Ontario Geological Survey
Permanent Link to this Record:
MDI000000000955
Record Name(s) | Wolf Zone - 2010, Peacock Showing - 2009 |
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Related Record Type | |
Record Status | Prospect |
Date Created | 2010-Nov-26 |
Date Last Modified | 2022-Jan-05 |
Created By | A Wilson |
Revised By | P Bousquet |
Primary Commodities: Gold
Township or Area: Hambleton
Latitude: 48° 48' 53.37" Longitude: -85° 1' 31.74"
UTM Zone: 16 Easting: 644952 Northing: 5408751 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42C14NE
Point Location Description: precise
Location Method: Based on Assessment
2008-2011: Corona Gold Corporation and Harte Gold Corporation - airborne geophysics, prospecting, sampling, ground geophysical survey, stripping, trenching, DD-37-6585m. 2011-2017: Harte Gold Corp. – DD – 2 – 333m, prospecting, sampling, geological mapping, assays, DD – 14 – 7346m, airborne geophysical survey, induced polarization survey, ground magnetic survey.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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WP Odlum.9 / 2.43277 | 20000005374 | 20000005374 |
WP Odlum.10 / 2.51495 | 20000008138 | 20000008138 |
WP Odlum.11 / 2.54077 | 20000009026 | 20000009026 |
WP Hambleton.23 / 2.55786 | 20000014193 | 20000014193 |
WP Hambleton.26 / 2.55782 | 20000014995 | 20000014995 |
WP Hambleton.28 / 2.58387 | 20000015086 | 20000015086 |
WP Hambleton.29 / 2.58388 | 20000015087 | 20000015087 |
WP Hambleton.30 / 2.58374 | 20000015432 | 20000015432 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Dayohessarah-Kabinakagami
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Contains |
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Vein | 2 | Quartz | Host | |
Quartz-Feldspar Porphyry | 3 | Quartz-Feldspar | Intrudes |
Sep 05, 2012 (A Wilson) - The auriferous Wolf Zone lies in the northern extent of the SDZ, but drilling between the two zones indicates that the zones are complexly separate from each other. Like the Sugar Zone, the Wolf Zone is north-northwesterly striking, and southwesterly dipping. Unlike the Sugar Zone, there is only one gold mineralized zone, and not two or more parallel zones. The auriferous Wolf Zone lies along strike of the Sugar Zone, and may represent the northern extension of the SDZ. It is defined as highly strained packages consisting of variously altered mafic volcanic flows and gabbros. The zone ranges in true thickness from 0.5 to 8 m. The zone is made up of highly sheared mafic volcanics, and a network of intrusive, intermediate quartz-feldspar porphyry dykes/sills. Alteration in the mafic volcanic and gabbro units consists mainly of silicification (both pervasive and quartz veining), diopside alteration and magnesium rich, brown biotite alteration. Alteration within the intermediate porphyry units consist of mostly silicification, with small amounts of magnesium-rich brown biotite, and no diopside. The zone is observed in trenches to pinch and swell over 30 m.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Pyrrhotite | Economic | Ore | ||||
4 | Molybdenite | Economic | Gangue | ||||
5 | Galena | Economic | Gangue |
Sep 05, 2012 (A Wilson) - A grab sample taken by G. Peacock from a boulder in 2009 returned 87.8 g/t gold. Follow up sampling by Harte Gold Corp. in 2010 returned 9.85 g/t Au, 52.8 g/t Au, 6.84 g/t Au and 37.3 g/t Au. Grab samples collected in 2010 from a trench located to the north of the original sampling returned 6.53 g/t Au and 5.97 g/t Au. Assays from drill hole NZ10-02 returned 9.5 g/t Au over 7.5 m, including 111 g/t Au over 0.5 m. Mineralization consists of disseminated sulphides with visible gold. Gold mineralization mostly occurs in quartz veins, stringers and quartz flooded zones predominantly associated with porphyry zones, and hydrothermally altered basalts and gabbros. Fine grained specks of visible gold are occasionally observed in the Wolf Zone quartz veins. The visible gold itself is often observed to be concentrated within thin fractures, indicating some degree of remobilization. Quartz veins and floods also contain varying amounts of pyrrhotite, pyrite and occasional galena. The presence of galena is a strong indicator of the presence of visible gold. Pyrite and pyrrhotite form most of the total sulphides, but do not appear to be directly related to the presence of gold mineralization. Assays from WZ-10-16 returned values of 7.33 g/t Au over 7.33 m, including 21.6 g/t Au over 0.45 m. Assays from WZ-10-18 returned values of 4.8 gt Au over 5 m, including 15.4 g/t Au over 1.5 m and 35.1 g/t Au over 0.5 m.
Rank | Classification |
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1 | Vein |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 600 | 20 |
Map - Precambrian Geology, Dayohessarah Area (Central)
Publication Number: P3310 Scale: 1:20,000 Date: 1995
Author: Stott G.M., Mahoney K.L., Zwiers W.G.
Publisher Name: Ontario Geological Survey
Mono - Precambrian Geology of the Dayohessarah Lake Area, White River, Ontario
Publication Number: OFR5984 Scale: Date: 1999
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Publication - Press realeases
Publication Number: Scale: Date: 2010
Author: Harte Gold Corp.
Publisher Name:
Publication - NI 43-101 Technical Report on the Preliminary Economic Assessment of the Sugar Zone Project, North-western Ontario, Canada, for Harte Gold Corp.
Publication Number: NI 43-101 Scale: Date: 2012
Author: M. Buck, A.S. Hayden, B. LeBlanc
Publisher Name:
Publication - NI 43-101 Technical Report and mineral resource update for the Dayohessarah Lake Property Sugar Zone Project, Ontario, Canada, for Harte Gold Corp., 133 p.
Publication Number: NI 43-101 Scale: Date: 2012
Author: M.W. Kociumbas, D. Power-Fardy
Publisher Name:
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