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作 者:Meng-xu Guo Jia-jun Liu De-gao Zhai Guo-ming Weng Rui Zhu
机构地区:[1]State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China [2]Zaozigou Gold Mine,Zhaojin Mining Industry Co.Ltd.,Hezuo 747000,China
出 处:《China Geology》2024年第3期586-588,共3页中国地质(英文)
基 金:supported by Records of China’s Mineral Geology from the China Geological Survey(DD20190379);the State Key Program of National Natural Science Foundation of China(41730426);the 111 Project of the Ministry of Science and Technology(BP0719021)。
摘 要:1.Objective The West Qinling Orogen extends east-west over 1500 km and is endowed with dozens of large-super large scale gold deposits.The Zaozigou gold deposit has a proven reserve of 134 t with an average grade of 3.08 g/t thus is one of the largest deposits in the West Qinling Orogen.However,whether the fluid type is metamorphic or magmatichydrothermal and ore-formation processes of the Zaozigou gold deposit are equivocal.Scheelite is a ubiquitous accessory mineral in geologically diverse ore-deposit types and attested to be a strong indicator of ore-forming conditions and oredeposit genesis.
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