Orogenically-derived gold deposits of the Zhongchuan area in the west Qinling are distributed in the exocontact thermal metamorphic zone. The country rocks host
The Fenghuangshan Pluton is located in the Tongling polymineral-cluster district in the middle-lower section of the Yangtze metallogenic belt. In tectonic terms
The superlarge Baguamiao, large Liba and Xiaogouli gold deposits represent three typical gold deposits different from the Carlin type in the west Qinling Orogen