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The Jinxi–Yelmand gold deposit is located in the late Paleozoic Tulasi intra-arc volcano-sedimentary basin in the Xinjiang Uygur Autonomous Province of northwest China. Although all known deposits in the Tulasi Basin were previously described as low-sulfidation epithermal systems, the recently discovered Jinxi–Yelmand deposit is interpreted here to be a modified high-sulfidation epithermal gold deposit...
The Uti gold deposit occurs within amphibolites of the late Archaean Hutti-Maski greenstone belt of southern India. Gold mineralization is associated with intense silicification, biotite-actinolite- and sulfide-rich alteration zones in between small anastomozing shear zones. Characteristic biotite-K-feldspar alteration and arsenopyrite thermometry constrain the mineralizing event to above 400 °C,...
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