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首页> 外文期刊>Geophysical Research Letters >Regional wavefield reconstruction for teleseismic P-waves and surface waves - art. no. 1544
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Regional wavefield reconstruction for teleseismic P-waves and surface waves - art. no. 1544

机译:远震P波和面波的区域波场重建-艺术。没有。 1544

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1] With the recent availability of dense seismological array data there is the opportunity to reconstruct 2D wavefields of propagating seismic energy. Such a reconstruction allows seismic data to be viewed as wavefields rather than as single station traces. Reconstruction of such wavefields within an array will improve our understanding of complex wave propagation effects and, hence, the underlying Earth structure beneath the array. We propose an algorithm applicable for teleseismic waves that is based on wavefield expansion by cubic B-splines. Application to the high-density array in Southern California shows that we can identify basin resonances and wavefront shifts; such wavefield shifts could be caused by local structure or travel path structure, as waves pass through major structural contrasts. [References: 12
机译:1]随着密集地震学阵列数据的最新可用性,有机会重建传播地震能量的二维波场。这样的重构允许将地震数据视为波场而不是单站迹线。在阵列内重建此类波场将改善我们对复杂波传播效应的理解,从而改善对阵列下方的潜在地球结构的了解。我们提出了一种适用于远震波的算法,该算法基于三次B样条的波场扩展。在南加州的高密度阵列中的应用表明,我们可以识别盆地共振和波前位移。当波通过主要的结构对比时,这种波场偏移可能是由局部结构或行进路径结构引起的。 [参考:12

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