The Jianchaling giant Au deposit is hosted by a fault in the MLY area, Qinling Orogen.
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The deposit was characterized by low-salinity and CO2-rich fluids.
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Fuchsite ArAr dating constrained the Au mineralization to ~ 200 Ma.
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The Jianchaling is an orogenic gold deposit, and formed during continental collision.
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The beginning of the continental collision between the Yangtze and the North China cratons took place ~ 200 Ma.
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