Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI41P12SW00049

Record: MDI41P12SW00049

General

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Molybdenum, Silver

Location

Township or Area: Chester

Latitude: 47° 33' 22.2"    Longitude: -81° 55' 30.34"

UTM Zone: 17    Easting: 430402.575   Northing: 5267386.691    UTM Datum: NAD83

Resident Geologist District: Timmins

NTS Grid: 41P12SW

Point Location Description: Head frame on shaft.

Location Method: Field Visit with GPS

Access Description: Access to the shaft is easy from Highway 144 by taking the Mesomikenda Lake Road to the lake of the same name then an old mine access road leads from the lake to the mine around the Three Duck Lakes. Alternative access is possible from the Sultan Industrial Road in the south via the Chester Twp logging road. From this road tertiary logging roads connect with the old mine road west of the shaft.

Exploration History

1930: Three Ducks Syndicate - prospecting. 1931: Cominco - resampling. 1932: Three Ducks Syndicate - diamond drilling. 1934: Martin Syndicate - prospecting. 1935-37: Young Shannon Gold Mines Ltd. - stripping, trenching, diamond drilling, bulk sample from an open cut, inclined shaft sunk with underground development. 1946: Young Shannon Gold Mines Ltd. - diamond drilling. 1965: Gogama Gold Mines Ltd. - geological reconnaissance, ground VLF-EM and magnetometer survey. 1973: Park Precious Metals Inc. - IP survey. 1975-79: Canadian Crest Gold Mines Ltd. - property development, underground rehabilitation. 1984-87: Young Shannon Gold Mines Ltd. - VLF-EM and IP surveys, diamond drilling (62 ddh - 7850 m), dewatering of workings. 1986: Westport Resources Inc. – IP, Samp, DD, GL. 1997: Young Shannon Gold Mines Ltd. - Drilling, assays 2002: Young Shannon Gold Mines/1478837 Ontario Inc.- Drilling. 2005: Young-Shannon Gold Mines, Limited - DD - 5 - 1295m, IP (T-5510). 2010: Trelawney Mining and Exploration Inc performed a diamond drilling campaign which resulted in a 43-101 report covering the area southwest of Côté Lake. 2010: Trelawney Mining and Exploration Inc. – AEM, AMag. 2015: IAMGOLD corp. completed 3 diamond drill holes totaling 1,025m along with assaying and analyses. 2018-2019: IAMGOLD Corp. completed 23 diamond drill holes totaling 8663.78, extensive assaying and analyses, and geological surveys and mapping. 2019-2020: IAMGOLD Corp. completed 33 drill holes, totaling 13,735m, and assaying and analyses.

Assessment Work on File

Geology

Province: Superior

Subprovince: Abitibi

Terrane: Wawa-Abitibi

Belt: Swayze

Geological Age: Neoarchean   Geochronological Age: 2740 MA   Geochron. Age Ref.: GSC OF 3384A

Geology Comments

Dec 07, 2005 (S Fumerton) - The mineralization is hosted within a northeast trending shear zone. Within this shear there are a complex set of quartz sulphide veins - veinlets which have reportedly been deformed. The sulphide veins and quartz-sulphide veins also contain rounded fragments (milled) of quartz set in a fine to medium grained matrix. The matrix may be secondary quartz or massive sulphides. All quartz veins are fragmented.

Lithology

Lithology Comments

Dec 07, 2005 (S Fumerton) - Massive medium grained granodiorite to leuco granodiorite is the main lithological unit in the area. Other phases present are dioritic xenoliths, altered shear zones and quartz, carbonate, sulphide veins. Chlorite alteration is the most widespread within the shear zones and is more strongly developed where the shear zones cut through dioritic phases. Other alteration minerals include disseminated biotite, disseminated pyrite and veins of hornblende. Sericite and carbonate alteration has also been reported. The biotite occurs in both the dioritic and granodioritic phases as well as in quartz veins. Hornblende alteration - recrystalization occurs in small veinlets (<5mm) where the chlorite alteration is strong. Pyrite alteration is disseminated and variable in intensity though generally declining away from the shear zone axis.

Mineralization

Mineralization Comments

Dec 07, 2005 (S Fumerton) - Some very fine grained quartz veins as well as very coarse quartz veins occur in swarms within the shears. Individual veins are up to 20cm thick. Typical these quartz and associated sulphide veins and veinlets occur discontinuously along shears. In addition there is a 5m wide zone of sparsely disseminated sulphides within granodiorite adjacent to the mineralized veins. Molybdenite typically occurs in the sheared wall rock adjacent to the veins as relatively large flakes in the plane of the foliation. Visible gold has been reported in 'blebs' within the veins but gold mineralization is also associated with the disseminated sulphides in the shear zones adjacent to the veins. The mode of occurrence for the other minerals reported present in the deposit is unknown though the scheelite and tourmaline have only been found in trace amounts. N.B. The reported grade was derived from a selectively mined underground bulk sample whereas the strike length quoted refers more to the length of the shear zone which contains discontinuous mineralization. There is also some reference to three hanging wall and one footwall zones associated with the main mineralized zone.

