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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 被引量:32
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作者 Shuguang Song Liming Yang +4 位作者 Yuqi Zhang Yaoling Niu Chao Wang Li Su Yanlin Gao 《Science Bulletin》 SCIE EI CAS CSCD 2017年第15期1035-1038,共4页
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].Thre... 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 展开更多
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
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