An Anomalous Seamount on the Southwestern Mid-Ridge of the South China Sea

查看全文 作　　者：WANG [1,2]Yanlin;WANG [3]Jun;YAN [1]Pin;QIU [3]Yan 机构地区：[1]CAS Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,CAS;[2]Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology;[3]Guangzhou Marine Geological Survey 出　　处：《Acta Geologica Sinica(English Edition)》索引2017年第91卷第6期,共2页 基　　金：financially supported by the National Natural Science Foundation of China (grants No.91328205, 41376062 and 41206039);the Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology (grant No.MGQNLMKF201708);726 Plan (grant No.GZH201100205) 摘　　要：Objective The development of continental rifting and seafloor spreading can be predominated by magmatic upwelling(magma-rich)or tectonic stretching(magma-poor).Located in the terminal portion of propagating seafloor spreading of the South China Sea(SCS),the southwestern mid-ridge of the southwest sub-basin(SWSB)of the 关 键 词：An Anomalous Seamount on the Southwestern Mid-Ridge of the South China Sea