Dec 07, 2005 (A Wilson) - At the time of discovery assays up to 85 g/t Au and 20 g/t Ag were obtained. One sample collected from the #20 Vein by the Martin Syndicate returned a value of 570 g/t Au. A 7 kg bulk sample with visible gold, collected by Young Shannon Gold Mines returned a value of 30 g/t au, 1.7 g/t Ag. An average grade of 12 g/t Au across 1.2 m was obtained during diamond drilling conducted by Young Shannon in 1937. Grab samples collected in 1978 returned values of 1.7 g/t au; 0.34 g/t Au; 6.17 g/t Au; 2.06 g/t Au.

Oct 20, 2022 (Sheree Hinz) - The Gosselin deposit is located approximately 1.5km northeast from the Côté deposit. Mineralization lies within the hydrothermal breccia, diorite breccia, and tonalite units. Both the Gosselin deposit and the Côté deposit are classified as intrusion related disseminated gold deposits.

Assay Samples

Mineral Record Details

Mineral Zones - Size and Shape

Rank: 2       Structure Type: Breccia

Rank: 1       Structure Type: Shear

Site Visit Information

Date: Jul 28, 1954

Geologist: W Savage

Notes: Geo Moody, field geologist for N.A. Timmins Explorations Ltd placed a prospector and helper, W. Hyland and R. Auberton, in Chester township early in June 1954 and paid them a visit on July 27th. The writer flew in from Gogama by Department of Lands and Forests plane and joined Moody and his party on July 28th. The N.A. Timmins camp was located on the south shore of the southeast bay of the north lake of the Three Ducks Lakes. The shaft is located near the shore of the south bay of the west arm of the north lake, about 600 feet southeast of the outlet from Cote Lake, on claim S-19971. The three foot wide quartz vein on which the shaft was sunk can be seen in old trenches east and west of the shaft. (The Three Ducks Syndicate's No.4 showing, not included in Laird's reports). In the west trench the vein strikes N70E and dips 60 to 70 to the south. It occurs on the contact between white to grey weathering granite (alaskite?) to the north and biotite schist to the south. The shaft was sunk on the vein and is inclined 70 to the south. It appears to have run out of the vein since the dump is predominantly rock. The hanging wall rock is coarse crystalline hornblendite. [ PRECIS ]

Date: Dec 07, 1977

Geologist: L Tihor

Notes: A one day visit was made to the Erana Mines Limited gold prospect in west-central Chester Township. The writer was accompanied by Paavo Kivsto, District Mining Engineer, and Clarence Frost, Mine Safety Inspector. The property is owned by Ed. Blanchard of Sudbury. But, at the time Blanchard was not available and we were given permission to examine the property by Ron Dillabough, general foreman. We found one shaft with levels at 100 and 200 feet. The 200 foot level was inaccessible due to flooding. It appears that the 'Keewatin volcanics' are hydrothermally altered portions of the granodiorite flanking the shear zone. The mineralization zone itself, averaging about 2m in width is a complex zone of shearing and brecciation with myriad small veinlets of calcite, quartz and sulfides. There are occasionally distinct veins up to 50cm wide consisting of quartz or calcite or a combination of these with or without sulfides. These veins parallel the plane of shearing and strike N80E and dip 50S. The sulphides are predominantly pyrrhotite, with minor amounts of chalcopyrite and pyrite. Although the assessment files are generously sprinkled with reports of very high gold assays and visible gold, no v.g. was found during this visit. [ PRECIS ]

Date: Jun 30, 1980

Geologist: L Lutha

Notes: The principal American financiers for Canadian Crest Gold Mines have suspended operations in June at their property in Chester Township pending an investigation. The Resident Geologist accompanied Walter Hayduk and Stan Barron from New Jersey and recommended that they do a complete re-evaluation of the property (sampling, new ore reserve calculations and feasibility studies). In the residents geologist's opinion previous work and interpretations may not be reliable. Since the visit new staff have been hired and work is to start soon. [ PRECIS ]

Date: Jul 27, 1993

Geologist: S Fumerton

Notes: A brief visit was made to the site. The buildings, a cabin, a bunkhouse, a garage, a core shack, and a hoist house are in a moderate state of repair. The steel headframe is still intact with skip plus wire rope attached, though the siding around the headframe has been removed. The single compartment shaft is covered with 2x6' lumber weighted down with the skip and steel railings. However, a manway equipped with a sturdy ladder is only covered with loose plywood though the shaft is flooded to within 3m of the collar. This loose access was mentioned to an affiliate of the owner who gave assurances that the access would be secured right away. The single drum compressed air hoist is intact and last licensed in 1978 but no air compressor is on site. The mill has been demolished. Recent drill core is stored outside on steel racks and is generally in good order. An attempt was made to locate the original Three Ducks Syndicate #2 vein south of the Young Shannon headframe. Though there is now a system of drill roads, washed outcrops etc in the expected area, no sign of any old trenching or quartz veining was found. Laird's (1932) description of a north dipping vein system to original discovery is at odds with the south dip of the Young Shannon deposit suggesting that they are distinct prospects. As no one has relocated the original workings they has been a tendency to regard the Three Ducks #2 vein as the same as the Young Shannon deposit.

