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Observation of a distinct compressional‐mode interface wave on a single fracture
Author(s) -
Roy Sanjit,
PyrakNolte Laura J.
Publication year - 1997
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 - 10.1029/96gl03775
Subject(s) - longitudinal wave , fracture (geology) , transverse plane , displacement (psychology) , transverse wave , longitudinal mode , particle displacement , mode (computer interface) , geology , mechanics , wave propagation , physics , geotechnical engineering , optics , amplitude , wavelength , structural engineering , engineering , psychology , computer science , psychotherapist , operating system
A compressional‐mode interface wave propagating along a fracture has been observed in a fracture in limestone. This compressional‐mode interface wave co‐propagates with the bulk compressional wave, is localized to the region surrounding the fracture, and has particle motions containing both transverse and longitudinal displacements. As stress across the fracture increases, the wave energy shifts to earlier arrival times, and is accompanied by a decrease in the transverse displacement and an increase in the longitudinal displacement of the particle motion.

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