Ontario Geological Survey
Permanent Link to this Record:
MDI53D16NE00006
Record Name(s) | Borland Lake - 1979, Beatrice Lake - 1979, Barymin - 1979, Johnston - 9999 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect With Reported Reserves or Resources |
Date Created | 1979-May-10 |
Date Last Modified | 2022-Sep-26 |
Created By | |
Revised By |
Primary Commodities: Silver, Gold, Lead, Zinc
Township or Area: Borland Lake Area
Latitude: 52° 56' 13.21" Longitude: -94° 6' 28.76"
UTM Zone: 15 Easting: 425535.46 Northing: 5865837.21 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 53D16NE
Point Location Description: Precise
Location Method: Data Compilation
Access Description: Accessible by float or ski equipped aircraft. Approximately 200 km N of Red Lake. Winter road available in the cold months
1961-1964: Noranda Exploration Company drilled 2 DDH totalling 62.48 m. 1962: Noranda drilled 8 DDH totalling 750.11 m. 1963: Noranda drilled 7 DDH totalling 55.19 m. 1964: Noranda drilled 8 DDH totalling 1001.57 m. 1965: Astrabrun Mines Ltd. drilled 4 DDH totalling 547.7 m along the Borland Lake trend. 1978: Union Oil Company of Canada conducted a program of geological mapping, soil geochemical sampling and radiometric surveying immediately west of the Borland Lake Showing. 1981: Noranda conducted an exploration program that included linecutting, ground magnetometer surveying, and pulse and EM surveys. 1985: Massive Energy Ltd. optioned the property from Noranda and drilled 19 DDH totalling 1577 m. 1986: Massive conducted detailed magnetics and IP surveys and drilled 6 DDH totalling 924 m. 1987: Massive drilled 3 DDH totalling 643 m. Massive terminated their option agreement with Noranda after the fall of precious and base metal prices in the late 1980s. 2005: claims staked by Gold Canyon Resources Inc. Gold Canyon signed a joint venture agreement with Shoreham Resources Ltd. 2006: Shoreham conducted an exploration program including linecutting, airborne magnetic and EM geophysical surveys, sampling and prospecting. 2008 Gold Canyon completed AEM,AM, ARA surveys and completed line cutting and prospecting. 2009: Shoreham changes its name to Guyana Frontier Mining Corp. 2010: Guyana Frontier completed a drill program of 12 DDH totalling 4072.66 m. 2011: Guyana Frontier drilled 2 DDH totalling 236 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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RL AF # 53D/16NE # 11 | 53D16NE0013 | 53D16NE0013 |
RL AF # 53D/16NE #16 | OM84-1C-235 | OM84-1C-235 |
RL AF # 53D/16NE # 17 | OM86-1-C-15 | OM86-1-C-15 |
RL AF # 53D/16NE #18 | OM87-1C-001 | OM87-1C-001 |
2.38651 | 20000003103 | 20000003103 |
2.50176 | 20000007854 | 20000007854 |
10 | 53D16NE0014 | 53D16NE0014 |
63.4865 | 53D16NE8136 | 53D16NE8136 |
63.4834 | 53D16NE0006 | 53D16NE0006 |
2.38466 | 20000003044 | 20000003044 |
2.34895 | 20000002124 | 20000002124 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Belt: Favourable Lake
Geological Age: Archean
Feb 27, 2015 (Therese Pettigrew) - The subject property is dominantly underlain by mafic to intermediate metavolcanic, metavolcaniclastic and metasedimentary rocks comprising the Favourable Lake-Setting Net greenstone belt. These stratified rocks are locally deformed and intruded by intermediate to felsic intrusives (Blanchflower, 2006).
Rock Type | Rank | Composition | Texture | Relationship | Sandstone | 1 | Greywacke | Contains |
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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 | Argentite | Economic | Ore | ||||
3 | Galena | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Pyrrhotite | Economic | Ore | ||||
6 | Sphalerite | Economic | Ore | ||||
7 | Arsenopyrite | Economic | Ore | ||||
Garnet | Alteration | Garnetization | 1 | Unknown | Disseminated |
Nov 02, 2007 (Mark Puumala) - Johnson (1987) reported that the Borland Lake prospect consists of two parallel approximately east-striking, silicified, silver-bearing shear zones (north and south zones) hosted by metasedimentary rocks (greywacke). Blanchflower (2007) reports the presence of a mineralized shear oriented 280/80. The deposit was delineated by diamond drilling over a total strike length of 365 m, in an area located immediately to the east of an ultramafic intrusion (Johnson 1987). The two parallel shear zones have been named the north and south zones, with the north zone having an average thickness of 2.1 m and the south zone having an average thickness of 3.2 m. According to Johnson (1987), silver mineralization occurs in three distinct ¿cigar-shaped¿ lenses that plunge to the southeast at approximately 45 degrees. Each of these lenses is reported to cover a strike length of approximately 46 m and is open at depth. Mineralization is reported to consist of varying amounts (in order of abundance) of pyrrhotite, pyrite, argentite, galena, sphalerite and arsenopyrite (Johnson 1987). The total sulphide content of the mineralized zones typically does not exceed 10%, and the sulphides occur as irregular stringers and disseminations along foliation and shear planes. A distinct zone of garnet alteration is reported by Johnson (1987) to occur in the hanging wall sediments. The most notable structural feature in the vicinity of this prospect is the approximately 300-striking Bear Head fault zone, which is located immediately to the north (as shown on ODM Map 2262). Geological information compiled by Blanchflower (2007) also indicates that foliations in the area generally trend 300 with steep northerly dips, and that this fabric is axial planar to commonly-observed tight/isoclinal folds. North-trending and northeast-trending faults are also reported to occur in the area. Blanchflower (2007) reports that a non-NI 43-101 compliant reserve estimate of 431,967 tons grading 8.43 oz/ton Ag and 0.02 oz/ton Au was calculated for this deposit by Massive Energy in 1986. Significant gold and silver assay results from the historical diamond drilling programs carried out on this deposit are compiled by Blanchflower (2007). It should also be noted that this deposit also hosts significant lead and zinc mineralization. Surface chip samples (covering 1 m2) collected by Blanchflower (2007) assayed up to 2.67% Zn and 2.18% Pb.
