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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2017  >  39(6): 819-824
Liu Zhongrong, Li Xiangquan. Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819
Citation: Liu Zhongrong, Li Xiangquan. Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819
shu

Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau

doi: 10.11781/sysydz201706819
  • 1.

    SINOPEC Exploration Company, Chengdu, Sichuan 610041, China

  • 2. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education(China University of Geosciences), Wuhan, Hubei 430074, China

  • 3. College of Marine Science and Technology, China University of Geosciences, Wuhan, Hubei 430074, China

  • Received Date: 2017-08-18
  • Rev Recd Date: 2017-10-20
  • Publish Date: 2017-11-28
    Abstract
  • The 2D seismic data of the Lunpola Basin showed that the late tectonic deformation of the basin could be classified into four types:tensional-torsional lateral adjustment, thrust-depression, compressive folding and compressive-torsional uplifting. Ten tectonic deformation partitions were identified:thrust, compressive folding and compressive-torsional uplifting belts in the south and north, respectively, compressive-torsional uplifting and thrust-depression belts in the west, tensional-torsional lateral adjustment belt in the center, and thrust-depression, compressive folding belts in the east. Tensional and compressive structural styles coexist in the Lunpola Basin, and were controlled by the regional sinistral strike-slip compressive stress, which are the most unique characteristics of late tectonic deformation of the basin.

     

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