Volume 47 Issue 2
Feb.  2022
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Chen Yingying, Li Yiquan, Wei Dongtao, Mao Yuqiong, Wang Xianyan, 2022. Quantitative Relationship between Tectonic Deformation and Topography in Bogda Piedmont of Eastern Tianshan Mountains: Based on 3D Structural Modeling and Geomorphic Analysis. Earth Science, 47(2): 418-436. doi: 10.3799/dqkx.2021.097
Citation: Chen Yingying, Li Yiquan, Wei Dongtao, Mao Yuqiong, Wang Xianyan, 2022. Quantitative Relationship between Tectonic Deformation and Topography in Bogda Piedmont of Eastern Tianshan Mountains: Based on 3D Structural Modeling and Geomorphic Analysis. Earth Science, 47(2): 418-436. doi: 10.3799/dqkx.2021.097
shu

Quantitative Relationship between Tectonic Deformation and Topography in Bogda Piedmont of Eastern Tianshan Mountains: Based on 3D Structural Modeling and Geomorphic Analysis

doi: 10.3799/dqkx.2021.097
  • 1.

    School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, China

  • 2.

    Xi'an Center of Geological Survey, China Geological Survey, Xi'an, 710054, China

  • Received Date: 2021-05-23
  • Publish Date: 2022-02-25
    Abstract
  • The specific neotectonic activities, spatial variations of erosion rates in Tianshan Mountains are led by the far-field effect of the India-Asia collision and variable precipitations. It is an ideal place to discuss the interaction of tectonic, surface processes and climatic change. The relationship of the amount of fault slip and topographic relief in this area might provide clues for understanding the interaction between tectonic and climate, and resulted topography. In this study, the subsurface three-dimensional structural geometry model of a fault-related anticline (Gumudi) at the western fault zone (Fukang) at the eastern Tianshan Mountains was constructed by the interpretation of the 3D seismic reflection data in depth. It shows that the dip of the fault is about 40°-50°, and fault-propagation folds developed. The tectonic deformation of this fault originated from the central zone and gradually propagated to the east and west ends. The amounts of the fault slip and the topographic relief at different areas were calculated from the subsurface three-dimensional tectonic structural geometry. The results show that the topographic relief (△H) is linearly related to the amount of fault slip (Sl). The maximum denudation, the maximum shortening, and the denudation rate are deduced to be as about 5.05 km, 9.20 km, and 0.38-0.60 mm/a, respectively, in the central area of the Fukang fault zone, which is based on the linear relationship between the faultslipandthetopographic relief. In addition, it presents a similar relationship that △H was equal to 1/10 Sl at different areas in spite of quite various dip angles of faults. This indicates that the relict topography is mainly controlled by the dynamic balance of the tectonic activities and erosion of the orogenic wedge rather than the magnitudes of the fault dip in this area.

     

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