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Li Jie, Chen Gang, Wei Wenxin, Zainula Paerhati, Wang Xiaoqiang, Liu Daiqin, Li Guirong, Fang Wei, Chen Shujiang, Sun Xiaoxu. 2016: Characteristics of present-day tectonics movement of typical faults in northern Tianshan mountain deduced from GPS observation. Acta Seismologica Sinica, 38(5): 751-760.
Citation: Li Jie, Chen Gang, Wei Wenxin, Zainula Paerhati, Wang Xiaoqiang, Liu Daiqin, Li Guirong, Fang Wei, Chen Shujiang, Sun Xiaoxu. 2016: Characteristics of present-day tectonics movement of typical faults in northern Tianshan mountain deduced from GPS observation. Acta Seismologica Sinica, 38(5): 751-760.
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Characteristics of present-day tectonics movement of typical faults in northern Tianshan mountain deduced from GPS observation

  • 1.

    Earthquake Administration of Xinjiang Uygur Autonomous Region, Vrümqi 830011, China

  • 2.

    Faculty of Information Engineering, China University of Geosciences, Wuhan 430074, China

  • 3.

    Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China

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  • Received Date: November 21, 2015
  • Revised Date: April 11, 2016
  • Published Date: August 31, 2016
    Graphical Abstract
    • Abstract
  • Based on the latest multiple-epoch observation data of the GPS sites in northern Tianshan mountain, this paper obtained the present-day GPS sites velocity fields of the crustal movement in northern Tianshan mountain, using GAMIT/GLOBK processing software. Based on an elastic half-space dislocation model, slip rate of the two typical faults are constrained by GPS-derived crustal deformation displacement velocities of the northern Tianshan mountain. One fault is Boluokenu-Aqikekuduke (BoA for short) fault, and the other is southern margin fault of Junggar basin. The GPS results show that the slip rate difference between east and west segment of right-lateral strike-slip BoA fault is not obvious. The fault exhibted creeping slightly with micro-seismicity within 1—2 mm/a since MS7.2 south Wusu earthquake occurred on March 10, 1944. The present-day slip rate in southern margin fault of Junggar basin almost keeps (5.6±1.0) mm/a.
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    • References (64)
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