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Bulletin of the Seismological Society of America; October 1973; v. 63; no. 5; p. 1611-1636
© 1973 Seismological Society of America
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Extension and interpretation of the Cagniard-Pekeris method for dislocation sources

ARI BEN-MENAHEM and MOSHE VERED

ADOLPHO BLOCH GEOPHYSICAL OBSERVATORY DEPARTMENT OF APPLIED MATHEMATICS THE WEIZMANN INSTITUTE OF SCIENCE, REHOVOT, Israel

Abstract

A variant of the Cagniard-Pekeris inversion technique is extended to nonsymmetric earthquake sources of arbitrary multipolar order with a particular emphasis on shear dislocations. In the present work, we concentrate on the infrastructure of the time-domain displacement field in the presence of a single interface. A series of transformations in the complex plane together with a novel decomposition of the total field into three fundamental constituents enables us to separate the real-time contributions due to head waves, geometrical waves and the so-called non-least-time arrivals.




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