Ontario Geological Survey
Permanent Link to this Record:
MDI000000002213
Record Name(s) | Wabassi A Zone Gold - 2017, Wabassi Property - 2012 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2018-Aug-20 |
Date Last Modified | 2023-Aug-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Venton Lake Area, Oxtoby Lake Area
Latitude: 51° 44' 56.55" Longitude: -86° 37' 52.61"
UTM Zone: 16 Easting: 525454 Northing: 5733191 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42M10NE, 42M15SE
Point Location Description: Location of collar of DDH 12WA-30 in AFRI 20000009211
Location Method: Based on Assessment
Access Description: Site access is by floatplane and helicopter in the summer from Hearst or Nakina and by snow mobile in the winter. The north portion of the Wabassi Property can be accessed by boat from Martin Falls First Nation located 54 km to the west by navigating the Albany River and the Wabassi River to Wabassi Falls then becomes unnavigable as the historical portage is no longer passable.
1942: Bedrock mapping by V.K. Prest of the Ontario Geological Survey (OGS). 1970: Reconnaissance mapping by Thurston and Carter for the OGS’ Operation Fort Hope. 1979: Diamond drilling by Hanna Mining Co., on an area to the west of, and overlapping, the Wabassi Property. 1980: Kerr Addison Mines Ltd., completed an airborne electromagnetic survey on an area north of the Wabassi Property. 1983: Kerr Addison Mines Ltd., undertook limited diamond drilling as follow-up to their 1980 airborne survey. 2003: Ontario Geological Survey flew an airborne magnetic survey as part of the Fort Hope geophysical program. 2007: Northern Shield Resources Inc., staked the Wabassi and Wabassi North properties based on the 2003 geophysical magnetic survey by the Ontario Geological Survey in the Fort Hope area. 2008: Geotech Ltd. conducted three VTEM EM and magnetic surveys over the Wabassi property. Initial drilling to test EM responses. 2010: Northern Shield Resources Inc. had Geotech Ltd. perform an airborne VTEM survey, ground and downhole magnetic and EM geophysical survey and diamond-drilling with assays and lithogeochemistry was completed on core samples from this drill program. Northern Shield Resources Inc., optioned 51% to Discovery Harbour Resources. 2011: Crone Geophysics and Exploration Ltd. performed a ground and downhole geophysics followed by a diamond drill program by Northern Shield Resources Inc. 2011: Northern Shield Resources Ltd. initiated a winter exploration program on their Wabassi property consisting of diamond drilling, both ground and down-hole electromagnetic and magnetic surveys and airborne versatile time-domain electromagnetic (VTEM) survey. 2012-2013: Multiple diamond drill programs were conducted as well as a ground magnetic survey and both ground and bore-hole electromagnetic (EM) surveys, on the Wabassi Property by Northern Shield Resources Ltd., and joint venture partner Discovery Harbour Resources Corp. 2014: Discovery Harbour Resources Corp. and former joint-venture partners Northern Shield Resources Inc., and Great Lake Resources LLC, announced the results of a fall diamond-drilling program including down-hole EM surveys also identified a number of off-hole anomalies. Northern Shield Resources Inc. subsequently announced that it sold its remaining interest in the Wabassi property to Great Lakes Resources LLC. The sale agreement transferred Northern Shield’s 49% interest in the Wabassi property. 2015: Wabassi completed the acquisition of the Wabassi project from Northern Shield Resources Inc. and Discovery Harbour Resources Inc. (Great Lakes Resources LLC purchased the remaining 51% interest in the Wabassi project, east of Eabametoong First Nation (Fort Hope), from Discovery Harbour Resources Corp. 2016: Great Lakes reorganized its interest in the project through Wabassi Resources ULC, a wholly owned subsidiary. Wabassi Resources completed 1 diamond drill hole on the Wabassi A Gold Zone. A regional mapping program was also completed in the summer of 2016, which targeted outcrop areas exposed in river and stream channels. In March 2017, Wabassi Resources completed a 10 hole, 1,823.4 m drill program on the Wabassi A Zone Gold target. Drilling at the Wabassi A Gold Zone has successfully delineated a narrow, strongly mineralized, vein system with local visible gold over an approximately 250 m strike length.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.57744 | 20000013564 | 20000013564 |
2.58159 | 20000015067 | 20000015067 |
2.57503 | 20000013560 | 20000013560 |
2.52098 | 20000014358 | 20000014358 |
2.54970 | 20000009211 | 20000009211 |
2.52066 | 20000007336 | 20000007336 |
2.51306 | 20000008133 | 20000008133 |
2.50726 | 20000006763 | 20000006763 |
2.50163 | 20000006363 | 20000006363 |
2.45532 | 20000006727 | 20000006727 |
2.42781 | 20000004275 | 20000004275 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Miminiska-Fort Hope
Geological Age: Archean
Aug 20, 2018 (Greg Paju) - From AFRI 20000009211: The Wabassi Property is located in the Archean Miminiska-Fort Hope greenstone belt in the Uchi Domain (2.8-2.9 Ga) of the Superior Province’s Sachigo Superterrane. (Stott and Rayner, 2004, Stott et al., 2007 and Stott, 2007a-b).
