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Elastic interface waves along a fracture
Author(s) -
PyrakNolte Laura J.,
Cook Neville G. W.
Publication year - 1987
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl014i011p01107
Subject(s) - rayleigh wave , discontinuity (linguistics) , geology , displacement (psychology) , seismic wave , fracture (geology) , seismology , surface wave , mechanics , geophysics , geotechnical engineering , physics , optics , mathematical analysis , mathematics , psychology , psychotherapist
Non‐welded interfaces can be treated as a displacement discontinuity characterized by elastic stiffnesses. Applying this boundary condition to a generalized Rayleigh wave, it is shown that a fast and a slow dispersive wave can propagate along the fracture, even when the seismic properties of the rock on each side are identical.

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