Fluid inclusion geochemistry and 40Ar/39Ar geochronology constraints on the genesis of the Jianchaling Au deposit, China
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文摘

The Jianchaling giant Au deposit is hosted by a fault in the MLY area, Qinling Orogen.

The deposit was characterized by low-salinity and CO2-rich fluids.

Fuchsite Arsingle bondAr dating constrained the Au mineralization to ~ 200 Ma.

The Jianchaling is an orogenic gold deposit, and formed during continental collision.

The beginning of the continental collision between the Yangtze and the North China cratons took place ~ 200 Ma.

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