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DOI http://dx.doi.org/10.1029/95GL01323
Title Wavelet analysis of velocity dispersion of elastic interface waves propagating along a fracture
Creator/Author Pyrak-Nolte, L.J. [Univ. of Notre Dame, IN (United States)] ; Nolte, D.D. [Purdue Univ., West Lafayette, IN (United States)]
Publication Date1995 Jun 01
OSTI IdentifierOSTI ID: 150485
Other Number(s)Journal ID: GPRLAJ; ISSN 0094-8276; TRN: TRN: 95:005687-0001
Resource TypeJournal Article
Resource RelationJournal Name: Geophysical Research Letters; Journal Volume: 22; Journal Issue: 11; Other Information: PBD: 1 Jun 1995
Subject58 GEOSCIENCES; SEISMIC WAVES; FREQUENCY ANALYSIS; WAVE PROPAGATION; VELOCITY; DISPERSION RELATIONS; GEOLOGIC FAULTS
Description/AbstractA wavelet analysis is performed on seismic waveforms of elastic interface waves that propagate along a fracture. The wavelet analysis provides a direct quantitative measure of spectral content as a function of arrival time. The authors find that the spectral content of the interface wave signals is not stationary, but exhibits increasing frequency content for later arrival times, representing negative velocity dispersion. The dispersion increase from {minus}11 m/sec/MHz to {minus}116 m/sec/MHz as the stress on the fracture is increased from 3.5 kPa to 33 MPa. The negative velocity dispersion agrees with predictions from the displacement-discontinuity theory of the seismic response of fractures, and can be used to fit fracture stiffness. 16 refs., 3 figs., 1 tab.
Country of PublicationUnited States
LanguageEnglish
FormatMedium: X; Size: pp. 1329-1332
System Entry Date2008 Feb 04

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