Qi-Qin Accretionary Belt in Central China Orogen: accretion by trench jam of oceanic plateau and formation of intra-oceanic arc in the Early Paleozoic Qin-Qi-Kun Ocean

查看全文 作　　者：Shuguang [1]Song;Liming [1]Yang;Yuqi [1]Zhang;Yaoling [2,3]Niu;Chao [1]Wang;Li [4]Su;Yanlin [5]Gao

机构地区：[1]MOE Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871,China;[2]Department of Earth Sciences, Durham University, Durham DHI 3LE, UK;[3]Institute of Oceanology, Chinese Academy of Science, Qingdao 266071, China;[4]School of Scientific Research and State Key Laboratory of Geological Processes and Mineral Resources, Chinese University of Geosciences, Beijing 100083, China;[5]Qinghai Science & Technology Department, Xining 810000, China

出　　处：《Science Bulletin》索引2017年第62卷第15期,共4页

基　　金：supported by the Major State Basic Research Development Program (2015CB856105);National Natural Science Foundation of China (41572040 and 41372060) 摘　　要：Most orogenic belts have experienced a complex accretionary process with multiple episodes of sea?oor subduction and trench retreat.This accretionary process is important in continenta development and growth[1,2].Three giant orogens extend in China,e.g.,the Central Asian Orogen in the north,the Central China Orogen in the middle and the Himalayan Orogen in the southwest.They are keys for the formation of the Eurasian continent(Fig.1a).The Central China Orogen 关键词：中央造山带增生带早古生代堵塞沟槽弧形高原海洋

相关文献

参考文献（15）
引证文献（34）
耦合文献（28）

参考文献(15)

引证文献(34)

耦合文献(28)

互联网出版许可证新出网证(渝)字10号全国400电话 - 免长途话费

Qi-Qin Accretionary Belt in Central China Orogen: accretion by trench jam of oceanic plateau and formation of intra-oceanic arc in the Early Paleozoic Qin-Qi-Kun Ocean

参考文献(15)

引证文献(34)

耦合文献(28)

用户提示