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dc.contributor.authorJinzhong, Zhang
dc.contributor.authorCheng, C. H.
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-11-27T20:36:52Z
dc.date.available2012-11-27T20:36:52Z
dc.date.issued1985
dc.identifier.urihttp://hdl.handle.net/1721.1/75064
dc.description.abstractA numerical investigation of asymmetric modes of elastic wave propagation in a fluid-filled borehole is treated in this paper. The dispersion curves of guided waves (called flexural waves) and synthetic microseismograms are presented. The guided waves are found to be highly dispersive, with the phase velocities decreasing from the formation shear wave velocities in both hard and soft formations. They have much lower cut-off frequencies than the pseudo-Rayleigh waves in axisymmetric modes of propagation. We found that under conditions of low frequency (2-3 kHz) and long source-receiver separation (3-4 m), the flexural wave is the prominent arrival in a microseismogram generated with an asymmetric source, traveling with a phase velocity equal to the formation shear wave velocity, while the compressional wave arrival before that is generally suppressed. The results of this study may be meaningful for designing a shear wave logging tool.en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Full Waveform Acoustic Logging Consortiumen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;1985-04
dc.titleAsymmetric Modes of Elastic Wave Propagation in a Fluid-Filled Boreholeen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorJinzhong, Zhang
dc.contributor.mitauthorCheng, C. H.
dspace.orderedauthorsJinzhong, Zhang; Cheng, C. H.en_US


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