1887

Abstract

Strain amplitude cycling experiments were conducted on dry samples of sedimentary rocks to investigate the<br>strain amplitude dependence of P- and S- wave velocities in the range of ε~1,5*10-7 to 9*10-7. Wave<br>velocities increase with amplitude strain. Wave velocities obtained from experiments show a remain<br>hysteresis.

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/content/papers/10.3997/2214-4609-pdb.38.F251
2003-09-01
2020-03-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.38.F251
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