LI Yuan
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, ChinaLI Yuan.2018. Detachment-accretion formed the Xigaze Ophiolite along the southern margin of the Eurasian Plate in southern Tibet[J]. Acta Geologica Sinica(),92(z2):15
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