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

查看全文 作  者:ZHANG Guowei1, DONG Yunpeng1, LAI Shaocong1, GUO Anlin1, MENG Qingren2, LIU Shaofeng3, CHENG Shunyou1, YAO Anping1, ZHANG Zongqing4, PEI Xianzhi5 & LI Sanzhong6 1. Department of Geology, Northwest University, Xian 710069, China;2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101, China;3. Earth Science and Resource Faculty, China University of Geosciences, Beijing 100083, China;4. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;5. Changan University, Xian 710054, China;6. Qingdao University of Oceanography, Qingdao 266003, China 高影响力作者 出  处:《Science China Earth Sciences》索引2004年第47卷第4期,共17页高影响力期刊 基  金:This work was supported by the National Natu-ral Science Foundation of China (Grant Nos. 49732080, 40234041). 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. 关 键 词:CENTRAL OROGENIC system, Mianlue TECTONIC zone, Mianlue SUTURE zone, CONTINENTAL dynamics.
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