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
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Granite | 2 | Granite | Contains |
Aug 20, 2018 (Greg Paju) - From AFRI 20000013564: The Wabassi Intrusive Complex underlying the Wabassi Property is a layered mafic-ultramafic intrusion and the lithologies identified to date are olivine-gabbronorite, gabbronorite, norite and troctolite. The mafic metavolcanic assemblages are of basaltic to andesitic composition. It is generally very altered and pale green, which makes it difficult to distinguish from the felsic metavolcanic that is not quartz-phyric. Felsic metavolcanic rocks vary in composition between rhyolite and dacite and a large proportion of these lithologies display blue quartz eyes up to about 5 mm in size. They are generally massive flows, fragmentals and breccias. The volcanogenic massive sulphides encountered to date are mostly contained within or just above this assemblage of felsic metavolcanic rocks. The area of the gold mineralization has 20 to 25 m of glacial overburden coverage with no outcrop exposure. The Wabassi A Zone Gold Occurrence is hosted to date in three separate quartz veins, with the main quartz vein varying in width from approximately 0.20 m to 1.0 m and is associated with a shear zone hosted in the granitic rocks in the west or the gabbro in the east The 2nd vein is sub-parallel and located approximately 20 m south of the east end of the main vein. The 3rd vein is located 850 m south and was intersected by drill hole 17WA-64. The majority of the holes have intersected the northern vein (main quartz vein) and the orientation is well defined with a strike of 093°and sub-vertical dip. In hole 17WA-57, the shear is associated with the development of mylonite in granite and local development of a crenulation cleavage. Locally the veinlets form a stockwork in granite with silicification, carbonate alteration and disseminated sulphides.
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 | Chalcopyrite | Economic | Ore | ||||
4 | Gold | Economic | Ore | ||||
5 | Arsenopyrite | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Tourmaline | Economic | Gangue |
Aug 20, 2018 (Therese Pettigrew) - From AFRI 20000009211 and 20000013564: The drilling done to date on the Wabassi A Gold Zone has delineated a narrow, mineralized vein system with local visible gold over an approximately 250 m strike length. The quartz veining is associated with trace to approximately 5% sulphide mineralization consisting of pyrite, pyrrhotite, and minor chalcopyrite. Visible gold was observed in 4 of the 12 diamond drill holes and occurs as fine 1 to 2 mm individual grains and grain clusters hosted in the quartz vein. Significant results from Hole 16WA-54 successfully intersected a heavily silicified shear zone with quartz veins containing tourmaline, pyrite, arsenopyrite, and visible gold. The 4.2 m interval from 137.98 to 142.18 m assayed 9.90 g/t Au, and included 2.67 m from 138.48 to 141.15 at 14.97 g/t Au. Visible gold was also identified with assays over 20 g/t Au. This was an intended follow up on the 2012 diamond drill hole 12WA-30; that had 3.1 m at 6.01 g/t Au.
