Ray-Tracing Method
Ray-Tracing Method :
A Computational method of calculating ground-shaking estimates that assumes that the ground motion is composed of multiple arrivals of seismic rays and related energy bundles (Gauss beams) that leave the source and are reflected or refracted at velocity boundaries according to Snell's Law. The amplitudes of reflected and refracted waves at each boundary are recalculated according to the Law of Conservation of Energy
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