Summary Broad-band seismic data available on the magnetic tape library at Berkeley have been used in a study comparing P, and Rayleigh waves from earthquakes, explosions and explosion afterevents, both collapse and earthquake types. Eighty-one events equidistant from Berkeley at 500-550 km provided the data for wave amplitude and spectra comparisons. Explosions exhibit characteristic low Rayleigh wave (12-s period) generation, for given P,, amplitude, relative to earthquakes as well as explosion afterevents. This discriminant, for events recorded at Berkeley, is well developed down to local magnitude M,, 4.0 or less (m; R 3.6) and shows no indication of convergence, although scatter increases, for smaller events. Rayleigh wave spectra for explosions and collapses are quite similar, the similarity continuing up to frequencies of 0.5 Hz for proximate events. However, they differ significantly from spectra of shallow earthquakes in the same source region. This implies the explosions, including those large ones with appreciable surface faulting, Love wave generation, and aftershock sequences, are sources with small time and space dimensions, relative to shallow earthquakes at the same site. Extensive fault displacements near large explosions is proposed as passive medium response to strong shaking and Love wave generation with Rayleigh wave asymmetry is suggested to occur through processes acting in the relatively small high stress explosive source region.
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