Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI41O15SE00029

Record: MDI41O15SE00029

General

Mineral Record Identification
Record Name(s) Kenty - 1984, Kenty #2 Shaft Veins - 1933, W.G. Atkins - 1984, Atkins - 1951, Emerald Isle - 1986
Related Record Type Simple
Related Record(s)
Record Status Developed Prospect With Reported Reserves or Resources
Date Created 1993-Jul-15
Date Last Modified 2023-Apr-14
Created By
Revised By

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Zinc, Lead, Molybdenum



Location

Township or Area: Swayze

Latitude: 47° 50' 17.03"    Longitude: -82° 36' 30.74"

UTM Zone: 17    Easting: 379636.802   Northing: 5299554.365    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 41O15SE

Point Location Description: Southeast corner of an old two compartment shaft which is now capped.

Location Method: Field Visit with GPS

Access Description: Secondary logging roads which branch off the Dore Main Haul road join up with the old Sultan to Kenty Mine road and lead directly to the shaft.



Exploration History

1931: J. G. and J. L. Kenty - discovery, prospecting, sampling. 1933-34: Kenty Gold Mines - shaft sinking of #2 shaft to 162 m with levels at 88m and 160 m, additional lateral development in 1934, 2255 m ddh. 1936: Brett-Trthway Mines Ltd - test stamp mill operational. 1947: Erndale Mines - 100 tpd mill established on property. 1983: Heron Resources - ground magnetic and self-potential surveys, humus sampling, geological mapping, 15 ddh. 1986-87: Emerald Isle Resources - airborne geophysics, trenching, mapping sampling, 28 ddh (2922.8 m). 1992: 994374 Ontario - leases property, test mining of No 3 vein. 1997-99: Emerald Isle Resources 7 ddh, stripping, trenching, bulk sampling ( 3 tons).


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
T-3117, 63.4914 41O15SE8631 41O15SE8631
T-4474 41O15SE2007 41O15SE2007
2.10363, T-3117 41O15SE0057 41O15SE0057

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Swayze

Geological Age: Neoarchean   Geochronological Age: 2695 +/- 2 MA   Geochron. Age Ref.: OF 3384B

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (S Fumerton) - There are a number of main parallel vein sets which trend 360/48. These veins are the axis for another en-echelon set of veins which trend 052/65. A conjugate pattern is apparent from the distribution of the quartz veins but there is little apparent deformation of the host rocks. The veins are braided with a 'pinch and swell' appearance.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 Vein Quartz Host
Porphyry-unsubdivided 2 Dyke N/A
Lamprophyre-Unsubdivided 3 Biotite N/A
Mafic pillowed flow 4 Basalt Tholeiitic, Pillowed, Pyroclastic N/A
Intermediate lava flow-unsubdivided 5 Andesite Adjacent
Schist-Unsubdivided 6 Adjacent
Vein 7 Quartz Contains
Feldspar Porphyry 8 Feldspar Adjacent

Lithology Comments

Dec 07, 2005 (S Fumerton) - Original Comments are more than 2000 characters. The data cannot be converted, however the data will still be available in Digitial Prospector Database.


Dec 07, 2005 (A Wilson) - (PRECIS OF FUMERTON) The mineralization is hosted in a pillowed Fe tholeiitic basalt intercalated with massive flows and breccia units. Little deformation or alteration is apparent in these rocks away from the mineralized veins and the sequence strikes NW with tops to the SW. Massive mafic units with coarse biotite in the matrix contain quartz feldspar porphyry fragments. This unit is cut by the alteration and veining associated with the gold mineralization. Closer to the mineralized veins, carbonate alteration occurs in a zone up to 2 m wide on either side of the vein. There is a large body of lamprophyre associated with the mineralization. This body has intruded the mafic metavolcanics and is cut by the quartz veins and associated alteration. This unit has also been described as an altered diorite. The mafic metavolcanic rocks are cut by irregular felsic feldspar porphyry dikes, which appear to post-date some of the alteration, but are themselves partially altered. Large bodies of feldspar porphyry with 20-30% subhedral feldspar phenocrysts are found to the south of the veins.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GoldEconomicOre
1PyriteEconomicGangue
2GalenaEconomicGangue
3MolybdeniteEconomicGangue
4SphaleriteEconomicGangue
5TourmalineEconomicGangue
PyriteAlterationPyritic1MediumDisseminated
ChloriteAlterationChloritic2WeakReplacement
HematiteAlterationHematization3WeakReplacement
SericiteAlterationSericitization4Replacement

