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Finite seismic source parameters inferred from stopping phases for selected events of west bohemia 2000 swarm

机译:从西波西米亚2000群选定事件的停止阶段推断出有限震源参数

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Parameters of finite seismic source model were determined for a set of 36 selected events of the West Bohemia 2000 earthquakes swarm (Ml from 1.7 to 3.0) using stopping phases method. Two stopping phases are generated along the source border where the rupture process terminates and these phases form Hilbert transform pair, which is also the criterion for their identification. Circular and elliptical source models were considered and corresponding source parameters were calculated by inverting interpreted stopping phases delays. As generalization of circular to elliptical model was found to be statistically insignificant, only results related to the circular source including error estimates are presented. Our results are in a good agreement with previously published theoretical formula concerning source radius and magnitude and also fairly well confirm general theoretical assumption about constant stress drop. The determined stress drop ranges between 1 - 10 MPa with the typical value of 2.4 MPa.
机译:使用停止阶段方法,为西波希米亚2000年地震群(MI从1.7到3.0)中的36个选定事件的集合确定了有限震源模型的参数。沿着破裂过程终止的源边界产生两个停止阶段,这些阶段形成希尔伯特变换对,这也是识别它们的标准。考虑了圆形和椭圆形源模型,并通过反转解释的停止相位延迟来计算相应的源参数。由于发现圆形到椭圆模型的泛化在统计上不重要,因此仅显示与圆形源相关的结果,包括误差估计。我们的结果与先前发表的关于源半径和大小的理论公式非常吻合,并且还很好地证实了有关恒定应力降的一般理论假设。所确定的应力降范围为1-10 MPa,典型值为2.4 MPa。

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