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Ontario Geological Survey
Permanent Link to this Record:
MDI42L04NE00014
Record Name(s) | Knucklethumb Lake - 1915, Kipper-Cameron - 1915, R.J. Noffke - 1991, Big Bear - 1997, Claim Line - 1997, Jaz - 1997 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1991-Jan-13 |
Date Last Modified | 2022-Feb-17 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Oboshkegan
Latitude: 50° 9' 54.06" Longitude: -87° 33' 54.28"
UTM Zone: 16 Easting: 459641.52 Northing: 5557131.06 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42L04NE
Point Location Description: Precise
Location Method: Data Compilation
Access Description: The Knucklethumb Lake property is located 53 km north of Jellicoe and approx. 72km northeast of the town of Geraldton. A logging road that extends north for 100km from the Trans-Canada Highway 11 comes within 1 km of the property.
1915: Albert Kipper discovered gold south of Hull Lake and west of Knucklethumb Lake. 1976: NWT Copper Mines Ltd. drilled 1 hole. Hollinger Argus Ltd. electromagnetic survey south of area. 1980-81: Hollinger Argus Ltd. carried out a mag survey and drilled 6 DDH totalling 443.2 m. 1984: Geological, Lithoogeochemical, VLF-EM and MAG surveys by S.N. Roach. 1987: Humus sampling, IP, ground electromagnetic surveys done by Noranda under option from S.N. Roach. 1996: Mapping by G. Stott and J. Parker (OGS). 1996: Cameco acquires area by option from NWT Copper Mines Ltd. and by staking. 1997-99: Cameco Gold Inc. carried out line cutting, ground magnetic and IP/resistivity surveys, geological mapping, trenching and drilled 4 DDH totalling 1195 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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23 | 42L04NE0104 | 42L04NE0104 |
25 | 42L04NE0092 | 42L04NE0092 |
2.19772 | 42L03NW2006 | 42L03NW2006 |
14 | 42L04NE0112 | 42L04NE0112 |
2.20676 | 42L04NE2017 | 42L04NE2017 |
2.11416 | 42L04NE0070 | 42L04NE0070 |
2.11468 | 42L04NE0066 | 42L04NE0066 |
2.8940 | 42L04NE0083 | 42L04NE0083 |
2.10589 | 42L04NE0512 | 42L04NE0512 |
2.3612 | 42L04NE0098 | 42L04NE0098 |
Province: Superior
Subprovince: Wabigoon
Terrane: Eastern Wabigoon
Belt: Onaman-Tashota
Geological Age: Archean
Dec 07, 2005 (Q Unknown) - The property is located in the north-central portion of the Onaman-Tashota metavolcanic belt. Specifically, the property occurs within the Metcalfe Lake Metavolcanic belt. Amukun (1977) mapped the area east of Metcalfe Lake as being underlain by mafic to felsic metavolcanic rocks. Felsic metavolcanic rocks consist of rhyolite, rhyodacite, rhyolite porphyry, pyroclastic breccia and sericite schist. Mafic metavolcanic rocks consist of massive to pillowed basalt, and are foliated to strongly sheared. South and east of Knucklethumb Lake is a metasedimentary unit composed of slate, greywacke and conglomerate. Horebelned-quartz monzonite and gabbro intrude these metasedimentary rocks. Coarse-grained 'golfball' anorthosite and gabbroic rocs intrude the mafic metavolcanic rocks east of Hull Lake.
Rock Type | Rank | Composition | Texture | Relationship | Intermediate Pyroclastic Breccia | 1 | Calc-Alkaline Dacite To Rhyoli | Pyroclastic Ash Flow | Near |
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Mafic lava flow-unsubdivided | 2 | Tholitic Basalt | Massive To Pillows | Near |
Mafic lava flow-unsubdivided | 3 | Calc-Alkaline Basalts | Massive To Pillowed | Near |
Chert | 4 | Mineralized | Fine Grained - Exhalite | Host |
Lamprophyre-Unsubdivided | 5 | Lamprophyre | Dikes | Near |
Gabbro | 6 | Metagabbro | Coarse Grained Basaltic Flows | Near |
Granite | 7 | Fine Grained | Near | |
Diabase | 8 | Diabase | Dikes | Near |
Terrigenous-Clastic-Unsubdivided | 9 | Near |
Dec 07, 2005 (Q Unknown) - The Knucklethumb Lake property is located in an extensive felsic sequence that is 26 square km. The property consists of 94% felsic to intermediate metavolcanics, 5% mafic metavolcanics, and 1% metasedimentary rocks. Thin lamprophyre dikes cross-cut the metavolcanics. A small granitic intrusion lies to the south of the property.