Mineralization Comments

Dec 07, 2005 (S Fumerton) - Quartz veins which vary from 10 to 20cm occur in zones of strong carbonate alteration up to several metres thick. Parallel to the main veins within the alteration zone there are thin quartz veinlets. Within the main vein there are fractures perpendicular to the vein mineralized with carbonate and more rarely tourmaline. Brecciation of the wall rocks adjacent to the vein is common and the breccia has been infilled with quartz veining which appears to be part of the same phase as the main quartz vein. Fine grained pyrite occurs in trails along hairline joints - veins or along the contact of the quartz veins. In addition local pockets of coarse grained pyrite occurs in the less altered country rock and in the quartz veins. Pyrite typically forms between 5 and 20% of the carbonatized wall rock but locally forms up to 40% of the rock. Coarse subhedral galena is erratically distributed in the quartz veinlet stockwork that cuts the strongly carbonatized wall rock. Though the grains are hosted in the quartz veining the grains tend to be in contact with the vein walls. Molybdenite has been observed as medium grained flakes within hairline fractures within the wall rock adjacent to the veins together with some fine grained disseminated pyrite. Visible gold is erratically distributed in the quartz vein material and locally occurs in 'egg shaped' aggregates with spectacular concentrations of gold. Chalcopyrite, sphalerite, and specularite have also been observed.


Dec 07, 2005 (A Wilson) - There are five main veins in the vicinity of the #2 Shaft (#3, #8, #9, #11, #16 veins). Average gold grades obtained for each of these veins in 1933 were: 3.4 g/t Au over 117cm (#3 Vein); 1.7 g/t Au over 167 cm (#8 Vein); 17.5 g/t Au over 86 cm (#9 Vein); 8.2 g/t Au over 90 cm (#11 Vein) and 2.7 g/t Au over 123 cm (#16 Vein). Channel samples collected by the OGS in 1985 returned values of 0.045 g/t Au over 2 feet; 1.49 g/t Au over 4 feet, 0.415 g/t Au over 4 feet. Grab samples collected by the OGS in 1985 returned values of 24.2 g/t Au from a quartz vein. A muck sample taken by the OGS in 1993 returned values of 3.71 g/t Au and 1.6 g/t Ag. Sludge samples taken by the OGS in 1993 returned values of 2.18 g/t Au and 1.2 g/t Ag, 6.07 g/t Au and 1.2 g/t Au.



Assay Samples

Assay Samples
CommodityAnalytical MethodDigestion Method ResultUnitLimitQualifier
CopperUnknown.0108%
CopperUnknown.0101%
CopperUnknown.0057%
CopperUnknown.0088%
CopperUnknown.0098%
CopperUnknown.0079%
CopperUnknown.0246%
CopperUnknown.0085%
CopperUnknown.0243%
CopperUnknown.0106%
CopperUnknown.009%
GoldUnknown6.07ppm
GoldUnknown2.18ppm
GoldUnknown.96ppm
GoldUnknown3.71ppm
GoldUnknown2.7ppm
GoldUnknown1.17
GoldUnknown.59
GoldUnknown.415
GoldUnknown4.49
GoldUnknown.045ppm
GoldUnknown22.62ppm
GoldUnknown1.73ppm
GoldUnknown73.74ppm
GoldUnknown2.35ppm
GoldUnknown24.2
GoldUnknown3.75ppm
GoldUnknown7.97ppm
LeadUnknown.0845%
LeadUnknown.0147%
LeadUnknown.0063%
LeadUnknown.0256%
LeadUnknown.0169%
LeadUnknown.0139%
LeadUnknown.0072%
LeadUnknown.0072%
LeadUnknown.0098%
LeadUnknown.0978%
LeadUnknown.0109%
MolybdenumUnknown.0007%
MolybdenumUnknown.0008%
MolybdenumUnknown.0006%
MolybdenumUnknown.0008%
MolybdenumUnknown.001%
MolybdenumUnknown.001%
MolybdenumUnknown.0012%
MolybdenumUnknown.0006%
MolybdenumUnknown.0007%
MolybdenumUnknown.0008%
MolybdenumUnknown.0006%
SilverUnknown1.6ppm
SilverUnknown.5ppm
SilverUnknown1.2ppm
SilverUnknown1.2ppm
SilverUnknown1.7ppm
SilverUnknown.7ppm
SilverUnknown.9ppm
SilverUnknown1.9ppm
SilverUnknown16ppm
SilverUnknown.6ppm
SilverUnknown8.1ppm
ZincUnknown.0076%
ZincUnknown.0103%
ZincUnknown.0081%
ZincUnknown.0079%
ZincUnknown.0064%
ZincUnknown.0095%
ZincUnknown.0064%
ZincUnknown.0075%
ZincUnknown.0098%
ZincUnknown.0059%
ZincUnknown.0058%

Mineral Record Details

Classification
RankClassification            
1 Mesothermal
Characteristics
Rank Characteristic            
3 Breccia
2 Stockwork
1 Vein

Mineral Zones - Size and Shape

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Tabular 300 1 160 55 48 N/A N/A

