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Bulletin of the Seismological Society of America; October 1969; v. 59; no. 5; p. 1823-1841
© 1969 Seismological Society of America
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Aftershocks of the Dasht-e Bayaz, Iran, earthquake of August, 1968

STUART CRAMPIN

INSTITUTE OF GEOLOGICAL SCIENCES, GEOPHYSICAL LABORATORIES,, EDINBURGH

Abstract

Aftershocks of the Dasht-e Bayaz earthquake were recorded in the epicentral area with high-gain, high-frequency equipment. This study shows the general characteristics of the aftershock series. The foci are clustered near the ends of the 80 km surface faulting, at 25 km depth. In this earthquake sequence, the secondary series are not distinct in space or mechanism from the primary series, and microevents have the same strain release characteristics as the larger aftershocks.




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