A newly found Paleozoic Japan-type subduction–accretion system

作     者：Chun-Ming Wu 

作者机构：College of Earth Science University of Chinese Academy of Sciences 

出 版 物：《Science Bulletin》 (科学通报（英文版）)

年 卷 期：2015年第60卷第23期

页      面：2069-2070页

核心收录：

学科分类：070904[理学-构造地质学] 070903[理学-古生物学与地层学(含：古人类学)] 0709[理学-地质学] 07[理学] 

主　　题：增生杂岩 日本式 古生代 系统 俯冲 蛇绿混杂岩 板块边缘 弧后盆地 

摘      要：Accretionary orogenic belts are complicated collages composed of magmatic arcs,accretionary complexes,ophiolitic me′langes,fore-arc/back-arc basins and microcontinents formed at convergent plate margins,which are key sites of continental growth through earth history[1].Arcs are important orogenic components of accretionary orogenesis,but the types of active margin with old continental basement and intraoceanic arcs without continental basement and their roles in accretionary orogenesis are *** Japan-type arc is a special kind of arc