HAN Chunming
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2 Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, ChinaXIAO Wenjiao
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2 Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, ChinaAO Songjian
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaZHANG Jien
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaSONG Dongfang
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaZHANG Zhiyong
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaSONG Shuaihua
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaXIE Mingcai
1 Key Laboratory of Mineral Resource, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaWe are indebted to Prof. Li Xianhua, Mao Jingwen, Cui Bin, Qin Kezhang, Zhang Lianchang, and Yang Jianming for thoughtful discussions. Many of the ideas in this paper were initiated and rectified during these discussions. This study was financially supported by funds of the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK0801) and the National Key R&D Program of China (Grant Nos. 2021YFC2901704). This paper is a contribution to the ILP (ERAS) and IGCP 480.
HAN Chunming, XIAO Wenjiao, AO Songjian, ZHANG Jien, SONG Dongfang, ZHANG Zhiyong, SONG Shuaihua, XIE Mingcai.2022. Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China[J]. Acta Geologica Sinica(),96(2):525-535
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