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Bulletin of the Seismological Society of America; October 1974; v. 64; no. 5; p. 1419-1427
© 1974 Seismological Society of America
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Time functions appropriate for deep earthquakes

L. J. BURDICK and D. V. HELMBERGER

DIVISION OF GEOLOGICAL AND PLANETARY SCIENCES CALIFORNIA INSTITUTE OF TECHNOLOGY, PASADENA, CALIFORNIA 91109

Abstract

The seismic signatures of isolated body phases from many deep-focus earthquakes were analyzed in the time domain. Most shocks were found to be multiple events when examined in detail. The time history derived from P waves for single events predict synthetic S-wave shapes that match the observations, indicating compatibility with shear dislocation theory. Several other features of source functions in the time domain have been brought to light.




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