Ontario Geological Survey
Permanent Link to this Record:
MDI000000000387
Record Name(s) | Sweet Spot & Sweet Spot 2 Trench - 2004 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2007-Aug-31 |
Date Last Modified | 2022-Jul-15 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper, Lead, Zinc, Silver
Township or Area: Moss
Latitude: 48° 34' 13.87" Longitude: -90° 47' 39.29"
UTM Zone: 15 Easting: 662712 Northing: 5382063 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52B10SW
Point Location Description: Field Visit
Location Method: Field Visit with GPS
Access Description: Approximately 120 kms W of Thunder Bay. The property is accessed via Hwy #11 W of Kashabowie for 15.6 kms where the Swamp Road and West Hermia are taken for 16 kms to the eastern boundary of the Larose property.
1989: Noranda Exploration completed some glacial till sampling and limited trenching. 2003: R. Kwiatkowski (prospector) sampled rusty schist yielding very anomalous gold grades and recorded as the original discovery of the Larose showing then optioned to Freewest Resources Canada Inc. 2003-2004: Freewest Resources Canada Inc. carried out prospecting, line cutting, soil geochemistry, magnetometer and IP surveys, 30 DDH (2,742 m), trenching and geological mapping. May 2011: Freewest changed its name to Cliffs Chromite who then optioned the property to Viking Gold Exploration Inc. Dec 2011: Golden Share Ltd. JVs the property to acquire 50% and performed line cutting, magnetometer survey and soil geochemistry. 2012: Golden Share contracted SRK Consulting to complete a structural geology study. 2015: Viking Gold Exploration transferred the property to Kwiatkowski, R. who then transferred title to Tashota Resources. 2016: Tashota Resources completed trench mapping and 5 DDH, 240.49 m, DDH under the P1 trench. An airborne time-domain EM, magnetic and radiometric survey was flown by Prospectair Inc.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.522224 | 20000007313 | 20000007313 |
2.30136 | 20000000768 | 20000000768 |
2.53456 | 20000007501 | 20000007501 |
2.57089 | 20000014552 | 20000014552 |
2.75050 | ||
2.29726 | 20000000363 | 20000000363 |
2.29727 | 20000000365 | 20000000365 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Shebandowan
Geological Age: Archean
Nov 28, 2012 (B Schnieders) - The Larose property was optioned to Freewest Resources Canada Inc., whose prospecting and stripping programs led to the discovery of several gold zones or occurrences, including (from the southwest to the northeast): the J and R, Larose, the P, Central P, Snoopy, Porphyry and Northwest View. Combined, these zones make up the ‘Main Zone’, which has a strike length of 1500m (Freewest Resources Canada Inc. Press Release November 11,2003). Two separate shear zones are observed at the Larose occurrence at 48/70NW. The shear zones are up to 7m wide and hosted in thinly bedded, turbiditic wacke and siltstone. The sheared and altered, host metasedimentary rocks display quartz veining and stringers, chloritization, silicification, carbonatization, seritization and sulphidization. Fine-grained pyrite and pale visible gold occur in the milky-white to maroon quartz stringers. Sugary, recrystallized quartz veins and pods are up to 30 cm wide. A chip sample collected by the authors across 30cm of the altered metasedimentary host and quartz stringers assayed 70.6 g/t gold (Resident Geologist Files, Thunder Bay’s South District, Thunder Bay). A parallel shear zone on the same stripped outcrop is located 10m to the northwest of the aforementioned shear zone. The second shear zone is hosted in the ‘DE’ turbidites (southeast-younging). Bedding/cleavage relationships suggest tight to isoclinal folding is present. Here the shear zone is sulphide-rich. Galena, sphalerite, pyrite and arsenopyrite are associated with ‘rotten’ sugary quartz.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Host |
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Wacke | 2 | Host | ||
Quartz-Feldspar Porphyry | 3 | Quartz-Feldspar | ||
Siltstone | 3 | Host | ||
Syenite | 4 | Adjacent |
