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Bulletin of the Seismological Society of America; October 1972; v. 62; no. 5; p. 1217-1222
© 1972 Seismological Society of America
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Dilatancy, pore fluids, and premonitory variations of ts/tp travel times

AMOS NUR

DEPARTMENT OF GEOPHYSICS STANFORD UNIVERSITY, STANFORD, CALIFORNIA 94305

Abstract

Nerseov et al. (1969) found that the travel-time ratio of shear and compressional waves, {xi} = ts/tp varies prior to the occurrence of earthquakes in the Garm region, USSR. Laboratory results indicate that the decrease of {xi} can result from dilatancy of rocks around the focal zone. The subsequent increase of {xi}, which terminates with an earthquake, can be caused by the flow of ground water into the dilated zone. The increasing pore pressure weakens the rock and leads to the observed failure.




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