Characterization of Ground Motion in Regions of South Africa at Rock Sites (original) (raw)

AGU Fall Meeting Abstracts, 2008

Abstract

The objective of this evaluation is to determine the crustal amplification function of the seismic signal for different regions in South Africa. In order to model crustal amplification, models of the S-wave velocity and the shear quality factor Q are determined. All currently run seismic hazard assessment projects in South Africa are utilizing the attenuation equations mostly from central and

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