Feb 27, 2015 (Therese Pettigrew) - The most significant intercepts of the 2010 drill program were in Hole 6 (75.2 grams Ag/tonne, 6.04% Zn, 0.55% Pb across a true width of 0.5 meters), Hole 7 (0.3 g/t Au, 118.8 g/t Ag, 1.4% Zn and 1.8% Pb across a true width of 2.6 meters), Hole 11 (two intercepts including 2.13 g/t Au, 14.5 g/t Ag, 0.46% Zn and 1.38% Pb across a true width of 1 meter and 1.7 g/t Au, 170.0 g/t Ag, 1.9% Zn and 1.19% Pb across a true width of 2.0 meters), and hole 13 (19.5 g/t Ag and traces of the other reported metals across a true width of 18.1 meters) (Guyana Frontier press release, Oct 27, 2010). DDH B-11-01 encountered silver, gold, lead and zinc mineralized veinlets, disseminated sulphides and breccias from 76.8 to 90.8 m within siliceous metagreywacke and quartzite rocks, and in two other mineralized intervals between 92.1 and 108.9 m downhole. Sulphides containing argentite were noted in the core, with accompanying sphalerite, pyrrhotite and pyrite. The estimated true width of the mineralized interval was 7.7 m (25.26 ft), which averaged 291 g/t (8.49 ounces per ton) silver, including 365 g/t (10.65 oz/ton) silver over 6.08 m (19.94 ft). Minor values of gold, lead and zinc were also encountered. Hole B-11-02 was collared approximately 84 m from Hole B-11-01 and intersected mineralized zones at downhole depths of 23.8 to 64.5 m, and from 67.7 to 73.7 m. Mineralization was again observed within siliceous metagreywacke and quartzite rocks with notably higher silver and gold values than were seen in B-11-01, averaging 99 g/t (2.89 oz/ton) silver and 1.03 g/t gold over an estimated true width of 30.53 m (100.14 ft), which included 285 g/t (8.3 oz/ton) silver and 1.63 g/t (0.05 oz/ton) gold over 8.53 m (27.98 ft), and 438 g/t (12.78 oz/ton) silver and 2.99 g/t gold (0.09 oz/ton) over 4.6 m (15.1 ft). Pegmatites were observed cutting through the mineralized zones, from 64.5 to 66.24 m, for example (Guyana Frontier press release, June 12, 2011).
Rank | Classification |
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1 | Vein (Polymetallic) |
Rank | Characteristic |
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1 | Sheared |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 46 | 152 | 45 |
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
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Borland Lake | 1986 | Probable | 431967 | Blanchflower, 1996 | Gold .02 Ounce per Ton, Silver 8.43 Ounce per Ton |
Publication - Report on the Favourable Lake Property
Publication Number: Tech Rep Date: 2006
Author: Blanchflower, J.D.
Publisher Name: Minorex Consulting for Shoreham Resources
Location: Gold Canyon website
Map - Precambrian Geology, Deer Lake Area
Publication Number: P3381 Scale: 1:250,000 Date: 1998
Author: Stone D.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian geology, Borland Lake
Publication Number: P3177 Scale: 1:50,000 Date: 1990
Author: Stone D., Good D.J.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological compilation series, Favourable Lake-Poplar Hill area, Deer Lake sheet, District of Kenora (Patricia Portion)
Publication Number: P0768 Scale: 1:126,720 Date: 1972
Author: Ayres L.D., Raudsepp M., Averill S.A., Edwards G.R.
Publisher Name: Ontario Division of Mines
Location:
Mono - Silver cobalt calcite vein deposits of Ontario
Publication Number: MDC010 Page: 37 Date: 1968
Author: Sergiades A.O.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 184 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
File - Report on the Favourable Lake Property (Non-assessment report)
Publication Number: AF RL5088 Date:
Author: Blanchflower, J.D. 2007.
Publisher Name:
Location: Red Lake RGP
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