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Ontario Geological Survey
Permanent Link to this Record:
MDI52O06NE00004
Record Name(s) | Dobie Zone - 1990, Dobie Lake # 3 - 1990 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect With Reported Reserves or Resources |
Date Created | 1990-Nov-28 |
Date Last Modified | 2024-Jun-10 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Dobie Lake Area
Latitude: 51° 22' 52.53" Longitude: -91° 13' 38.18"
UTM Zone: 15 Easting: 623365 Northing: 5693715 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O06NE
Point Location Description: OFR5869 p. 160
Location Method: Conversion from MDI
Access Description: The Dobie Zone is located about 71 km west of Pickle Lake and about 500 m east of Tonsil Lake (local name for the first lake downstream on the Dobie River from Dorothy Lake). Tonsil Lake is marginal for float and ski equipped aircraft. Helicopter access of this occurrence is recommended.
1960-80: Umex and Inco conducted airborne and ground geophysical surveys and limited diamond drilling for base metals in the mid-1970s. UMEX subsequently drilled on the Dobie Zone. 1986: Geocanex Ltd. and St. Joe Canada Inc. commissioned separate airborne mag and EM surveys over areas including the Dobie Zone. 1986: St. Joe Canada Inc. did ground mag, EM and IP surveys on the Dobie Grid and drilled the initial holes intersecting the Dobie Zone. 1987: St. Joe Canada Inc. did diamond-drilling on the Dobie Zone. 1988: Bond Gold Canada Inc. did additional geophysical surveys and geological mapping in the area and completed additional drill holes. 1990: Bond Gold Canada Inc. did further diamond- drilling. 2006: Canadian Golden Dragon Resources Ltd. conducted geological mapping. 2007: Canadian Golden Dragon conducted prospecting. 2008: the property was transferred to Trillium North Minerals Ltd.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.28126 | 52O06NE2001 | 52O06NE2001 |
2.32497 | 20000001402 | 20000001402 |
52O06NE8898 | 20000006239 | 20000006239 |
52O06NE8897 | 20000005720 | 20000005720 |
12 | 52O06NE0011 | 52O06NE0011 |
10 | 52O06NE0014 | 52O06NE0014 |
2.32496 | 20000001401 | 20000001401 |
2.12224 | 52O06NE0012 | 52O06NE0012 |
2.38316 | 20000003427 | 20000003427 |
2.35257 | 20000002214 | 20000002214 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Meen-Dempster
Geological Age: Neoarchean
Dec 07, 2005 (B Nelson) - This occurrence consist of what Bond Gold Canada Inc. refers to as the Dobie Zone and the Dobie North Zone. The Dobie North Zone is located about 100 m north of the Dobie Zone towards the latter's west end. The Dobie Zone and the Dobie North Zone are hosted in a succession of mafic metavolcanic flows and tuffs with interbeds of iron formation. The succession is cut by quartz-feldspar porphyry dykes. Both zones trend southeast and dip north. They are characterized by strong shearing, silicification, carbonatization and sericitization. They are mineralized with up to 8% pyrite and pyrrhotite with traces of chalcopyrite and arsenopyrite. The sulphides occur as massive bands, stringers, blebs and disseminations.
Mar 10, 2015 (Therese Pettigrew) - The Dobie Lake property lies within the northwestern portion of the Meen-Dempster greenstone belt, in the Uchi Lake Subprovince, near the northern margin of the Dobie Lake batholith. The belt consists of three volcanic cycles, each of which is dominated by massive to pillowed tholeiitic flows capped by intermediate-felsic pyroclastics. Stratigraphic tops are to the southwest and dips are generally vertical to slightly overturned to the south. Major deformation zones along the northern and southern boundaries of the Meen-Dempster belt have been interpreted as contact strain aureoles. Work suggests that the northern deformation zone that lies near the granite-greenstone boundary represents the southeastern end of a major fault zone (Bear Head Fault zone) which extends to the northwest for approximately 515 km to Lake Winnipeg and has a consistent dextral sense of movement. Along the northern contact, the main shear often lies within the Dobie batholith, however secondary shears transect the greenstone belt near the margin. Additionally, a system of conjugate shear bands occur with decreasing intensity and frequency away from the granite greenstone contact. The Golden Patricia Gold mine and the Dobie Lake Zone prospect are related to shear zones thought to be splays off the main shear/deformation zone to the north (AFRI 20000001401).
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Alteration/Shear Zone | Host |
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Ironstone-unsubdivided | 2 | Near | ||
Quartz-Feldspar Porphyry | 3 | Quartz/Feldspar Porphyry | Near |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Gold | Economic | Ore | ||||
2 | Arsenopyrite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Pyrrhotite | Economic | Ore | ||||
Quartz | Alteration | Silicification | 1 | Unknown | Disseminated | ||
Unspecified | Alteration | Carbonatization | 2 | Unknown | Disseminated | ||
Unspecified | Alteration | Sericitization | 3 | Unknown | Disseminated |
Dec 07, 2005 (B Nelson) - RESERVE CATEGORY: Drill Inferred, 301 000 tonnes at 5.5g/t Au.
Mar 10, 2015 (Therese Pettigrew) - Mineralization in the Dobie Zone is found between the deformed and altered amphibolite and the sheared felsic volcanics below. Mineralization is restricted to a variably sheared, locally silicified, biotitic alteration zone which contains at or near its base a narrow crack seal, greyish, cherty quartz vein. The quartz vein varies in width from 2 mm to 28 cm and is generally within 10 cm of the base of the alteration zone. Gold values range from <1g/t Au to 20 g/t Au (AFRI 20000002214).
Rank | Classification |
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1 | Lode (Gold) |
Rank | Characteristic |
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1 | Sheared |
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
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Dobie Zone | 1993 | Unclassified | 301000 | OFR 5869 (Seim 1993). | The average grade is reported to be 5.5 g/t. Estimate pre-dates NI 43-101. | Gold 5.5 g/t |
MonoMap - Geology of the Cat Lake-Pickle Lake area, districts of Kenora and Thunder Bay
Publication Number: R207 Date: 1982
Author: Sage R.P., Breaks F.W.
Publisher Name: Ontario Geological Survey
Location:
Map - Cat Lake-Pickle Lake, geological compilation series, Kenora and Thunder Bay districts
Publication Number: M2218 Scale: 1:253,440 Date: 1976
Author: Sage R.P., Breaks F.W., Troup W.R.
Publisher Name: Ontario Division of Mines
Location:
Mono - Mineral Deposits of the Central Portion of Uchi Subprovince, Volume 1, Meen Lake to Kesagiminnis Lake Portion
Publication Number: OFR5869 Page: 160-163 Date: 1993
Author: Seim G.Wm.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian geology, Muskegsagagen-Bancroft lakes area, District of Kenora (Patricia Portion)
Publication Number: M2507 Scale: 1:50,000 Date: 1986
Author: Stott G.M., Wilson A.C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Precambrian geology, Meen Lake area, eastern part, Kenora District (Patricia Portion)
Publication Number: P2620 Scale: 1:15,840 Date: 1983
Author: Stott G.M., LaRocque C.
Publisher Name: Ontario Geological Survey
Location:
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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office