Dilatancy, pore fluids, and premonitory variations of ts/tp travel times
1972 ◽
Vol 62
(5)
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pp. 1217-1222
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Keyword(s):
Abstract Nerseov et al. (1969) found that the travel-time ratio of shear and compressional waves, ξ = ts/tp varies prior to the occurrence of earthquakes in the Garm region, USSR. Laboratory results indicate that the decrease of ξ can result from dilatancy of rocks around the focal zone. The subsequent increase of ξ, 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.
1973 ◽
Vol 63
(3)
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pp. 1157-1161
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Keyword(s):
2021 ◽
pp. 036119812110184
2015 ◽
Vol 2015
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pp. 1-9
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Keyword(s):
1977 ◽
Vol 67
(1)
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pp. 33-42
Keyword(s):
1952 ◽
Vol 42
(4)
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pp. 313-314
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2000 ◽
Vol 1717
(1)
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pp. 120-129
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