YANG Jingsui
Center for Advanced Research on the Mantle (CARMA), Key Laboratory of Deep Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaPaul ROBINSON
Center for Advanced Research on the Mantle (CARMA), Key Laboratory of Deep Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaXU Xiangzhen
Center for Advanced Research on the Mantle (CARMA), Key Laboratory of Deep Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaXIONG Fahui
Center for Advanced Research on the Mantle (CARMA), Key Laboratory of Deep Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaLIAN Dongyang
Center for Advanced Research on the Mantle (CARMA), Key Laboratory of Deep Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaYANG Jingsui, Paul ROBINSON, XU Xiangzhen, XIONG Fahui, LIAN Dongyang.2018. Diamond in oceanic peridotites and chromitites: Evidence for deep recycled mantle in the global ophiolite record[J]. Acta Geologica Sinica(),92(z2):42
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