Mineral Range Tungsten Project
District-scale tungsten project comprising 25 granted claims and 84 applications covering ~838 hectares in the Mineral Range, Utah
The Project includes ~12km of prospective mineralisation linked to the Mineral Range batholith, with a well-understood geological setting focused on scheelite-bearing skarn zones at the contact between granite and limestone.
Significant brownfield upside with modern exploration to target extensions of known mineralisation at depth and along strike
The Project area includes multiple past producing mines with robust production data summarized and published in a June 1957 report Tungsten Deposits of the Mineral Range, Beaver County, Utah.
The Mineral Range Tungsten Project, Beaver County, Utah, USA
Geology
The Mineral Range batholith, which forms the structural core of the range, is the primary source of mineralisation in the district. The batholith intruded the surrounding Paleozoic carbonate rocks altering them to scheelite-bearing, garnet-rich skarn assemblages along the 12-km intrusive contact.
The Paleozoic host rocks are exposed continuously on the eastern front of the range as vertical to sub-vertical dipping marble, dolostone, and skarn beds. Scheelite occurs both finely disseminated throughout the skarn and in higher-grade concentrations along fractures, shears, and other structural conduit.
Board members, Gary Lyons, Mathew Walker and Teck Wong accompany local partner Burgex Mining Consultants founder Stuart Burgess and lead geologist Kirk Schleiffarth on a recent site visit
Historical workings and trenching along strike of the Garnet mine.
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