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Advancement in Source Estimation Techniques Using Broadband Regional Seismograms

机译:利用宽带区域地震图进行震源估算技术的进展

摘要

One important constraint on source retrieval from regional seismograms comes from the amplitude difference between various phases (such as Pnl/surface wave, SV/SH). Because the misfit errors used in some waveform inversions are normalized by the data and synthetics, the amplitude information in the data has not been fully utilized. In this article, we modify the "cut and paste" source estimation technique (Zhao and Helmberger, 1994) by removing this type of normalization. It is shown that the modified method increases the stability and resolution of inversion. When multiple stations at different distance ranges are used, a distance scaling factor is introduced to compensate for the amplitude decay with distance. By applying the technique to the TERRAscope data, we have determined source mechanisms and depths of 335 southern Californian events with M_L ≧ 3.5. The amplitude decaysudwith distance are r^(1.13) for Pnl, r^(0.55) for Love waves, and r^(0.74) for Rayleigh waves. In contrast to generally shallow source depths reported by the southern California short period network, the depth distribution from waveform inversion shows a strong peak around 12 km with few earthquakes occurring above 5 km and below 20 km.
机译:从区域地震图中获取震源的一个重要限制来自于各个相位之间的振幅差异(例如Pnl /地波,SV / SH)。由于在某些波形反演中使用的失配误差已通过数据和合成进行归一化,因此数据中的幅度信息尚未得到充分利用。在本文中,我们通过删除此类归一化方法来修改“剪切并粘贴”源估计技术(Zhao和Helmberger,1994)。结果表明,改进后的方法提高了反演的稳定性和分辨率。当使用不同距离范围的多个站时,引入距离比例因子以补偿随距离的幅度衰减。通过将该技术应用于TERRAscope数据,我们已经确定了M_L≥3.5的335个南加州事件的源机制和深度。对于Pnl,幅度衰减随距离为r ^(1.13),对于Love波为r ^(0.55),对于瑞利波为r ^(0.74)。与南加州短周期网络报道的通常较浅的震源深度相比,来自波形反演的深度分布在12 km附近显示一个强峰值,在5 km以上和20 km以下发生的地震很少。

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