Volume 40 Issue 10
Oct.  2015
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Article Navigation >  Earth Science  > 2015  >  40(10): 1767-1780
Li Yuhang, Cui Duxin, Hao Ming, 2015. GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau. Earth Science, 40(10): 1767-1780. doi: 10.3799/dqkx.2015.158
Citation: Li Yuhang, Cui Duxin, Hao Ming, 2015. GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau. Earth Science, 40(10): 1767-1780. doi: 10.3799/dqkx.2015.158
shu

GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau

doi: 10.3799/dqkx.2015.158
  • 1.

    Institute of Geology, CEA, Beijing 100029, China

  • 2.

    Second Crust Monitoring and Application Center, CEA, Xi'an 710054, China

  • Received Date: 2014-11-18
  • Publish Date: 2015-10-15
    Abstract
  • GPS mwasurements can provide a high accuracy of spatio-temporal images, but there aren't enough study about it. We use the spherical linear block theory constrained by geodetic observations from Global Positioning System (GPS) stations to estimate fault slip rates on the Northeastern margin of Tibet plateau and spatially variable coupling on Haiyuan fault in abroad sense. The 3D geometric block model is based on the previous researches of active block. The result provides a new constraint and reference for the geodynamics of present crustal deformation and the middle-long term strong earthquake hazard study in this area.

     

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