Processing of seismic precursor data

Physics

Scientific paper

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Scientific paper

The correct interpretation of precursor signals associated with the seismic phases PP, PKIKP, PKPPKP and others has an important bearing on the delineation of structure within the Earth's interior. Of particular importance in this respect is the problem of identifying and analysing seismic waves which have resulted by scattering in regions of small-scale random irregularities in density and elastic parameters especially in the uppermost and lowermost parts of the mantle. Many previous studies of precursors have implicitly discriminated against the possibility of scattering-type interpretations in their data selection and analysis methods. Experiments capable of discriminating between scattering and other possible interpretations of precursor signals must necessarily involve array data sampled densely and simultaneously in space for estimating slowness and azimuths of the various arrivals.

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