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    Volume 39 Issue 9
    Sep.  2014
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    Article Contents
    Deng Mingli, Sun Heping, Xu Jianqiao, Zhu Yiqing, 2014. Theoretical Simulation of Co-Seismic and Post-Seismic Deformations and Gravity Changes of Lushan Earthquake. Earth Science, 39(9): 1373-1382. doi: 10.3799/dqkx.2014.120
    Citation: Deng Mingli, Sun Heping, Xu Jianqiao, Zhu Yiqing, 2014. Theoretical Simulation of Co-Seismic and Post-Seismic Deformations and Gravity Changes of Lushan Earthquake. Earth Science, 39(9): 1373-1382. doi: 10.3799/dqkx.2014.120

    Theoretical Simulation of Co-Seismic and Post-Seismic Deformations and Gravity Changes of Lushan Earthquake

    doi: 10.3799/dqkx.2014.120
    • Received Date: 2014-01-05
    • Publish Date: 2014-09-01
    • This paper aims at studying the seismogenic process and long-term tectonic process of the source area and explain the post-seismic deformation and gravity data in Lushan earthquake. Based on the layered half-space model, we calculate the co- and post-seismic surface deformations and gravity changes and their time series gained by the GPS and gravity stations, considering regional rheological coefficients, and using the numerical simulation method. It is found that the surface co-seismic deformation shows seismogenic fault is of obvious thrusting characteristics The range of influence of viscoelastic relaxation is significantly enlarged than that of the co-seismic, but changes gradually reduce with the increase of viscousity coefficients. The time-variable curves of the stations show that post-seismic deformation and gravity changes are significant in 50 years after the earthquake, become gentle after 100 years and tend to be stable. The post-seismic observations of the GPS stations are convinced to consider the effect of viscoelastic relaxation except for the MEIG and the MYAN.

       

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