Nov 27, 2017 (Therese Pettigrew) - The Sweet Spot and Sweet Spot 2 trenches are located at the contact between metasedimentary rocks and a relatively large (approximately 20 m wide) quartz-feldspar porphyry intrusion. The contact is not visible, but coincides with a depression, trending approximately 215 degrees, that likely marks a sheared contact. The quartz-feldspar porphyry intrusion, southeast of the contact, displays significant shearing, faulting and fracturing with variable alteration. Shears that parallel the primary foliation display quartz veining and contain disseminated sulphide mineralization. The Sweet Spot 2 trench displays the contact between a quartz-feldspar porphyry intrusion at the metasedimentary rocks. Deformation at this location is not as pervasive as the Sweet Spot trench (Puumala et al., 2017).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore | ||||
3 | Galena | Economic | Ore | ||||
4 | Sphalerite | Economic | Ore | ||||
5 | Arsenopyrite | Economic | Ore | ||||
6 | Gold | Economic | Ore | ||||
Sericite | Alteration | Sericitization | 1 | Unknown | Replacement | ||
Chlorite | Alteration | Chloritic | 2 | Unknown | Replacement | ||
Carbonate | Alteration | Carbonization | 3 | Unknown | Replacement |
Nov 28, 2012 (Shannon Zurevinski) - Gold mineralization is intimately related to a continuous high strain zone known as the Larose shear zone (LSZ), that has been traced over a minimum 4 km strike length. The LSZ trends to the northwest (050°), dips subvertically and attains a maximum width of about 25 metres. It is a sinistral shear zone that contains several gold zones occurring as discrete shoots within it. The LSZ hosts quartz veins, quartz vein stockwork and sulphide disseminations enclosed by greywacke host rocks characterized by heavy alteration. The quartz veins contain and wallrock disseminations comprise pyrite, galena, sphalerite, chalcopyrite, arsenopyrite and visible gold. The geological setting at Larose has been compared to that of the Malartic district of Quebec, which comprises host rocks of greywacke, quartz-feldspar porphyry and syenitic intrusive rocks.
Nov 27, 2017 (Therese Pettigrew) - From the Freewest 2004 drill program, DDH L04-23 shows gold mineralization primarily from 69-74 m within a feldspar-porphyry dyke that is crosscut by chalcopyrite-pyrite stringers (AFRI 20000007501).
Feb 28, 2017 (Q Unknown) - up to 13.4 g/t Au (news release 2010 Freewest) 2016: Although low assay values were obtained from the grab samples collected during the RGP site visit, some of the best historic diamond-drilling results on the Larose property were obtained from this area.
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Sheared |
Date: Oct 03, 2016
Geologist: Dorothy Campbell
Notes: The Sweet Spot and Sweet Spot 2 trenches are located at the contact between metasedimentary rocks and a relatively large (approximately 10 m wide) quartz-feldspar porphyry intrusion. At the Sweet Spot trench, the metasedimentary rocks display graded bedding indicative of northwest younging. Bedding planes strike 035° with near-vertical dip. The fine-grained portions of the graded turbidite beds are fissile and display a cross-cutting cleavage that is oriented 222° and dips 75° toward the northwest
Date: Nov 16, 2016
Geologist: Mark Puumala
Notes: The Sweet Spot 2 trench displays the contact between a quartz-feldspar porphyry intrusion and the metasedimentary rocks. Deformation at this location is not as pervasive as at the Sweet Spot. However, the porphyry intrusion contains many quartz-filled and sulphide mineralized brittle fractures. The fractures are steep-dipping and there appear to be three sets that strike 260°, 300° and 340°. The foliation at this location strikes 050°.
Map - Precambrian Geology, Moss Township
Publication Number: M2624 Scale: 1:20,000 Date: 1997
Author: Osmani I.A.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology and Mineral Potential, Greenwater Lake Area, West-Central Shebandowan Greenstone Belt
Publication Number: R296 Date: 1997
Author: Osmani I.A.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2003, Resident Geologist Program, Thunder Bay South Regional Resident Geologist Report: Thunder Bay South Kenora District
Publication Number: OFR6129 Page: 17-19 Date: 2004
Author: Schnieders B.R., Scott J.F., O'Brien M.S., Magee M.A., Komar C.L.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2016, Resident Geologist Program, Thunder Bay South Regional Resident Geologist Report: Thunder Bay South District
Publication Number: OFR6326 Page: 34-44 Date: 2017
Author: Puumala M.A., Campbell D.A., Tuomi R.D., Tims A., Brunelle M.R.
Publisher Name: Ontario Geological Survey
Location:
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