Red Star
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Red Star is approximately 3,005 hectares in size (398 unpatented federal lode mining claims) and is adjacent to the Star mining district, Utah. Surface alteration and mineralization suggests the presence of a porphyry copper system beneath post-mineral cover composed of volcanics and alluvium. Polymetallic (Pb-Zn-Ag-Cu-Au) fissure veins, mantos, and local Zn-rich skarn are hosted in east-tilted and fault-repeated Paleozoic carbonate rocks in the Star mining district. These fissure veins may be analogous to fissure veins found in the periphery of the Bingham and Tintic districts. Red Star also shares a similar regional geophysical signature with Bingham and Tintic porphyry copper deposits, each lying within ENE-trending aeromagnetic domains considered to be representative of Tertiary batholiths (see Figure 3). The timing of Tertiary magmatism in Utah youngs southward such that the age of an undiscovered porphyry system at Red Star would likely be ~34-27 Ma.. At Red Star, known polymetallic fissure veins and replacement mantos, and a copper-zinc skarn occurrence (Moscow mine), define a WSW-trending vector towards a 2.0 x 1.5 km porphyry target area with anomalous geophysics (Spartan IP-MT and UAV magnetics). The primary target zone starts about 1.5 km west of the Moscow mine skarn.
Red Star Location
