由地震图上的终止相研究1976年松潘续发性大震的震源破裂过程
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STUDY ON THE SOURCE RUPTURE PROCESS OF THE 1976 SONGPAN GREAT EARTHQUAKES USING THE STOPPING PHASE
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    摘要:

    利用WWSSN长周期远场P波的初相、破出相和终止相研究了1976年8月16日、22日和23日松潘三次大震的震源断层面破裂错动传播的全过程,判定了发震断层面和确定了它们的震源动力学参数。由较弱的P波初相求得三次大震的始破裂区长度分别为8、5和6 km。它们均为双侧破裂,震源体的破裂长度分别为73、43和52km。由于震源区存在重叠现象,因此,总的震源尺度仅为90 km。由破出相确定8月16日松潘大震的震源深度为9 km。此外,研究还发现,显著的终止相和较大的破裂速度与震源端部存在调整单元有关。

    Abstract:

    Using the initial phase, breakout phase and stopping phase of long period P-wave records of WWSSN, we have studied the source rupture process of the 1976 Songpan great earthquakes (Aug. 16, M=7.2; Aug. 22,M=6.7; Aug. 23, M=7.2), and got the dynamic parameters of sources of the three great earthquakes. The length of initial rupture area for the three great earthquakes is 8.5 and 6km respectively, calculated by the weaker initial, phase of P-wave. All of the three great earthquakes is two-side rupture, the rupture length of source body is 73, 34 and 54 km respectively.
    The result shows that in the source regions, the three great earthquakes exist a part of superposition phenomena, so total source dimension is only 90 km; and the source depth is 9km determined by the breakout phase of the Songpan great earthquake of Aug. 16. It is also found that the obvious stopping phase and quicker rupture speed of source fault are related to the adjustment element located at the ends of source region.

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秦保燕,姚兰予,汪进,李亚荣.由地震图上的终止相研究1976年松潘续发性大震的震源破裂过程[J].地震工程学报,1990,12(2):1-15. Qin Baoyan, Yao Lanyu, Wang Jin, Li Yarong. STUDY ON THE SOURCE RUPTURE PROCESS OF THE 1976 SONGPAN GREAT EARTHQUAKES USING THE STOPPING PHASE[J]. China Earthquake Engineering Journal,1990,12(2):1-15.

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  • 收稿日期:1989-01-28
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  • 在线发布日期: 2017-07-04