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Occurrence Details


Occurrence Number
105D 225
Occurrence Name
Carlisle
Occurrence Type
Hard-rock
Status
Deposit


General Information

Primary Commodities: copper, gold, silver
Aliases: Whitehorse Copper, Tamarac-Carlisle
Deposit Type(s): Skarn
Location(s): 60.738530 N, -135.139120 W
NTS Mapsheet(s): 105D11
Hand Samples Available at YGS: No

Capsule

The Whitehorse Copper Belt is located west of Whitehorse and contains 30+ mines, deposits and showings. By 1900, most of the important deposits had been discovered and the first small ore shipment was made that year. Many of the occurrences in the Copper Belt are skarns. The skarns form on or near the contact between the Whitehorse batholith and the Lewes River group. The Whitehorse batholith is commonly a grey coarse-grained hornblende granite and ranges from quartz monzonite to granodiorite to diorite. The Lewes River group contains numerous different rock types, most importantly of which is the limestone group, which is essential in the formation of skarns in the area.  A small number of occurrences within the Copper Belt are vein and/or replacement and occur within the Whitehorse batholith granite.

The Carlisle mine is located within an irregularly shaped roof pendant of limestone and skarn, some 600 feet in diameter. The pendant is enclosed to the north, south and east by the Whitehorse batholith hornblende granite. Towards the west is the larger limestone section, which contains the Copper King deposit. The contact zones in the vicinity are marked by an intense alteration of the Lewes River limestone to brown garnet (andradite) and epidote. The principal ore at Carlisle is bornite and chalcopyrite with a tremolite-rich gangue. When the dump was tested with a UV lamp, a minor amount of white scheelite was present in the quartz rich specimens, in silicified garnet, and in siliceous skarn. A quartz rich specimen with scheelite was assayed and showed 0.005 ounce per ton (0.16 g/t) Au and 0.75% WO3.

Production from the Carlisle mine totalled 907 tonnes of ore at 3.58% Cu, 0.34 g/t Au and 51.4 g/t Ag. 

Location Map

Regional Geology - Terrane

Group: Intermontane
Affinity: W Laurentia
Name: Stikinia
Realm: peri-Laurentian


Regional Geology - Bedrock

Supergroup:
Group/Suite: Lewes River
Formation: Aksala
Member: Hancock
Terrane: Stikinia
Period Max: Triassic
Age Max: 217 MA
Period Min: Triassic
Age Min: 204 MA
Rock Major: conglo/limestone/dolostone
Rock Minor: chert
Reference: Hart & Radloff (1990) - YGS OF 1990-4
Geological Unit (1M): uTrAK
Geological Unit (250K): uTrAK2

Assessment Reports that overlap occurrence

Report Number Year Title Worktypes Holes Drilled Meters Drilled
093895 1997 Assessment Report for the Exploration Work on the DM 1-8 Quartz Mining Claims Rock - Geochemistry, Line Cutting - Other, Prospecting - Other, Hand - Trenching, Handblast - Trenching, Mechanical - Trenching
093635 1996 Assessment Report for the Exploration Work on the DM 1-8 Quartz Mining Claims Rock - Geochemistry, Line Cutting - Other, Prospecting - Other, Mechanical - Trenching
062018 1973 Preliminary Report on Geological Control to Ore Distribution in the Whitehorse Copper Belt Reverse Circulation - Drilling, Bedrock Mapping - Geology, Petrographic - Lab Work/Physical Studies 665 5555
018884 1967 Geological Mapping, Magnetometer and Electro Magnetic Survey Detailed Bedrock Mapping - Geology, EM - Ground Geophysics, Magnetics - Ground Geophysics, Line Cutting - Other
091123 1964 Summary of assessment work for 316 claims Diamond - Drilling 46 3652.57

Related References

Number Title Page(s) Document Type
ARMC004783 Correspondence Re: Copper King - Carlisle Drilling Miscellaneous Company Documents
Citations
Carriere, J J, et al. “Copper Deposits and Occurrences in Yukon Territory.” Ottawa: Geological Survey of Canada, 1982, 1981, doi:10.4095/109350.
Kindle, E.D., “Summary of Research: Field, 1962”; Geological Survey of Canada, Paper no. 63-1, 1963, https://doi.org/10.4095/121464 (Open Access)

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