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Ontario Geological Survey
Permanent Link to this Record:
MDI000000003172
Record Name(s) | Joy Zone - 1978, Dixie 24 - 1978 |
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Related Record Type | |
Related Record(s) | |
Record Status | Prospect |
Date Created | 2022-Oct-03 |
Date Last Modified | 2022-Oct-04 |
Created By | |
Revised By |
Primary Commodities: Copper
Secondary Commodities: Zinc, Silver
Township or Area: Gerry Lake Area
Latitude: 50° 55' 17.98" Longitude: -93° 9' 1.02"
UTM Zone: 15 Easting: 489437 Northing: 5641124 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52K14NE
Point Location Description: DDH 24-1 from map in Assessment report 52K14NE2015
Location Method: Data Compilation
1976-78: Selco Mining Corp. Ltd. carried out line cutting and mag and EM surveys. 1978: Selco drilled 10 DDH totalling 2867 m, including 4 DDH totalling 1377 m on the zone. 1985: BP Resources Canada Ltd. conducted magnetometer and VLF-EM surveys. 1992: Noranda Exploration Company Ltd. drilled 4 DDH totalling 969 m, including 1 DDH totalling 334.1 m on the zone. 1993-94: Noranda and joint venture option partners Major General Resources and Pathfinder Resources drilled 14 DDH totalling 4454.8 m, including 4 DDH totalling 1023.8 m on the zone, and conducted borehole EM surveys. 2021: Trillium Gold Mines Inc. carried out a spatiotemporal geochemical hydrocarbon soil sampling program.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.2412 | 52K14NE0035 | 52K14NE0035 |
27 | 52K15NE0206 | 52K15NE0206 |
2.2698 | 52K14NE0021 | 52K14NE0021 |
36 | 52K14NE8947 | 52K14NE8947 |
OM94-045 | 52K14NE2015 | 52K14NE2015 |
2.15736 | 52K14NE0030 | 52K14NE0030 |
2.17026 | 52K14NE0045 | 52K14NE0045 |
2.17974 | 52K14NE0049 | 52K14NE0049 |
4154, 4159, 4160 | 20000019724 | 20000019724 |
2.8604 | 52K14NE0013 | 52K14NE0013 |
2.9916 | 52K14NE0005 | 52K14NE0005 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Confederation Lake
Geological Age: Archean
Metamorphism Grade: U Grnst - L Amp
Oct 03, 2022 (Therese Pettigrew) - The Joy property is generally overlain by overburden cover up to 30 m in thickness. Interpretation of geology is based largely on ground geophysics, diamond drilling, and limited outcrop on the northern portion of the property. The Joy Property is underlain by an east-west to east-northeast trending, steeply south dipping sequence of volcanic rocks which consist of undifferentiated, strongly altered and metamorphosed felsic to intermediate pyroclastics and subvolcanic quartz-feldspar porphyritic intrusives. This sequence is underlain to the north by basalt flows, and has been intruded to the south by regional granitic to granodiorite intrusives. The volcanic rocks are representative of the third cycle of volcanism of the Confederation Lake Volcanic Belt. The volcanic rocks exhibit widespread hydrothermal alteration mineral assemblages consisting of chlorite-biotite-sericite-cordierite garnet ± anthophyllite. The observed alteration mineral assemblages are consistent with hydrothermally altered volcanics typical of a VMS mineralizing environment which have been overprinted by a strong (ie upper greenschist-lower amphibolite) regional metamorphic event (Assessment report 52K14NE2015).
Rock Type | Rank | Composition | Texture | Relationship | Intermediate Tuff | 1 | Adjacent |
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Felsic Crystal Tuff | 2 | |||
Quartz-Feldspar Porphyry | 3 |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrrhotite | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Sphalerite | Economic | Ore |
Oct 03, 2022 (Therese Pettigrew) - The Joy property host several zones of Cu-Zn rich massive to stringer sulphide mineralization localized along at least two stratigraphic horizons within the felsic pyroclastic volcanics. The northern horizon hosts the Joy-Diamond Willow-Creek zones over a 2.3 km strike length while the southern horizon hosts the South and Caravelle zones. The former is characterized by Cu-rich Zn mineralization, while the latter is characterized by Zn-rich mineralization with little or no Cu enrichment. The Joy Zone was discovered by shallow drilling carried out by Selco and was tested by four diamond drill holes along strike for 150 m to a depth of 90m. Mineralization is hosted by a strongly altered felsic fragmental and consists of massive to stringer sulphides dominated by pyrrhotite, chalcopyrite and minor sphalerite. Best DDH hole intersection (24-1) returned 3.01% Cu, 0.20% Zn over 5.7 m including 7.2% Cu, 0.75% Zn, and 0.84 oz/t Ag over 4.3 feet from a massive sulphide unit (75% pyrrhotite, 20% chalcopyrite, 2-4% sphalerite, 1-3% chlorite) in an intermediate tuff breccia. DDH 150-24-6 returned up to 4.22% Cu, 0.59% Zn, and 0.21 oz/t Ag over 1 foot from an intermediate tuff with 20% pyrrhotite, 20% pyrite, and 5% chalcopyrite (Assessment report 52K15NE0206). DDH 92-1 returned 4.01% Cu, 0.17% Zn, and 0.49 opt Ag over 3.35 m, including 8.45% Cu, 0.6% Zn, and 0.77 opt Ag over 0.5 m and 11.4% Cu, 0.2% Zn, 0.59 opt Ag over 0.5 m from a massive sulphide zone in a intermediate tuff (Assessment report 52K14NE8947). The Joy-Diamond Willow horizon has now been systematically tested to the -200m level for a 2.5 km strike length. Numerous small lenses of Cu +/- Zn bearing massive sulphide mineralization have been outlined within intensely altered felsic volcanic pyroclastics. The Joy and Diamond Willow Zones both remain open down plunge at the -300m level (Assessment report 52K14NE2015).
Rank | Classification |
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1 | VMS Base Metal |
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For detailed information regarding this mineral record please contact the Red Lake Resident Geologist District Office