Ontario Geological Survey
Permanent Link to this Record:
MDI42A11SE00006
Record Name(s) | Owl Creek - 1967 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Past Producing Mine With Reserves or Resources |
Date Created | 1984-Aug-31 |
Date Last Modified | 2022-Sep-21 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Hoyle, Hoyle
Latitude: 48° 33' 2.08" Longitude: -81° 8' 21.67"
UTM Zone: 17 Easting: 489716 Northing: 5377507 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A11SE
Point Location Description: Centre of open pit.
Location Method: AMIS Site Visit
Access Description: Access to the Kinross Gold Corporation's property is via gravel road extending from Florence Ave in Porcupine, Ontario. This road arrives at the security gatehouse, whereby one is accompanied to the open pit by Kinross personnel.
1966-1973: International Nickel Co. - DD-5-1058 m, ground and airborne geophysics. 1978-84: Kidd Creek Mines Ltd. - DD-16-5578m. 1986-87: Syngold Exploration Inc. and Falconbridge Ltd. - DD-51-28,522 ft., resource calculation. 1982-1989: Kidd Creek Mines Ltd. - mine operated as open pit.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-3232 / OM86-5P-121 / 63.5196 | 42A11SE0913 | 42A11SE0913 |
T-3232 / OM87-5L-111 / 63.5127 | 42A11SE0115 | 42A11SE0115 |
T-1321 / 15 | 42A11SE0103 | 42A11SE0103 |
T-1321 | 42A11SE0102 | 42A11SE0102 |
T-1321 | 42A11SE0086 | 42A11SE0086 |
30 | 42A11SE0072 | 42A11SE0072 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Tisdale
Geological Age: Neoarchean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Nov 04, 2011 (R Pressacco) - All of the stratigraphic units at Owl Creek strike in an east-northeasterly direction, with dips being generally to the north ranging from 45 to 90 deg. The host unit to the gold mineralization is a small massive basalt unit separated from a larger band of easterly striking mafic/ultramafic rocks by a thin interval of interbedded greywacke and argillitic sediments. Diamond drilling information has shown that this small basalt unit is a folded portion of the larger band to the north.
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Mg-Tholeiite | Massive/Pillowed, Local Variolitic+Amyg | Host |
---|---|---|---|---|
Terrigenous-Clastic-Unsubdivided | 2 | Greywacke | Interbedded Arkosic Wackes And Argillite | Near |
Mudstone | 3 | Graphitic Argillite | Strongly Schistose | Near |
Nov 04, 2011 (R Pressacco) - Stratigraphic tops in the mafic volcanic rocks are towards the south in the southern portions of the open pit. Textures are dominated by massive to pillowed flows with locally developed variolitic and amygdaloidal textures. These basalts have been variably altered by an assemblage of carbonate and sericite, resulting in a light grey to buff colouration. The greywackes are in fault contact on both the north and south contacts of the basalt flows, with a unit of strongly sheared carbonaceous argillite marking the fault contact. The greywackes are lithologically identical to greywackes of the Porcupine Assemblage and are composed of interbedded light to medium grey arkosic wackes and darker grey argillite typical of distal turbidites within a submarine fan environment. Graphitic argillites are the least abundant rocks at Owl Creek, and their distribution is confined to both the north and south contact of the basalt where they typically contain a sheared texture. The northern graphitic argillite ishighly sheared and is the locus of some of the quartz veining present in the open pit.
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 | ||||
1 | Quartz | Economic | Gangue | ||||
Carbonate | Alteration | Carbonatization | 1 | Strong | Disseminated | ||
Sericite | Alteration | Unknown | 2 | Strong | Disseminated | ||
Quartz | Alteration | Unknown | 3 | Weak | Disseminated | ||
Chlorite | Alteration | Unknown | 4 | Weak | Stockwork |
Nov 04, 2011 (R Pressacco) - Gold content is proportional to content of disseminated pyrite in altered portions of the Mg-tholeiitic basalt unit. Some native gold, at times in spectacular amounts, is present in quartz veins, stockworks, and breccia zones.
