Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI000000002214

Record: MDI000000002214

General

Mineral Record Identification
Record Name(s) Tempest Zone - 2017, Tempest Property - 2012
Related Record Type
Related Record(s)
Record Status Occurrence
Date Created 2018-Aug-20
Date Last Modified 2022-Feb-24
Created By
Revised By

Commodities

Primary Commodities: Silver, Zinc

Secondary Commodities: Copper, Gold



Location

Township or Area: Gittins Lake Area

Latitude: 51° 51' 23.75"    Longitude: -86° 22' 19.2"

UTM Zone: 16    Easting: 543250   Northing: 5745275    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 42M16SW

Point Location Description: From DDH 12TP-12 collar in AFRI 20000014870

Location Method: Based on Assessment

Access Description: The Tempest Zone is accessible by floatplane and helicopter in the summer and by plane on skies and snowmobile in the winter.



Exploration History

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. 2011: The Tempest group of claims were acquired for Northern Shield. 2011: Geotech Ltd. flew a helicopter-borne VTEM survey over the Tempest Property for Northern Shield Resources. 2011: Three diamond drill programs were performed on the property totalling 12 holes and 4,791 m. 2012: Geotech Ltd. flew a helicopter-borne VTEM geophysical survey over Northern Shield and Discovery Harbour’s Wabassi and Storm Group of Properties (The Storm Claim Group consists of 6 claims blocks identified as Tempest, Typhoon, Blizzard, Squall, Gale and Monsoon). 2012: A high-resolution ground magnetic geophysical survey was completed on the Tempest Property by consultants Gary Smith and Glenn O’Keefe. The goal of the survey was to enhance the understanding of the geometry and location of the magnetic response from the massive sulphide body to assist in the positioning of future drilling. 2013: A structural geology study was conducted on several drill holes from the Tempest 1 grid. The structural study included additional logging, sampling and structural interpretation of holes 11TP-01, 02, 03 and 12TP-04, 07,08, 09, 10, 11 and 12. 2016: Wabassi Resources acquired the Tempest Property from Northern Shield and subsequently staked additional claims to form a contiguous property. 2016-2017: Compilation of geophysics and a new interpretation of geological data combined with re-examination and sampling of core from holes drilled by Northern Shield Resources.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.58159 20000015067 20000015067
2.58020 20000014870 20000014870
2.54985 20000008159 20000008159
2.54195 20000008883 20000008883
2.53270 20000008275 20000008275

Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Miminiska-Fort Hope

Geological Age: Archean  



Geology Comments

Aug 20, 2018 (Greg Paju) - From AFRI 20000008159: The Tempest Zone 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). However, the subdivisions of the North Caribou Terrane are based mostly on work carried out on the western portion of the Sachigo Superterrane and since there is very little data available in the area of the Tempest Zone, these boundaries remain highly speculative.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1
Felsic Pyroclastic Breccia 2 Pyroclastic Host

Lithology Comments

Aug 20, 2018 (Greg Paju) - Geology on the property consists of a succession of deformed, greenschist facies metavolcanic rocks. The succession is E-W trending with a well-defined S1 foliation oriented approximately E-W and dipping steeply to the south, a less well defined S2 axial planar foliation dipping to the SW and a locally strong lineation possibly plunging steeply to the WSW. The overall stratigraphy from south to north consists of mixed mafic and felsic volcanic flows including some breccia, mafic tuff and argillaceous tuff, in the area of the main Tempest mineralization, a 200-metre thick intermediate pyroclastic unit separates the two “exhalative” horizons. Silver-rich mineralization was intersected in association with stringer, semi-massive and massive sulphides dominated by pyrite and pyrrhotite, and is hosted in intensely altered felsic volcanic rocks.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyriteEconomicOre
2PyrrhotiteEconomicOre
3SphaleriteEconomicOre
4ArsenopyriteEconomicOre
1QuartzEconomicGangue
2ChloriteEconomicGangue
3MuscoviteEconomicGangue
4SericiteEconomicGangue

Mineralization Comments

Aug 20, 2018 (Greg Paju) - From AFRI 20000014870, 20000008883, 20000008159, OFR6272 and OFR6284: Silver-rich mineralization was intersected in association with stringer, semi-massive and massive sulphides dominated by pyrite, pyrrhotite, minor sphalerite and trace arsenopyrite, and is hosted in intensely altered felsic volcanic rocks. According to Colin Bowdidge, the gold mineralization at Tempest is epigenetic, but possibly formed by remobilization of volcanogenic gold. Its juxtaposition and partial overlap with a silver zone is probably coincidental. The gold is hosted in a silicified zone with minor quartz veining and associated with trace sulphides (seen in DDH 12TP-07), and as visible gold in near surface laminated quartz vein (seen in DDH 12TP-12). The silver mineralization is associated with stringer, semi-massive and massive sulphides dominated by pyrite and pyrrhotite and hosted by intensely altered metavolcanic rocks. Alteration of the Tempest property consists of chlorite, muscovite, Fe-Oxide and minor sericite. Chlorite alteration is variable and occurs throughout the stratigraphy independently of lithology. Silicification, quartz veining, carbonatization and Fe-carbonate alteration are common throughout most of the stratigraphy. Sulphides are generally associated with chlorite, carbonate, silica alteration, and quartz veins Some highlights of the drilling on the Tempest property are from DDH 11TP-01 (extended) which intersected 1 m of 3% Zn and 16.7 m of 29.6 g/t Ag; DDH 11TP-02 intersected 104.2m with 19 g/t Ag, this includes a higher grade interval of 51 g/t Ag over 19.8 meters. The highest silver value from this intersection assayed 195 g/t Ag over 1 meter. Bowdidge (2017) re-assayed some of the Tempest core as part of a study of the gold and silver mineralization. A few highlights of this program are 1 m in DDH 12TP-08 containing 0.009 g/t Au, 28.2 ppm Ag, 42 ppm Cu, 17 ppm Pb and 59 ppm Zn, and DDH 12TP-07 with 1 m containing 0.082 g/t Au, 2.2 ppm Ag, 25 ppm Cu, 34 ppm Pb and 48 ppm Zn.



Mineral Record Details

Classification
RankClassification            
1 VMS Base Metal

References

Data - Ontario Airborne Geophysical Surveys, Magnetic Data, Attawapiskat Area - Purchased Data

Publication Number: GDS1211 Scale:     Date: 2003

Author: Ontario Geological Survey

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 Scale:     Date: 2017

Author: Cundari R.M., Brunelle M.R., White G.D., Tuomi R.D., Tims A.

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 Scale:     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 Scale:     Date: 2012

Author: White G.D., Smyk M.C., Cooke A., Lockwood H.C., Wilson A.C.

Publisher Name: Ontario Geological Survey

Location:


Compend - Summary of Field Work and Other Activities, 2004

Publication Number: OFR6145 Scale:     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 Scale:     Date: 2007

Author: Stott, G.M., Corkery, T., Leclair, A., Boily, M. and Percival, J.

Publisher Name: Intitute on Lake Superior Geology

Location:


Compend - Summary of Field Work and Other Activities, 2010

Publication Number: OFR6260 Scale:     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:


Mono - Operation Fort Hope

Publication Number: MP042 Scale:     Date: 1970

Author: Thurston P.C., Carter M.W.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


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