References

File - Resident Geologist files T-6350

Publication Number: Date:

Author:

Publisher Name:

Location: Timmins RGP office

Map - Three Duck Lakes area, District of Sudbury, Ontario

Publication Number: ARM41D Scale: 1:47,520    Date: 1997

Author: Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:

Publication - Technical Report on the C�t� Gold Project, Ontario, Canada Report for NI 43-101

Publication Number: NI 43-101 Page: 14-34  Date: 2022

Author: Coulson, A.L., Shah, B., Davachi, M.M., O'Hara, P.M, Turenne, R.J., Daniel, S.E., Nada, D.

Publisher Name: IAMGOLD Corp.

Location: SEDAR

Map - Geological series, Precambrian geology of Chester and Yeo townships, and parts of Neville and Potier townships, Jerome area, Sudbury District

Publication Number: P2449 Scale: 1:15,840    Date: 1981

Author: Siragusa G.M.

Publisher Name: Ontario Geological Survey

Location:

Map - Precambrian Geology, Parts of Chester, Neville, Potier and Yeo Townships

Publication Number: OFM0214 Scale: 1:15,840    Date: 1993

Author: Siragusa G.M.

Publisher Name: Ontario Geological Survey

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: 41P-43  Date: 1985

Author: Rose, D. G.

Publisher Name: Geological Survey of Canada

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

Map - Geology, Swayze greenstone belt, Gogama, Ontario

Publication Number: OF3384G Scale: 1:50,000    Date: 1999

Author: Heather, K B; Shore, G T

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/210455

Article - Jerome area, District of Sudbury

Publication Number: MP096.012 Page: 51-54  Date: 1997

Author: Siragusa G.M.

Publisher Name: Ontario Geological Survey

Location:

Part - Geology of the Three Duck lakes area

Publication Number: ARV41-03.001 Page: 78  Date: 1998

Author: Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:

Part - Geology of the Makwa-Churchill area

Publication Number: ARV43-03.002 Page: 28-30  Date: 1998

Author: Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:

Part - Mines of Ontario in 1935

Publication Number: ARV45-01.003 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 - Mines of Ontario in 1936

Publication Number: ARV46-01.003 Date: 1997

Author: Sinclair D.G., Tower W.O., Bayne A.S., Cooper D.F., Weir E.B., Webster A.R.

Publisher Name: Ontario Dept. of Mines

Location:

Part - Mines of Ontario in 1937

Publication Number: ARV47-01.003 Date: 1997

Author: Sinclair D.G., Tower W.O., Taylor J.B., Douglass D.P., Bayne A.S., Cave A.E., Cooper D.F., Weir E.B., Webster A.R.

Publisher Name: Ontario Dept. of Mines

Location:

Publication - Molybdenum in Canada Part 2 : Molyfile; Geological Survey of Canada, Economic Geology Report 33

Publication Number: Econ Geol 33 Date: 1982

Author: Kirkham, R V; McCann, C; Prasad, N; Soregaroli, A E; Vokes, F M; Wine, G

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/109258

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

Publication - Mineral occurrences in Woman River district, Ontario; Geological Survey of Canada, Summary Report 1929, pt. C

Publication Number: Sum Rep 1929 C Date: 1930

Author: Bannerman, H M

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/102021

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: 54  Date: 1979

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

Publisher Name: Ontario Geological Survey

Location:

Article - Timmins Resident Geologist's District - 1990

Publication Number: MP152.011 Date: 1997

Author: Luhta L.E., Sangster P.J., Ireland J.C., Farrow D.G., Draper D.M., Hamblin C.D.

Publisher Name: Ontario Geological Survey

Location:

Mono - Copper, nickel, lead and zinc deposits in Ontario (revised to February, 1957)

Publication Number: MDC002 Date: 1957

Author: Thomson J.E., Ferguson S.A., Johnston W.G.Q., Pye E.G., Savage W.S., Thomson R.

Publisher Name: Ontario Dept. of Mines

Location:

Mono - Molybdenum deposits of Ontario

Publication Number: MDC007 Page: 66-67  Date: 1968

Author: Johnston F.J.

Publisher Name: Ontario Dept. of Mines

Location:

Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file

Publication Number: OFR5467 Date: 1983

Author: Hodgson C.J.

Publisher Name: Ontario Geological Survey

Location:

MonoMap - Geology, Geochemistry and Mineralization of the Southern Margin of the Swayze Belt

Publication Number: OFR5844 Page: 89-90  Date: 1993

Author: Siragusa G.M.

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: 391-395  Date: 1995

Author: Fumerton S.L., Houle K.A.

Publisher Name: Ontario Geological Survey

Location:

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