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作 者:HAN Qingsen PENG Songbai Ali POLAT Timothy KUSKY
机构地区:[1]School of Earth Sciences, China University of Geosciences [2]Center for Global Tectonics, School of Earth Sciences, China University of Geosciences [3]Wuhan 430074, China3.State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences [4]Department of Earth and Environmental Sciences, University of Windsor
出 处:《Acta Geologica Sinica(English Edition)》2016年第S1期215-216,共2页地质学报(英文版)
基 金:supported by the fundings (No. 41272242) from National Natural Science Foundation of China
摘 要:Ophiolites represent fragments of ancient oceanic lithosphere,tectonically incorporated into continental margins during plate subduction or remained in the subduction–collisional orogenic belt.They provide
关 键 词:META GA A Paleoproterozoic Ophiolitic M Orosirian lange
分 类 号:P542[天文地球—构造地质学] P588.3[天文地球—地质学]
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