Ministry of Energy, Northern Development and MinesPermanent Link to this Record: MDI52O11SW00012
|Deposit Name(s)||Altered Zone - 1985, East Bay Property - Altered - 2015, McVicar Lake #9 - 1959|
|Related Deposit Type||None|
|Date Last Modified||2019-Sep-26|
|Created By||Q Unknown|
|Revised By||T Pettigrew|
Primary Commodities: gold
Township or Area: McVicar Lake Area
Latitude: 51° 33' 45.59" Longitude: -91° 23' 32.15"
UTM Zone: 15 Easting: 611441 Northing: 5713623 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52O11SW
Point Location Description: Assessment file map (McKay 2004).
Location Method: data compilation
Source Map: MCVICAR LAKE (EDITION 1) 52O11
Sources Map Scale: 1:25 000
Access Description: Accessible year round via fixed-wing aircraft or helicopter from the town of Pickle Lake. A winter road from Pickle Lake to the First Nation community of Cat Lake is situated approximately 3 km south of the property. A backhoe trail leads from the winter road to the eastern portion of the property.
1959-62: Kenlew Mines Ltd. carried out mapping, stripping, trenching, magnetometer and EM surveys, and drilled 4 DDH totalling 221 m. 1985: BHP-Utah Mines carried out mapping, prospecting, airborne EM and magnetic surveys, and ground VLF-EM, mag, and HLEM surveys. 1987: BHP-Utah Mines Ltd. drilled 16 DDH totalling 1356.1 m. 2003: Continuum Resources Ltd. and Prospector Consolidated Resources Inc. carried out stripping, sampling, and drilled 2 DDH totalling 168 m. 2011: Wildcat Exploration carried out prospecting, channel, soil sampling, aeromagnetic, spectrometric, and EM geophysical surveys. 2016-17: Reliant Gold Corp. carried out prospecting and sampling.
|Office File Number||Online Assessment File Identifier||Online Assessment File Directory|
Belt: Lang Lake
Geological Age: Neoarchean
Tectonic Assemblage: Confederation
|Altered Zone Fault East Of Flexure||regional||300||45|
|Altered Zone West Of Flexure||regional||330||45|
|Surface Showing Foliation||local||302||43|
|Zone Of Mineralization||local||110||38|
03/29/2007 (M A Puumala) - The area geology is described in MDI52O11SW00007. The dominant structural feature in the area is the Bear Head fault zone, a southeaststriking, regional-scale, dextral shear zone classified by Stott and Corfu (1991) as a trans-crustal megafault. This fault zone extends approximately 515 km from Lake Winnipeg to the northern boundary of the Meen–Dempster greenstone belt (Osmani and Stott 1988). Two other west-northwest-trending deformation zones, referred to as the Lower McVicar fault and Altered Zone fault (McKay 2004), are also present in the area and are associated with a number of gold occurrences. Fumerton (1997) suggested a relationship between the Altered Zone fault and the axial plane of the regional syncline. Fumerton (1997) indicated that supracrustal rocks between the Bear Head and Lower McVicar faults have been folded into sigmoidal S-folds, and that a number of splay faults also exist in this area. The geometry of these structures has been interpreted as being consistent with a dextral sense of displacement (Fumerton 1997).
11/15/2011 (T Pettigrew) - The visited occurrences lie within the Lang Lake greenstone belt, which is dominated by tholeiitic basalt flows and calc-alkalic pyroclastic deposits; the eastern portion of the belt contains a significant clastic metasedimentary sequence that also includes iron formation horizons (Stott and Corfu 1991). The supracrustal rocks of this belt were provisionally assigned to the Confederation assemblage by Stott and Corfu (1991) based on a single age determination from a dacitic tuff in the lowermost (i.e., interpreted to be oldest) portion of the supracrustal sequence. The entire belt was isoclinally folded into an east-trending and east-plunging syncline (BHP–Utah Mines 1988). BHP–Utah Mines (1988) also indicated that the belt contains 2 significant intrusions, including a mafic stock in the Sor–McVicar lakes area, and a later felsic intrusion in the Shonia–McVicar lakes area that hosts several gold occurrences. The Altered Zone prospect is located at the eastern end of McVicar Lake, on the Altered Zone fault, which was described by BHP–Utah Mines (1988) as a northwest-trending ductile shear zone that is refracted north-northwest at a contact between mafic metavolcanic rocks and gabbro. Gold mineralization at the Altered Zone prospect occurs within a dilation zone in the fault structure that developed within this flexure (Puumala 2009). The deformation zone associated with the fault was reported to have a width of approximately 5 to 6 m to the northwest and southeast of the Altered Zone (BHP–Utah Mines 1988). McKay (2004) reported that the Altered Zone is exposed on surface over a total strike length of 150 m. Gold mineralization largely occurs in lenticular quartz ± iron carbonate veins with minor pyrite and rare chalcopyrite. Channel sampling carried out in 2003 returned assay values up to 12.77 g/t Au over 0.8 m. A summary of the results of earlier surface sampling is provided by Janes, Seim and Storey (1991). The main stripped area (UTM Zone 15: 611422 Easting / 5713642 Northing) exposes the east-southeast-trending deformation zone in gabbro. The zone is characterized by shallowly northeast-dipping foliation surfaces and iron carbonatization, sericitization and sulphidization. White, iron carbonate- and sericite-bearing quartz veins up to 2 m wide are boudinaged within this zone and contain finely disseminated pyrite.
