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| Mianle tectonic zone and Mianle suture zone on southern margin of Qinling-Dabie orogenic belt | |
| 作者单位： | 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 |
| 摘 要： | The Mianle tectonic zone, defined as a series of fault zones consisting mainly of south-verging thrusts and nappes, represents the south boundary of the Qinling-Dabie orogenic belt. The north side of the eastern end of the Mianle tectonic zone adjoins the exposure of the Dabieshan UHP rocks. Further to east, the zone was offset by the Tanlu faults and moved to eastern Shandong Province. While to its west, across the Qinghai-Tibetan Plateau, the zone was dislocated by the Altun fault, and… |
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