Rank | Classification |
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1 | Lode (Gold) |
1 | Vein |
Rank | Characteristic |
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1 | Sheared |
1 | Vein |
Data - Ontario Airborne Geophysical Surveys, Magnetic Data, Attawapiskat Area - Purchased Data
Publication Number: GDS1211 Date: 2003
Author: Ontario Geological Survey
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-West Sheet
Publication Number: P3597-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2016, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6325 Page: 32-33, 54 Date: 2017
Author: Cundari R.M., Brunelle M.R., White G.D., Tuomi R.D., Tims A.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-East Sheet
Publication Number: P3598-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2015, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6315 Page: 15 Date: 2016
Author: White G.D., Cundari R.M., Brunelle M.R., Pettigrew T.K., Tuomi R.D., Tims A., Debicki R.L.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2014, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6302 Page: 16-17 Date: 2015
Author: White G.D., Cundari R.M., Brunelle M.R., Pettigrew T.K., Tims A., Debicki R.L.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2013, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6292 Date: 2014
Author: White G.D., Cundari R.M., Tuomi R.D., Brunelle M.R., Debicki R.L., Moses P., Zurevinski S.E.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2012, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6284 Page: 29-30 Date: 2013
Author: White G.D., Cundari R.M., Lockwood H.C., Tuomi R.D., Debicki R.L., Moses P., Zurevinski S.E.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2011, Resident Geologist Program, Thunder Bay North Regional Resident Geologist Report: Thunder Bay North District
Publication Number: OFR6272 Page: 25-26 Date: 2012
Author: White G.D., Smyk M.C., Cooke A., Lockwood H.C., Wilson A.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral Deposits of Northern Ontario, North of Latitude 49° 30'
Publication Number: OFR6242 Date: 2009
Author: Stott G.M., Josey S.D.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of Field Work and Other Activities, 2004
Publication Number: OFR6145 Page: 10-1 to 10-8 Date: 2004
Author: Baker C.L., Debicki E.J., Parker J.R., Kelly R.I., Ayer J.A., Easton R.M.
Publisher Name: Ontario Geological Survey
Location:
Publication - A Revised Terrane Map for the Superior Province as Interpreted from Aeromagnetic Data; In: Institute on Lake Superior Geology Proceedings, 53rd Annual Meeting, Lutsen, Minnesota, p. 74-75
Publication Number: ILSG v.53 Date: 2007
Author: Stott, G.M., Corkery, T., Leclair, A., Boily, M. and Percival, J.
Publisher Name: Institute on Lake Superior Geology
Location:
Compend - Summary of Field Work and Other Activities, 2010
Publication Number: OFR6260 Page: 20-1 to 20-10 Date: 2010
Author: Ayer J.A., Easton R.M., Beakhouse G.P., Stott G.M., Kelly R.I., Debicki E.J., Parker J.R., Brown T.
Publisher Name: Ontario Geological Survey
Location:
Article - Overview of the Mafic and Ultramafic Intrusions in the Eastern Uchi Domain of the Superior Province, Northern Ontario
Publication Number: OFR6290.51 Date: 2013
Author: Sappin A.-A., Houlé M.G., Lesher C.M., McNicoll V.J.
Publisher Name: Ontario Geological Survey
Location:
Mono - Operation Fort Hope
Publication Number: MP042 Date: 1970
Author: Thurston P.C., Carter M.W.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Publication - Technical Report on the Wabassi Property for Discovery Harbour Resources Corp. and CVC Cayman Ventures Corp., 170 p.
Publication Number: 2012 Tech Rep Date: 2012
Author: Clark, J.G.
Publisher Name:
Location:
Publication - Technical Report on the Exploration of the Wabassi, Wabassi North and Max Mafic-Ultramafic Intrusions., 54 p.
Publication Number: 2010 Tech Rep Date: 2010
Author: Vaillancourt, C., and Biss, I.
Publisher Name:
Location:
Publication - Technical Report and Initial Resource Estimate on the Wabassi “E” Deposit, Wabassi Property Thunder Bay and Porcupine Mining Divisions Northern Ontario For Wabassi Resources, ULC., 103p.
Publication Number: 2016 Tech Rep Date: 2016
Author: Puritch, E., Burga, D., Yassa, A. and Barry, J.
Publisher Name:
Location:
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