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Identification and Extraction of Surface Waves from Three-Component Seismograms Based on the Normalized Inner Product

机译:基于归一化内积的三分量地震波面波识别与提取

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Identification of different wave types in a seismogram is an important step for the understanding of wave propagation phenomena. Because in most seismograms, different types of waves with different frequencies may appear simultaneously, separation of waves is more effectively achieved when a time-frequency analysis is performed. In this work, we propose a new time-frequency analysis procedure to identify and extract Rayleigh and Love waves from three-component seismograms. Exploiting the advantage of the absolute phase preservation by the Stockwell transform, we construct time-frequency filters to extract waves based on the normalized inner product (NIP). Because the NIP is the time-frequency counterpart of the correlation, Rayleigh and Love waves can be identified depending on the NIP between the Stockwell transforms of the horizontal and vertical displacement components. The novelty and advantage of the proposed procedure is that it does not require specifying a priori the direction of propagation of the surface waves, but instead such direction is determined. Furthermore, it is shown that the NIP is a more stable parameter in the time-frequency domain when compared to the instantaneous reciprocal ellipticity, and thus it avoids smoothing (and with it, altering) the data. The procedure has been successfully tested with real signals, specifically to extract Rayleigh and Love waves from seismograms of one aftershock of the 1999 Chi-Chi earthquake. With the proposed procedure, we found different directions of propagation for retrograde and prograde Rayleigh waves, which might suggest that they are generated by different mechanisms.
机译:识别地震图中的不同波类型是理解波传播现象的重要步骤。因为在大多数地震图中,具有不同频率的不同类型的波可能会同时出现,所以在进行时频分析时,可以更有效地实现波的分离。在这项工作中,我们提出了一种新的时频分析程序,以从三分量地震图中识别和提取瑞利波和洛夫波。利用Stockwell变换保留绝对相位的优势,我们构造了时频滤波器以基于归一化内积(NIP)提取波。因为NIP是相关的时频对应物,所以可以根据水平位移分量和垂直位移分量的Stockwell变换之间的NIP来识别瑞利波和洛夫波。所提出的程序的新颖性和优点在于,它不需要先验地指定表面波的传播方向,而是确定了该方向。此外,还表明,与瞬时倒数椭圆率相比,NIP在时频域中是一个更稳定的参数,因此避免了平滑数据(并随之改变)。该程序已用真实信号成功进行了测试,特别是从1999年集集地震的一次余震的地震图中提取瑞利波和洛夫波。通过提出的程序,我们发现了逆行和前进瑞利波的传播方向不同,这可能表明它们是由不同的机制产生的。

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