteAlterationGraphitic1WeakDisseminated

Mineralization Comments

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.



Mineral Record Details

Classification
RankClassification            
1 Igneous Contact
Characteristics
Rank Characteristic            
1 Disseminated

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Contact

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Unknown 2 N/A N/A

References

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