U-Pb zircon, Re-Os molybdenite geochronology and Rb-Sr geochemistry from the Xiaobaishitou W (-Mo) deposit: Implications for Triassic tectonic setting in eastern Tianshan, NW China
The Xiaobaishitou deposit is characterized by typical calc-silicate mineralogy.
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Re–Os and U–Pb dating constrained the mineralization to 242–240 Ma.
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Re contents and Sr isotope suggest the fluids were sourced from granite and carbonate.
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The Xiaobaishitou is a skarn deposit formed in a tectonic transition setting.
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