Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (4): 1142-1154.doi: 10.13278/j.cnki.jjuese.201504117

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Relation of Huangling Anticline and Landslide Group in the Three Gorges Reservoir Area

Wang Kongwei1, Zhang Fan1, Qiu Dianming2   

  1. 1. College of Civil Engineering and Architecture, Three Gorges University, Yichang 443002, Hubei, China;
    2. Editorial Department of Journal, Jilin University, Changchun 130026, China
  • Received:2014-12-24 Published:2015-07-26

Abstract:

The study to Huangling anticline-Zigui syncline in the Three Gorges area is hot in the field of structure geology. Predecessors thought that it was the result of a later reformation of the east-west structure, and classified it into Qinling orogenic belt. Another focus is whether Xiannü Mountain fault is across Yangtze River or not. To Solve these problems is of great importance for disclose the distribution of the geological disasters in the study area. The authors put forward a new opinion from sedimentology and tectonics based on the predecessors' studies and a lot of field work by the authors. Huangling anticline, Zigui syncline, Dangyang syncline, and Xiannü Mountain fault belong to one unified tectonic system. This is consistent with the formation and evolution of the fracture of the East-West China. Huangling anticline is the characteristics of fracture related fold, Zigui syncline has a foreland flexural basin syncline tectonic attribute, and Xiannü Mountain fault is the characteristics of the transfer fault with undergoing tension at first and compression later,and not going across Yangze River. Impacted by the east-west and south-north structures as well as Zigui syncline's subsidence range, the landslide accumulation areas are formed such as Jiajiadian landslide accumulation area, Bazimen-Xiangjadian landslide accumulation area, and Xingshan landslide accumulation area.

Key words: the Three Gorges reservoir area, Huangling anticline, Zigui syncline, landslide group, Qinling orogenic belt, Xiannü, Mountain fault

CLC Number: 

  • P542.2

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