Mianlüe tectonic zone and Mianlüe suture zone on southern margin of Qinling-Dabie orogenic belt

作     者：ZHANG Guowei DONG Yunpeng LAI Shaocong GUO Anlin MENG Qingren LIU Shaofeng CHENG Shunyou YAO Anping ZHANG Zongqing PEI Xianzhi LI Sanzhong 

作者机构：Department of GeologyNorthwest UniversityXian 710069China Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100101China Earth Science and Resource FacultyChina University of GeosciencesBeijing 100083China Institute of GeologyChinese Academy of Geological SciencesBeijing 100037China Changan UniversityXian 710054China Qingdao University of OceanographyQingdao 266003China 

出 版 物：《Science China Earth Sciences》 (中国科学（地球科学英文版）)

年 卷 期：2004年第47卷第4期

页      面：300-316页

核心收录：

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 

基　　金：This work was supported by the National Natu-ral Science Foundation of China (Grant Nos. 49732080  40234041) 

主　　题：central orogenic system Mianle tectonic zone Mianle suture zone continental dynamics. 

摘      要：The Mianle tectonic zone (Mianle zone), an ancient suture zone in addition to the Shangdan suture in the Qinling-Dabie orogenic belt, marks an important tectonic division geo-logically separating north from south and connecting east with west in China continent. To de-termine present structural geometry and kinematics in the Mianle tectonic zone and to recon-struct the formation and evolution history involving plate subduction and collision in the Qinling-Dabie orogenic belt, through a multidisciplinary study, are significant for exploring the mountain-building orogenesis of the central orogenic system and the entire process of the major Chinese continental amalgamation during the Indosinian.