Testing the geologically testable hypothesis on subduction initiation

查看全文 作　　者：Yaoling [1,2,3]Niu

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

出　　处：《Science Bulletin》索引2016年第61卷第16期,共5页

基　　金：supported by National Natural Science Foundation grant(41130314);Chinese Academy of Sciences Innovation grant(Y42217101L);grants from Qingdao National Laboratory for Marine Science and Technology(2015ASKJ03);for Marine Geological process and Environment(U1606401) 摘　　要：‘‘Resolution of the sixty-year debate over continental drift,culminating in the triumph of plate tectonics,changed the very fabric of Earth science.Plate tectonics can be considered alongside the theories of evolution in the life sciences and of quantum mechanics in physics in terms of its fundamental importance to our scientific understanding of the world.’’[1] 关键词：假设检验地质引发俯冲板块构造大陆漂移地球科学量子力学

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Testing the geologically testable hypothesis on subduction initiation

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