首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Rapid rupture directivity determination of moderate dip-slip earthquakes with teleseismic body waves assuming reduced finite source approximation
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Rapid rupture directivity determination of moderate dip-slip earthquakes with teleseismic body waves assuming reduced finite source approximation

机译:快速破裂方向性测定中等浸水地震与近距离射击地震的测定,假设有限源近似降低

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摘要

For an earthquake with along-dip rupture, there is opposite directivity effects on downgoing direct P wave and upgoing depth phases (pP and sP), and this can be exploited for resolving fault plane and rupture direction. We propose a method to calculate the reduced finite source synthetics for teleseismic P wave and determine the rupture directivity via waveform fitting. We verified the effectiveness of this method with forward tests and investigated its robustness against station selection, uncertainties in point source parameters, and uncertainties in source finiteness parameters. We applied this method to the 2011 M(w)5.8 Virginia earthquake, the 2008 M(w)6.0 Nevada earthquake, and six other dip-slip earthquakes. For most cases, we obtained rupture directivity results consistent with previous studies, but the method could fail for along-strike ruptures and very shallow earthquakes. Our method may help mitigate earthquake hazard by improving shake map with rapid rupture directivity analysis.
机译:对于沿倾斜破裂的地震,对正在进行的直接P波和上行深度阶段(PP和SP)相反的方向性影响,这可以利用用于解决断层平面和破裂方向。我们提出了一种方法来计算Telesismic P波的减少的有限源合成,并通过波形配件确定破裂方向性。我们验证了该方法的有效性,通过前进测试,并调查其对站选择的鲁棒性,点源参数中的不确定性,以及源事度的不确定性。我们将这种方法应用于2011米(W)5.8弗吉尼亚地震,2008米(W)6.0内华达地震和六个其他浸水地震。对于大多数情况而言,我们获得了与以前的研究一致的破裂派对导致结果,但该方法可能会失败沿着罢工的破裂和非常浅的地震。我们的方法可以通过快速破裂方向性分析改善抖动图来帮助减轻地震危害。

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