Influence of fluid-rock interaction on gold mineralization in the Dongwan deposit, East Qinling, China: Constraints from systematic sulfur isotope and trace element geochemistry
Ore Geology Reviews(2022)
Abstract
•The four generations of pyrite have distinguished trace element and sulfur isotope features.•The ore-forming materials were derived from mantle-related source.•The main mechanisms of gold precipitation are fluid-rock interaction and decrease of temperature.
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Key words
Trace element,Sulfur isotope,Fluid-rock interaction,Dongwan Au deposit,Qinling orogenic belt
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