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The Sartohay chromitite deposit, hosted in the Sartohay ophiolite mélange in western Junggar (Xinjiang province, NW China), contains irarsite, breithauptite, and Fe–Ni–As–S minerals. Petrographic observations indicate that the chrome-spinel was firstly altered to Fe-rich chromite at low-temperature with relatively lower Fe3+/Fe2+ ratios (0.14–0.34), and such Fe-rich chromite was altered to magnetite...
The Sayi gold deposit is part of the Sartohay ophiolitic mélange in west Junggar, Xinjiang, China, and is hosted by listwaenite, which was transformed from serpentinite in a shear zone via fluid–rock reaction. Gold mineralization is hosted by mylonitized listwaenites and quartz veins within listwaenite lenses, formed during shearing. Our study demonstrates that fluid concentrated Au, Ag, As, Sb, Cu,...
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