Advances in Earth Science ›› 2017, Vol. 32 ›› Issue (5): 488-501. doi: 10.11867/j.issn.1001-8166.2017.05.0488

Special Issue: 青藏高原研究——青藏科考

• Orginal Article • Previous Articles     Next Articles

River Geomorphic Evolution Connected to Tectonics Around the First Bend of Yangtze River

Yaling Tao 1, 2( ), Hong Chang 1, *( )   

  1. 1.Institute of Earth Environment,Chinese Academy of Sciences,Xi’an 710075, China
    2.University of Chinese Academy of Sciences,Beijing 100049, China
  • Received:2017-01-10 Revised:2017-03-10 Online:2017-05-20 Published:2017-05-20
  • Contact: Hong Chang E-mail:taoyl@ieecas.cn;changh@loess.llqg.ac.cn
  • About author:

    First author:Tao Yaling (1988-), female,Jingchuan County, Gansu Province, Master student. Research areas include tectonic geomorphology and fluvial geomorphology.E-mail:taoyl@ieecas.cn

  • Supported by:
    Project supported by the National Natural Science Foundation of China “Asia interior aridification and westerlies evolution since the Oligocene”(No.41290250)

Yaling Tao, Hong Chang. River Geomorphic Evolution Connected to Tectonics Around the First Bend of Yangtze River[J]. Advances in Earth Science, 2017, 32(5): 488-501.

The origin and formation time of the first bend are important scientific problems in the Yangtze River system and the evolution of the river system, even tectonic research around the southeastern margin of the Qinghai-Tibet Plateau. These problems have attracted the attention of many domestic and international scholars and they hold two different opinions. one is river capture hypothesis; another hypothesis is river natural adaptation to terrain. It is necessary to get reliable geological evidences and chronological data in order to reconstruct the evolution history of the Yangtze River. In the recent years, much work has been done to study the evolution history of the Yangtze River. Thus, it is possible now to integrate all the relevant chronological data and geological evidences to understand the evolution of Yangtze River.

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