GeologyOntario has moved. You will be redirected to the new site in 10 seconds. If you are not immediately redirected please follow the below link to the new GeologyOntario platform. For assistance please contact us.
Ministry of Energy, Northern Development and Mines
Permanent Link to this Record: MDI000000000365Deposit Name(s) | Ray Smith Occurrence - 1956, Hamlin - 2003, Hamlin-deaty - 2014 |
---|---|
Deposit Status | prospect |
Abandoned Mine Inventory Reference | 08431 |
Date Created | 2007-Aug-30 |
Date Last Modified | 2018-Sep-25 |
Created By | Q Unknown |
Revised By | T Pettigrew |
Primary Commodities: copper, gold
Secondary Commodities: molybdenum, silver
Township or Area: Powell Lake Area
Latitude: 48° 29' 14.07" Longitude: -90° 47' 12.5"
UTM Zone: 15 Easting: 663529 Northing: 5372823 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52B07NW
Point Location Description: DDH HAM-11-69 from AFRI 20000013643
Location Method: data compilation
Access Description: Access to these claims can be achieved by turning south down Swamp road, which is approximately 130 km west of Thunder Bay on Highway 11. Turn west on Hermia Lake Road then turn south on Tilly Road souththen follow Nelson Road for 9.8 km.
1956: R. Smith and R. Sanderson discovered the showing. 1957: an EM survey and trenching were conducted, then 2 DDH totalling 265.2 m were drilled. 1985: Kennco Explorations Canada Ltd. carried out ground magnetometer and VLF-EM surveys, geological mapping, and sampling. 1987: Grande Portage Resources Ltd. carried out trenching, and sampling. 1990: Noranda Exploration Company Ltd. carried out HLEM, magnetometer, IP and resistivity surveys, prospecting and humus sampling. 1991: Noranda drilled 3 DDH totalling 879 m. 2004: East West Resources carried out a VTEM survey, geological mapping, and prospecting. 2005-6: East West Resources carried out an EM survey and drilled 24 DDH totalling 5504.2 m. 2008-10: Xstrata Copper drilled 9 DDH totalling 3042.5 m. 2011: Xstrata drilled 17 DDH totalling 6179 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.31354 | 20000001032 | Open |
2.48888 | 20000007598 | Open |
63.847 | 52B07NW0057 | Open |
2.28044 | 52B07NW2010 | Open |
2.45445 | 20000006351 | Open |
29 | 52B07NW0005 | Open |
2.53580 | 20000013643 | Open |
13 | 52B07NW0070 | Open |
2.8715 | 52B07NW0042 | Open |
2.9890 | 52B07NW0074 | Open |
2.27257 | 52B10SW2016 | Open |
2.31114 | 20000001115 | Open |
2.32415 | 20000001488 | Open |
Province: Superior
Subprovince: Wawa
Belt: Shebandowan
Geological Age: Archean Geochronological Age: 2715-2720
Tectonic Assemblage: Central Felsic To Intermediate Metavolcanic Belt
Rock Type | Rank | Composition | Texture | Relationship |
---|---|---|---|---|
intermediate metavolcanics | 1 | dacite | breccia | host |
iron formation | 2 |
12/06/2016 (A Tims) - The breccia unit is a highly siliceous intermediate metavolcanic with intermittent sections of brecciated volcanics, foliated siliceous volcanics and mafic volcanics.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Habit Description |
---|---|---|---|---|---|---|---|
3 | magnetite | economic and alteration | ore | hydrothermal | 1 | unknown | veins |
1 | pyrite | economic | ore | ||||
2 | chalcopyrite | economic | ore |
12/06/2016 (A Tims) - Alteration in this unit consists of pervasive chloritic and epidote alteration throughout unit with trace qtz+calcite vugs. Occasional large blebs of magnetite are present. Chlorite veins occur as infilling around breccia clasts and as hairline veinlets cutting the core at varying angles. Pyrite occurs within both the qtz and chlorite veinlets, and as fine, subhedral grains. Magnetite averages 10-20% to WR and qtz+calcite vugs are at -10% to WR. Epidote alteration is patchy and occurs at -10-20% to WR. The breccia clasts are pink (sodic?) and cherty fragments averaging 1-3cm size, these clasts do not support any mineralization. Silica veinlets cut the core at varying angles. Gabbroic fragments are abundant throughout and are epidotized. Mineralization consists of disseminated Py+Cpy, and is patchy around vugs, sometimes occurring with epidote. Trace blebby molybdenite is present.
