ZHANG Lan
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.2 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaYANG Jingsui
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.Paul T. ROBINSON
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.XIONG Fahui
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.CHEN Yanhong
2 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaLAI Shengmin
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.2 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaCHEN Mei
1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.2 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaWe thank Ba Dengzhu for assistance with the field work, Rong He for the microprobe analyses and the China National Research Center for the geochemical analyses. This research was funded by National Natural Science Foundation of China (Grant No. 40930313) and the China Geological Survey (Grants No. 12120114061801; No.12120114057701; and No.12120114061501).
ZHANG Lan, YANG Jingsui, Paul T. ROBINSON, XIONG Fahui, CHEN Yanhong, LAI Shengmin, CHEN Mei.2015. Origin of Listwanite in the Luobusa Ophiolite, Tibet, Implications for Chromite Stability in Hydrothermal Systems[J]. Acta Geologica Sinica(),89(2):402-417
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