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dc.contributor.authorBriggs, Victoria
dc.contributor.authorRao, Rama V. N.
dc.contributor.authorBurns, Daniel R.
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2011-12-21T21:38:56Z
dc.date.available2011-12-21T21:38:56Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/1721.1/67859
dc.description.abstractA method to jointly invert for azimuthal angle and dispersion relations from cross-dipole data is presented. Dispersion curves from the joint inversion are compared to both Prony’s method and a simple back propagation schema and an agrrement is found. The azimuthal angle estimate is shown to differ from a frequency domain rotaion that takes no account of dispersion within the waveforms indicating the importance of joint inversion.en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.description.sponsorshipMassachusetts Institute of Technology. Borehole Acoustics and Logging Consortiumen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;2003-03
dc.titleSimultaneous Inversion of cross-dipole acoustic waveforms in anisotropic media for azimuthal angle and dispersion of fast and slow shear wavesen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorBriggs, Victoria
dc.contributor.mitauthorRao, Rama V. N.
dc.contributor.mitauthorBurns, Daniel R.
dspace.orderedauthorsBriggs, Victoria; Rao, Rama V. N.; Burns, Daniel R.en_US


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