论文部分内容阅读
In accordance with the principle of similarity in geology and topography,the V3S0(the average shear-velocity down to a 30m depth below the surface) approximation of sites is acquired by correlation between V3S0 and slopes after calculating the maximum slope of topography using the 30-sec Chinese Mainland DEM(Digital Elevation Model) data set.Site-amplification factors are then quantified with V3S0 and applied to the ShakeMap system developed by this study to revise ground-motion amplitudes on bedrock estimated from empirical relationships.Finally,the distribution of ground motion parameters on the surface is obtained.This article also introduces the calculation process,calculation models of the ShakeMap systems and related software systems.In conclusion,certain examples indicate that the ShakeMap system is feasible in the Chinese Mainland.
In accordance with the principle of similarity in geology and topography, the V3S0 (the average shear-velocity down to a 30m depth below the surface) approximation of sites is acquired by correlation between V3S0 and slopes after calculating the maximum slope of topography using the 30 -sec Chinese Mainland DEM (Digital Elevation Model) data set. Site-amplification factors are then quantified with V3S0 and applied to the ShakeMap system developed by this study to revise ground-motion amplitudes on bedrock estimated from empirical relationships. Finaally, the distribution of ground motion parameters on the surface is obtained. This article also introduces the calculation process, calculation models of the ShakeMap systems and related software systems. In conclusion, certain examples indicate that the ShakeMap system is feasible in the Chinese Mainland.