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Occurrence Details


Occurrence Number
105D 212
Occurrence Name
Suburban
Occurrence Type
Hard-rock
Status
Deposit


General Information

Primary Commodities: copper, gold
Aliases: Whitehorse Copper
Deposit Type(s): Skarn
Location(s): 60.659570 N, -135.113660 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. 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 Suburban occurrence is 250m southeast of the Artic chief deposit and occurs within the same pendant of Lewes River limestone as the Artic chief. Therefore it is likely that both deposits share similar geology and mineralization. The description for the Artic Chief is provided below:

The Arctic Chief pendent is characterized by copper rich skarn mineralization along the contact of the Lewes River limestone and the Laberge group greywacke/quartzite. The skarn mineralization consists of born mineralization, chalcopyrite, magnetite, valleriite, chalcocite, tetrahedrite, cuprite and pyrite. The calc-silicate minerals include serpentinite, phlogopite, red garnet, and rare wollastonite.

Between 1900 and 1907 it was determined that the grades ran 0.89% Cu and 1.03 g/t Au. The deposit was not mined.

Location Map

Last Updated: Mar 25, 2019

Work History

Year Work Type Comment
2002 Drilling: Diamond 2 holes completed
2002 Geochemistry: Drill Core
1980 Drilling: Diamond 7 holes completed
1980 Geochemistry: Drill Core
1976 Drilling: Diamond
1976 Geochemistry: Drill Core
1973 Geology: Bedrock Mapping
1966 Studies: Feasibility
1964 Drilling: Diamond

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
094325 2002 Diamond Drilling on Heather 3 Claim Diamond - Drilling, Drill Core - Geochemistry 2 118.26
090823 1980 [Diamond Drill Log - Whitehorse Copper Belt] Diamond - Drilling, Drill Core - Geochemistry 7 1208.83
091229 1976 [Diamond Drilling on the Arctic Chief Property] Diamond - Drilling, Drill Core - Geochemistry 1 212.44
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
062227 1966 An Evaluation of the New imperial Mines Ltd. Feasibility - Studies
091123 1964 Summary of assessment work for 316 claims Diamond - Drilling 46 3652.57

Related References

Number Title Page(s) Document Type
Citations
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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