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Estimation of finite seismic source parameters for selected events of the West Bohemia year 2008 seismic swarm

机译:西波西米亚2008年地震群特定事件的有限震源参数估计

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Finite seismic source parameters were determined for a set of 91 selected events of the West Bohemia year 2008 earthquake swarm (M (L) from 0.6 to 3.7) using the stopping phases method. According to the theory, two stopping phases are generated along the source border where the rupture process terminates. These two phases form a Hilbert transform pair; it is also a criterion for their identification. Circular and elliptical source models were considered and their parameters were recovered using the differences in arrival times between the identified stopping phases. Generalization of the circular to elliptical model was found to be statistically significant only for a minority of the events; consequently, only circular source models were investigated in detail. Individual source parameter errors were estimated with the use of the jackknife method. Our results are in good agreement with a previously published theoretical formula relating source radius and magnitude and also with the relation derived in the year 2000 swarm. Our results also confirm rather well the general theoretical assumption about the constant stress drop (with median value of 2.4 MPa and with the majority of values ranging from 1 to 10 MPa).
机译:使用停止阶段方法,为2008年西波西米亚地震群的91个选定事件(M(L)从0.6到3.7)确定了有限的震源参数。根据该理论,沿着破裂过程终止的源边界产生了两个停止阶段。这两个阶段构成一个希尔伯特变换对。这也是对其进行识别的标准。考虑了圆形和椭圆形源模型,并使用确定的停止阶段之间到达时间的差异来恢复其参数。发现圆形到椭圆模型的泛化仅对少数事件具有统计学意义;因此,仅详细研究了循环源模型。使用折刀法估计了各个源参数误差。我们的结果与先前发表的有关源半径和大小的理论公式以及2000年群推导的关系非常吻合。我们的结果也很好地证实了有关恒定应力下降的一般理论假设(中值为2.4 MPa,大多数值为1到10 MPa)。

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