ZHANG Li
1 School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 2 CARMA, State Key Laboratory forContinental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaYANG Jingsui
1 School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 2 CARMA, State Key Laboratory forContinental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 3 Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, ChinaLIAN Dongyang
2 CARMA, State Key Laboratory forContinental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 3 Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, ChinaLIU Fei
CARMA, State Key Laboratory forContinental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaZHAO Hui
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaHUANG Jian
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaYANG Yan
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaZHANG Li, YANG Jingsui, LIAN Dongyang, LIU Fei, ZHAO Hui, HUANG Jian, YANG Yan.2015. Gongzhucuo Massif: An Ever Slightly Depleted Peridotite in the Western Yarlung Zangbo Ophiolitic Belt of Southern Tibet[J]. Acta Geologica Sinica(),89(z2):117-119
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