09/25/2018 (T Pettigrew) - Assay results from original trenches at the Ray Smith Occurrence returned values of 0.23% Cu over 6.0 m. Noranda’s 1991 DDH GP-91-02 assayed 0.33% Cu (AFRI 52B07NW0005). The Noranda trenches exposed a semi-banded chert-magnetite iron formation in chloritic intermediate metavolcanics. Chalcopyrite occurs as narrow stringers with associated pyrite. A 0.5 m chip sample across the iron formation returned an assay of 735 ppb Au. Copper mineralization is generally associated with altered zones of rhyolite and andesite. Drill hole A6 from 1957 was drilled over the original copper showing. Five narrow zones from 12 to 36 cm wide occurred over 15.24 m yielding 0.5-3% Cu. Another 6.1 m section contained 0.23% Cu. In 1984, samples from the trenches yielded 620 and 10 ppb Au (AFRI 52B07NW0042). Mineralization in the iron formations consists of 1-10% pyrite and up to 40% magnetite in some of the units (AFRI 52B07NW2010). DDH DC-11-21 returned assays of 3.0 gpt Au over 1.5 m and 2.24 gpt Au over 0.4 m. DDH HAM-11-67 had assays between 0.5-1% Cu. DDH HAM-11-69 assayed 0.67% Cu at 101 m and 0.74% Cu at 141.5 m. DDH HAM-11-70 assayed 0.31% Cu, 0.21 gpt Au, and 2.18 gpt Ag over 21 m. DDH HAM-11-75 assayed 0.35% Vu, 0.015% Mo, 2.15 gpt Ag, and 087 gpt Au over 156.1 m (AFRI 20000013643). DDH NG-08-01 assayed 2649 ppm Cu over 14.1 m from 6.0-20.1 m, including up to 6513 ppm Cu over 1.4 m from 7.1-8.5 m, and 1326 ppm Mo over 1.5 m from 93.2-94.7 m. DDH NG-08-02 asasyed 4187 ppm Cu over 1.5 m from 61.3-62.8 m. DDH NG-10-07 had low grade mineralization over 144 m from 183-327 m, including assays up to 3730 ppm Cu over 3 m from 234-237 m, 5410 ppm Cu over 3 m from 264-267 m, 2320 ppm Cu over 15 m from 282-297 m, and 2248 ppm Cu over 319.5-327 m, and 1300 ppm Mo over 1.5 m at 222 m (AFRI 20000007591).
08/30/2007 (Q Unknown) - diss cpy, py, in volc bx tr Mo
Rank | Classification |
---|---|
1 | vms base metal |
2 | iocg |
Publication - Geology of the Moss Lake area, District of Thunder Bay
Publication Number: R085 Date: 1970
Author: Harris,H.E.
Publisher Name: ODM
Publication - Copper, Nickel, Lead and Zinc Deposits of Ontario
Publication Number: MDC012 Date: 1969
Author: Shklanka, R.
Publisher Name: ODM
Publication - Greenwater Lake Area, West-Central Shebandowan Greenstone Belt
Publication Number: R296 Date: 1997
Author: Osmani, I.A.
Publisher Name: OGS
Map - Precambrian Geology of the Wye and Hamlin Lakes Area
Publication Number: P2511 Scale: 1:20 000 Date: 2009
Author: Hart, T.R., Metsaranta, D.A
Publisher Name: OGS
We are continuously updating the Mineral Deposit Inventory. If you notice errors in the data please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral deposit please contact the Thunder Bay South Resident Geologist District Office