Site Visit Information

Date: Sep 11, 1986

Geologist: J Ireland

Notes: The writer returned to the property with Chris Keech of Placer Development as part of a tour of the area. The Emerald Isle Resources camp was still in place but no workers were on site. A John Deere tire mounted backhoe and a D-6 Caterpillar tractor was also on the property. Considerable stripping and trenching had been completed just north of the No. 2 Shaft on a narrow vein system parallel to, and approximately 20 metres northwest of, the No. 9 vein. All of the trenches were filled with rainwater and the only exposure of this parallel vein was northwest of the shaft. Extensive stripping was also noted at the north end of the Northeast (No 9) vein extension, approximately 350 metres northeast of the No 2 shaft. Two new vein systems have been exposed running parallel to, and approximately 20 and 60 metres east of the Northeast vein. The veins have been traced for approximately 150 metres along trend and have extended the known systems on the Kenty property another 100 metres. The new veins are very similar in width from 5 to 50cm and made up of white-grey glassy quartz and minor rusty carbonate. A new tractor road has been pushed southeast approximately 1,550 feet from the north end of the Northeast vein to a small pond located in the north half of patented claim S.20715. Several trenches have been cut in the hillside along this road but at the time of the visit they were water filled. Stripping has taken place on a small promontory located on the northeast side of the small pond on claim S.20715. The tractor road continues around the north end of the small pond to the site of the No.21 vein located approximately 600 feet east of the previously described zone. No evidence of stripping on this was seen. [ PRECIS ]


Date: Jul 13, 1993

Geologist: S Fumerton

Notes: Together with Bill Yee a visit was made to the property and were met by Mr Nick Bond. Mr Bond was supervising a three man crew stripping overburden and bulk sampling a series of quartz veins. Use was made of a John Deere 450 bulldozer equipped with front end loader and a backhoe together with an air compressor used for drilling and cleaning the outcrop. With this equipment quartz vein material is extracted from the outcrop and stockpiled prior to passing it through a test mill. The direction for blasting, trenching, and pitting is in part controlled by panning results on pulverized samples. There is a 5 ton per day portable mill on site. This is powered by a large portable generator and consists of:- 1) a small jaw crusher fed by the front end loader, 2) a second stage jaw crusher, 3) screens, 4) a ball mill, and 5) a large concentrating riffle shaker-table. The concentrate is shipped off site for processing. Permission was obtained to come back at a later date to sample the various stages from the open cut to the tailings pond.



Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
#9 Vein 1987 Possible 43300 DAVID CONSTABLE (1987) INTERIM EXPLORATION REPORT ON THE KENTY GOLD PROPERTY Gold 4.7 NA
#3 and #9 Vein 1947 Unclassified 335600 THIS IS A 'BACK OF THE ENVELOPE' CALCULATION Gold 1.3 NA

References

Book - Survey of Mines 1948

Publication Number: Page: 141  Date: 1948

Author:

Publisher Name: Financial Post

Location:


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:


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-118  Date: 1985

Author: Rose, D. G.

Publisher Name: Geological Survey of Canada

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


Map - Geological Compilation of the Swayze Area, Abitibi Greenstone Belt

Publication Number: P3511 Scale: 1:100,000    Date: 2002

Author: Ayer J.A., Trowell N.F.

Publisher Name: Ontario Geological Survey

Location:


Part - Statistical review of the mineral industry for 1954

Publication Number: ARV64-01.001 Page: 18  Date: 1997

Author: Arnoldi M.G.

Publisher Name: Ontario Dept. 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: 86  Date: 1979

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

Publisher Name: Ontario Geological Survey

Location:


File - Resident Geologist files 1980, air photos

Publication Number: Date: 1996

Author:

Publisher Name:

Location: Timmins RGP


Part - Geology of the Swayze area

Publication Number: ARV41-03.002 Date: 1998

Author: Furse G.D.

Publisher Name: Ontario Dept. of Mines

Location:


Part - Mines of Ontario in 1933

Publication Number: ARV43-01.002 Date: 1997

Author: Sinclair D.G., Cleland R.H., Cooper D.F., Keeley E.C., Webster A.R.

Publisher Name: Ontario Dept. of Mines

Location:


Part - Geology of the Swayze gold area

Publication Number: ARV43-03.001 Page: 21-25  Date: 1998

Author: Rickaby H.C.

Publisher Name: Ontario Dept. of Mines

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


Part - Mines of Ontario in 1934

Publication Number: ARV44-01.003 Page: 107  Date: 1997

Author: Sinclair D.G., Keeley E.C., Cooper D.F., Weir E.B., Webster A.R.

Publisher Name: Ontario Dept. of Mines

Location:


Part - Horwood Lake area

Publication Number: ARV44-07.002 Date: 1997

Author: Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of Swayze and Dore townships, District of Sudbury

Publication Number: R033 Page: 20-22  Date: 1997

Author: Donovan J.F.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of the Chapleau area, districts of Algoma, Sudbury, and Cochrane

Publication Number: R157 Page: 192-198  Date: 1977

Author: Thurston P.C., Siragusa G.M., Sage R.P.

Publisher Name: Ontario Division of Mines

Location:


Publication - Gold occurrences of Ontario east of lake Superior; Geological Survey of Canada, Memoir 192

Publication Number: GSC Mem 192 Date: 1936

Author: Kindle, E.D.

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/100824


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: 196-201  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


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