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SYSTEMS, SCIENCE AND SOFTWARE, P.O. BOX 1620 LA JOLLA, CALIFORNIA 92037
NATIONAL CENTER FOR EARTHQUAKE RESEARCH U.S. GEOLOGICAL SURVEY, 345 MIDDLEFIELD ROAD MENLO PARK, CALIFORNIA 94025
Abstract
The postearthquake deformation of a geodetic network which spans the zone of rupture of the 1966 Parkfield earthquake is not pure right-lateral shear as might be expected but rather is primarily an east-west extension. This deformation is consistent with that predicted by a dilatancy model.
This article has been cited by other articles:
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I. N. GUPTA Dilatancy and premonitory variations of P, S travel times Bulletin of the Seismological Society of America, June 1, 1973; 63(3): 1157 - 1161. [Abstract] [PDF] |
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