This website uses cookies so that we can provide you with the best user experience possible. Cookie information is stored in your browser and performs functions such as recognising you when you return to our website and helping our team to understand which sections of the website you find most interesting and useful.
Rosy, YT
Highlights
- 61 km2 road-accessible property is located 77 km east of Whitehorse, surrounding the Red Mountain Molybdenum deposit (owned by Tintina Mines Ltd.)
- Numerous low sulphidation epithermal quartz-carbonate veins occur on the property
- Anomalous gold in soil over 3 x 2.5 km with untested high priority follow up areas with significant gold- and copper-in-soil
- Rock samples have returned up to 35.92 g/t gold with 32.4 g/t silver
- Potential for regional-scale epithermal vein mineralization
Rosy Geology & Mineralization
The Rosy property is predominantly underlain by Devonian to Mississippian aged metasedimentary and metavolcanic rock of the Yukon-Tanana Terrane. The southern end of the property has been intruded by 184.28 ± 0.07 Ma Early Jurassic Sawtooth Pluton, which is composed of weakly foliated hornblende-biotite granodiorite. In the northern part of the property, the 81.2 ± 0.9 Ma Late Cretaceous quartz monzonite Boswell Pluton, which hosts the Red Mountain Molybdenum deposit, intrudes Yukon-Tanana rocks. Numerous cream-to-pink weathering quartz-feldspar porphyry dykes cut the Sawtooth Pluton and are commonly flanked by quartz-carbonate veins and/or carbonate altered wallrock. Primary structural features in the southern part of the property are a series of strong north-south trending linears and less obvious, secondary northeast-southwest trending linears that cut the primary structural trend.
Gold and silver mineralization is associated with orange weathered quartz-ankerite-calcite-sericite-arsenopyrite-pyrite bearing veins. The mineralized veins typically display crustiform, colloform and cockade textures all indicative of a low-sulphidation epithermal system.