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Both earthquake scenarios revealed significant ground motion amplification up to 15 in terms of spectral acceleration. In this paper, the authors conduct a multi-hole wave field simulation and characteristic analysis of a boulder model based on the 3 – D elastic wave staggered-grid finite difference theory, and also a 2- D imaging analysis based on first arrival travel time. A database was created to study 3 D landslide geometries. We constructed seismic convolution models with the acoustic impedance profiles and a source wavelet which is extracted from the seismic data, adjusting the seismic models to observed seismic traces with inversion method. We found a porosity anomaly zone with alteration of high and low porosities seaward of the trough axis. This method has proven to be the most efficient and is the core of his program.❿
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