Rank | Classification |
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1 | Hydrothermal |
Rank | Characteristic |
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2 | Breccia |
1 | Disseminated |
3 | Sheared |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
---|---|---|---|---|---|---|---|---|---|
Tabular | 300 | 50 | 90 | 84 | 74 |
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
---|---|---|---|---|---|---|
Owl Creek West | 1997 | Assay | 6530954 | OFR5985 p. 188 | 682,559 contained ounces | Gold 3.58 Grams per Tonne |
Owl Creek East | 1997 | Assay | 3019685 | OFR5985 p. 188 | 696,371 contained ounces | Gold 7.17 Grams per Tonne |
Year | Tonnes | Commodities | Reference | Comment |
---|---|---|---|---|
1990 | 151904 |
Gold 542540 Grams |
OFR5985 P. 188 | AVERAGE GRADE 4.1 GPT AU, MILL RECOVERY 88.2% |
1989 | 158645 |
Gold 617833 Grams |
OFR5985 P. 188 | AVERAGE GRADE 4.7 GPT AU, MILL RECOVERY 83.3%, CASH COST $US250/OZ |
1988 | 99996 |
Gold 509542 Grams |
OFR5985 P. 188 | AVERAGE GRADE 5.4 GPT AU, MILL RECOVERY 93.6%, CASH COSTS $US290/OZ |
1987 | 175444 |
Gold 805055 Grams |
OFR5985 P. 188 | AVERAGE GRADE 5.3 GPT AU, MILL RECOVERY 86.9%, CASH COSTS $US196/OZ |
1986 | 150979 |
Gold 675088 Grams |
OFR5985 P. 188 | AVERAGE GRADE 5.8 GPT AU, MILL RECOVERY 76.9%, CASH COSTS $US213/OZ |
1985 | 280000 |
Gold 1092014 Grams |
OFR5985 P. 188 | AVERAGE GRADE 3.9 GPT AU |
1984 | 280000 | OFR5985 P. 188 | AVERAGE GRADE 4.0 GPT AU | |
1983 | 239000 |
Gold 979899 Grams |
OFR5985 P. 188 | AVERAGE GRADE 4.1 GPT AU |
1982 | 250000 |
Gold 1024994 Grams |
OFR5985 P. 188 | AVERAGE GRADE 4.1 GPT AU |
Book - Gold 86 - Excursion Guidebook, p. 34-36
Publication Number: Date: 1986
Author: J. Pirie and M.J. Downes (ed)
Publisher Name:
Location: Timmins RGO
Book - Northern Miner 78-11-23, Gold Group, p. 1, 23
Publication Number: NMINER Date: 1996
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 79-11-15, Owl Creek, p. 1, 11
Publication Number: NMINER Date: 1996
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 81-03-05, Texasgulf, p. B9
Publication Number: NMINER Date: 1996
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 82-02-11, Kidd Creek, p. A1, A2
Publication Number: NMINER Date: 1996
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Book - Northern Miner 84-03-17, Kidd Creek, p. 21
Publication Number: NMINER Date: 1996
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Date: 1983
Author: Hodgson C.J.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1988
Publication Number: MP142.012 Page: 235 Date: 1997
Author: Luhta L.E., Sangster P.J., Draper D.M., Ireland J.C., Bradshaw M.P., Hamblin C.D.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1989
Publication Number: MP147.012 Page: 232 Date: 1997
Author: Luhta L.E., Sangster P.J., Ireland J.C., Hamblin C.D., Bradshaw M.P.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology, Hoyle Township
Publication Number: M2532 Scale: 1:20,000 Date: 1998
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Precambrian Geology, Hoyle and Gowan Townships
Publication Number: R299 Page: 31-32 Date: 1998
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Special Project: Timmins Ore Deposit Descriptions
Publication Number: OFR5985 Page: 169-198 Date: 1999
Author: Pressacco R.E.
Publisher Name: Ontario Geological Survey
Location:
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