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

Most orogenic belts have experienced a complex accretionary process with multiple episodes of seafloor subduction and trench retreat. This accretionary process is important in continental development and growth .

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Bibliographic Details
Published inScience bulletin Vol. 62; no. 15; pp. 1035 - 1038
Main Authors Song, Shuguang, Yang, Liming, Zhang, Yuqi, Niu, Yaoling, Wang, Chao, Su, Li, Gao, Yanlin
Format Journal Article
LanguageEnglish
Published Netherlands Elsevier B.V 15.08.2017
Subjects
中央造山带
堵塞
增生带
弧形
早古生代
沟槽
海洋
高原
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Summary:Most orogenic belts have experienced a complex accretionary process with multiple episodes of seafloor subduction and trench retreat. This accretionary process is important in continental development and growth .
Bibliography:Most orogenic belts have experienced a complex accretionary process with multiple episodes of seafloor subduction and trench retreat. This accretionary process is important in continental development and growth .
10-1298/N
ISSN:2095-9273
2095-9281
DOI:10.1016/j.scib.2017.07.009