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作 者:Yaoling Niu Jie Tang
机构地区:[1]Department of Earth Sciences, Durham University,Durham DH1 3LE, UK [2]Institute of Oceanology, Chinese Academy of Sciences,Qingdao 266071, China [3]Qingdao National Laboratory for Marine Science and Technology (Marine Geology), Qingdao 266061, China [4]College of Earth Sciences, Jilin University, Changchun 130061,China
出 处:《Science Bulletin》2016年第14期1076-1080,共5页科学通报(英文版)
基 金:supported by National Natural Science Foundation of China(41130314,91014003);Chinese Academy of Sciences Innovation Grant(Y42217101L);Qingdao National Laboratory for Marine Science and Technology(2015ASKJ03);Marine Geological Process and Environment(U1606401)
摘 要:Niu et al.[1]recently show that the basement of the Chinese continental shelf(beneath East China Sea and South China Sea)is geologically unrelated to the continental lithosphere of eastern China,but is of exotic origin.Niu et al. [1] recently show that the basement of the Chinese continental shelf (beneath East China Sea and South China Sea) is geologically unrelated to the continental lithosphere of eastern China, but is of exotic origin. This alien/exotic terrane of a sizeable mass with large compositional buoyancy (either an oceanic plateau or a micro continent) was transported along with the Pacific plate that spread in the course of NW direction and subducted beneath the eastern margin of the continental China in the Mesozoic.
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