|vein||1||quartz||veins and pods||host|
|gabbro||2||sheared and altered||adjacent|
|mafic metavolcanics||3||sheared and altered||adjacent|
|Rank||Mineral Name||Class||Economic Mineral Type||Alteration Mineral Type||Alteration Ranking||Alteration Intensity||Habit Description|
03/29/2007 (M A Puumala) - The Altered Zone prospect is located on the Altered Zone Fault, which is described by Thomas (1988) as a northwest-trending ductile shear zone that is refracted north-northwest at a contact between mafic metavolcanics and gabbro. To the southeast of the Altered Zone prospect, the fault strikes approximately 300 through the gabbro intrusion and dips steeply to the northeast. To the north of the gabbro-mafic metavolcanic contact, the fault strikes approximately 330. Gold mineralization at the Altered Zone prospect occurs within a dilation zone in the fault structure that developed within this flexure. The deformation zone associated with the fault is reported by Thomas (1988) to have a width of approximately 5 to 6 metres to the northwest and southeast of the Altered Zone. Within the Altered Zone, the area of deformation is reported to dilate to a with of approximately 20 m over a strike-length of 300m. McKay (2004) reports that the Altered Zone is exposed on surface over a total strike length of 150 m. Foliation in this portion of the shear zone varies in strike from 294 to 310 degrees and dips from 36 to 51 degrees to the northwest. Gold mineralization largely occurs in lens-shaped quartz +/- Fe-carbonate veins. These veins are indicated by McKay (2004) to be mineralized with minor pyrite and rare chalcopyrite. McKay reports that channel sampling carried out in 2003 provided assay results of up to 12.77 g/t over 0.8 m. A summary of the results of earlier surface sampling is provided by Janes, Seim and Storey (1991). Based on the results of an earlier diamond drilling program, Thomas (1988) describes the geology of the Altered Zone as consisting of sheared and/or brecciated basalt and gabbro, quartz-carbonate-sericite schist and apple green mica schist. The deformation zone also hosts significant quartz veining and pods of intermediate intrusive rock. Thomas (1988) indicates that pyrite mineralization occurs throughout the zone (generally 2-5%), and that visible gold also occurs in quartz veins. Gold mineralization also occurs in the altered wall rocks in association with pyrite, with grades generally proportional to the pyrite content. Thomas indicates that the gold mineralized dilation zone likely plunges 30 to 45 degrees to the east-southeast. McKay (2004) has also interpreted surface foliation trends and mineral elongation lineations as being indicative of shallow (15 to 31 degree) eastward to east-southeastward-plunging mineralized veins and ore shoots. In general, Thomas (1988) describes gold mineralization in the Altered Zone as consisting of widespread low-grade gold values interspersed with discrete high grade sections. The most significant assay reported from this zone by Thomas (1988) was 14 g/t Au in a 4.63 m interval of massive quartz from ddh ML-27. Other significant drill intersections are tabulated by McKay (2004).
09/26/2019 (T Pettigrew) - The 2003 stripping program exposed the Altered Zone for 150 m along strike. The width varies from 2.5 to 12.5 m. Extensive sampling conducted within Stripped Area AZ-03-05 indicates that the gold mineralization is localized primarily within discrete, syntectonic "fault-fill" quartz +I- Fe-carbonate veins. These veins are lens-shaped in plan and vary in size up to approximately 3 by 6 m. The veins typically contain trace to minor amounts of pyrite +/- rare chalcopyrite and locally contain narrow ribbons and septa of intensely altered, pyritic gabbro. Channel samples collected across the width of these veins returned assay values of up to 12.77 grams gold per tonne over 0.80 m (Assessment report 52O11SW2003). At trench area #3, weakly altered massive mafic metavolcanics host a series of north-trending intermediate feldspar porphyritic dykes. At the margins of one of the dykes a narrow (<1.5m) shear zone hosts a very narrow (1-10 cm) quartz vein. One grab sample taken from the vein contains 5% sulphides (Py, Po, Cp) and assayed 48,550 ppb Au, later examination revealed the presence of native gold. Trench area 2 is established on a xenolith of mafic metavolcanics within metagabbro. The mafic metavolcanics, in contrast to Trench area 3, are intensely altered with attendant shearing and quartz veining. Quartz veins and boudins in the shear zone are conformable to shearing and range from 0.1 m to 1.0 m in thickness. Extensive channel and grab sampling indicated that gold is principally contained within the quartz veins. The best sample obtained from this area is a grab sample of quartz which assayed 6990 ppb Au. BHP-Utah Mines drillhole ML-02 intersected 12 g/t Au over 0.82 m and DDH ML-18 intersected 7.3 g/t Au over 1.4 m (Assessment report 52O11SE0080). Continuum Resources’ DDH ML-03-01 assayed 5.72 ppm Au over 7.71 m, including up to 22.43 ppm Au over 0.75 m. DDH ML-03-02 assayed up to 1.112 ppm Au over 0.44 m (Assessment report 52O11SW2004).
Publication - Sioux Lookout Resident Geologist's District - 1990; in Report of Activities 1990, Resident Geologists, p. 67-105.
Publication Number: MP152 Date: 1991
Author: Janes, D.A, Seim, G.W. and Storey, C.C.
Publisher Name: OGS
Map - Precambrian Geology of the Lang Lake Greenstone Belt (West Half)
Publication Number: P3794 Scale: 1:20 000 Date: 2015
Author: Magnus, S.J.
Publisher Name: OGS
Map - Geological Series, Lang-Cannon Lakes Area (Central Part), District of Kenora (Patricia Portion)
Publication Number: P0665 Scale: 1:31 680 Date: 1971
Author: Fenwick, K.G.
Publisher Name: OGS
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For detailed information regarding this mineral deposit please contact the Thunder Bay North Resident Geologist District Office