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 | Chalcopyrite | Economic | Ore | ||||
4 | Pyrrhotite | Economic | Ore | ||||
5 | Arsenopyrite | Economic | Ore | ||||
Albite | Alteration | Feldspathization | 1 | Unknown | Disseminated | ||
Quartz | Alteration | Silicification | 2 | Unknown | Disseminated | ||
Sericite | Alteration | Sericitization | 3 | Unknown | Disseminated | ||
Chlorite | Alteration | Chloritic | 4 | Unknown | Disseminated |
Oct 30, 2018 (Therese Pettigrew) - The Big Bear showing (located at NAD83 UTM Zone 16 458925 m E, 5557514 m N) assayed 16 gpt Au from a grab sample. The Jaz showing assayed 3.1 gpt Au over 1.5 m. The Claim Line showing (located at NAD83 UTM Zone 16 460271 m E, 5557106 m N) assayed 145.2 gpt Au over 0.3 m. There are 4 styles of gold mineralization on the property: 1) auriferous hypabyssal intrusions porphyries/felsites) emplaced within intermediate to felsic fragmental volcanics, e.g., Hourglass and Ryne showings; 2) gold within highly altered (silicified/feldspathized, carbonatized, sulphidized) deformation zones, e.g., Ryne and Cabin showings; 3) gold within pyrite chalcopyrite pyrrhotite-bearing quartz-iron carbonate veins, e.g., Big Bear, MVP and Green Jimmy showings; and 4) free gold within quartz-tourmaline veins, felsite dykes and along shear/foliation planes, e.g., Claimline, Hourglass and Ryne showings. DDH OB-2-2-80 assayed up to 1.03 gpt Au over 1.52 m. DDH OB-2-3-80 assayed up to 4.8 gpt Au over 0.6 m. DDH ONA99-32 assayed up to 0.55 gpt Au over 3.0 m (AFRI 42L03NW2006).
Dec 07, 2005 (Q Unknown) - The Gold occurrences extend over a strike length of 1600m, but the width is very limited. Both sulphides and quartz veining are present within felsic volcanic rocks, but the mineralization is confined to narrow, tight shear zones. The largest occurrence on the property is the RYNE showing.
Dec 07, 2005 (Q Unknown) - Alteration is mainly due to strong shearing and fracturing. Altered rocks contain disseminated pyrite and arsenopyrte.
Rank | Classification |
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1 | Metamorphic |
Rank | Characteristic |
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1 | Sheared |
2 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown |
Date: Sep 16, 1999
Geologist: Q Unknown
Notes: MVP: occurs in mafic volcanics. The basalts are veined with calcite and are cut by narrow qtz. veins containing vuggy pyrite. The volcanics are moderately sheared. The qtz vein contains 5% pyrite and trace chalcopyrite. RYNE: consists of qtz veinlets and stringers hosted by a carbonatized felsic volcanic flow (tuff?). A 1cm carbonate rind is very evident when the rock is broken. The felsic volcanic contains 3-4% very fine grained pyrite. Minor qtz veining was observed in an outcrop at 17+35E on the baseline. No arsenopyrite was located at this showing. CLAIM LINE: hosted by felsic rocks (prob. tuffs). The area is characterized by intense sericitic alteration and moderate to strong shearing across a 5m width. A long trench has been blasted which measures 5m long by 3m wide by 2m deep. Sheared felsic volcanics with minor qtz veining is exposed along the trench wall. Stretched felsi blebby pyrite occurs in the felsic volcanic (up to 3%). Tourmaline was noted in qtz veins near a drill site just to the west of the pit. JAZ: is hosted by felsic to intermediate tuffaceous rocks. A very narrow shear zone crosses the outcrop and this zone contains narrow qtz veinlets and minor sulphides. The sulphides are primarily concentrated in the centre of the outcrop in a small pod with limited strike extent.
Book - NMINER HIST FILE T.BAY
Publication Number: NMINER Scale: Date: 1996
Author:
Publisher Name:
Location:
Map - Tashota, Thunder Bay District
Publication Number: M2354 Scale: 1:31,680 Date: 1976
Author: Amukun S.E.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Geology of the Tashota area, District of Thunder Bay
Publication Number: R167 Scale: Date: 1977
Author: Amukun S.E.
Publisher Name: Ontario Geological Survey
Location:
Part - Tashota-Onaman gold area (District of Thunder Bay)
Publication Number: ARV34-06.003 Scale: Date: 1998
Author: Gledhill T.L.
Publisher Name: Ontario Dept. of Mines
Location:
Book - GEOLOGICAL COMPILATION OF KNUCKLETHUMB LAKE PROPERTY
Publication Number: MIN DEP Scale: Date: 1994
Author: Roach, S.N.
Publisher Name:
Location: 42L04NE MINERAL DEPOSIT FILE
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