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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2013  >  35(3): 255-262
Zhang Yuhang, Tang Liangjie, Yun Lu, Xie Daqing, Qiu Haijun, Jiang Huashan. Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 255-262. doi: 10.11781/sysydz201303255
Citation: Zhang Yuhang, Tang Liangjie, Yun Lu, Xie Daqing, Qiu Haijun, Jiang Huashan. Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 255-262. doi: 10.11781/sysydz201303255
shu

Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin

doi: 10.11781/sysydz201303255
  • 1.

    State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China

  • 2. Basin & Reservoir Research Center, China University of Petroleum, Beijing 102249, China

  • 3. SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830011, China

  • 4. Oil and Gas Resources Strategic Research Center, Ministry of Land and Resources, Beijing 100034, China

  • Received Date: 2012-11-30
  • Rev Recd Date: 2013-03-20
  • Publish Date: 2013-05-28
    Abstract
  • Based on latest seismic interpretation data,the features of differential deformation of the Kalashayi Fault in the central Bachu Uplift were analyzed by means of fault-related fold theory and balanced section technique.The Kalashayi Fault is an active fault of multiple stages in the Bachu Uplift.It has suffered several stages of deformation,such as the early Caledonian,the episode Ⅰ of the middle Caledonian,the late Hercynian and the early Himalayan.On the plane,two faults of different scales converge like scissors from SW to NE.In profile,the Kalashayi Fault is composed of ramp-flat blind thrust fault which slips in Cambrian and high-angle basement-involved thrust fault.Gypsum-salt rocks control the multi-level deformation features of the Kalashayi Fault.The difference of pre-structure in basement leads to the segmental deformation features.Regional stress field transition results in the poly-phase deformation features.

     

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