WANG PEIDEup, FRANCIS T. Wuup2, CHEN YUNTAIup. 1990: DISTRIBUTION IN TIME AND SPACE OF TWO SUCCESSIVE EARTHQUAKE RUPTURES. Acta Seismologica Sinica, 12(1): 38-42.
Citation: WANG PEIDEup, FRANCIS T. Wuup2, CHEN YUNTAIup. 1990: DISTRIBUTION IN TIME AND SPACE OF TWO SUCCESSIVE EARTHQUAKE RUPTURES. Acta Seismologica Sinica, 12(1): 38-42.

DISTRIBUTION IN TIME AND SPACE OF TWO SUCCESSIVE EARTHQUAKE RUPTURES

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  • Published Date: September 01, 2011
  • Three near-field double-shock records of the Luanxian earthquake swarm,Heibe province.,of September to October 1981,are used to evaluate the time interval and separation in space between the successive two ruptures. The distances between those events with magnitude 2 are about 100 meters,and the velocity of rupture propagation is also estmated.
  • [1] Das. S., and Aki, K., 1977. Fault planes with banriers: A versatile earthquake modd. J. Geophys Res,82. 5658——5670.

    [2] Aki, K., 1979. Characterization barriers on an darthquake fault. J. Grophys. Res,84, Bu11,6190——6148.

    [3] Kanamori, H., 1981, The nature of scismicity patterns before large earthquakes, In: Smpson, D. W.,and Richards, Y. G. (Eds.), Earthguake Predntion—An International Review, 1——19. American Geophysical Union.

    [4] 吴人铭、王培德、陈运泰,1989.用SH波P波振幅比确定震源参数.地震学报,11,275——281,

    [5] Aki, K., 1983. Strong——motion seismology, Earzhdaake: Observation, Theory and Interpretation, 223——247, North——Holland Yubhshing Company.

    [6] Masakuzu, O,1986. Fault length of small——sized earthquake as estimated from the pulse width for initial P wave. J. Phys. Earth, 34, 397——406.

    [1] Das. S., and Aki, K., 1977. Fault planes with banriers: A versatile earthquake modd. J. Geophys Res,82. 5658——5670.

    [2] Aki, K., 1979. Characterization barriers on an darthquake fault. J. Grophys. Res,84, Bu11,6190——6148.

    [3] Kanamori, H., 1981, The nature of scismicity patterns before large earthquakes, In: Smpson, D. W.,and Richards, Y. G. (Eds.), Earthguake Predntion—An International Review, 1——19. American Geophysical Union.

    [4] 吴人铭、王培德、陈运泰,1989.用SH波P波振幅比确定震源参数.地震学报,11,275——281,

    [5] Aki, K., 1983. Strong——motion seismology, Earzhdaake: Observation, Theory and Interpretation, 223——247, North——Holland Yubhshing Company.

    [6] Masakuzu, O,1986. Fault length of small——sized earthquake as estimated from the pulse width for initial P wave. J. Phys. Earth, 34, 397——406.
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