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dc.contributor.authorCheng, C. H.
dc.contributor.authorToksoz, M. Nafi
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-11-27T20:07:58Z
dc.date.available2012-11-27T20:07:58Z
dc.date.issued1983
dc.identifier.urihttp://hdl.handle.net/1721.1/75041
dc.description.abstractDirect determination of formation shear wave travel time is impossible in "slow" formations where the shear wave velocity is lower than the borehole fluid (mud) velocity. However, the Stoneley waves in these formations are very sensitive to changes in formation shear wave properties and can be used to indirectly determine the formation shear velocity, In addition, the P wave packet is highly dependent on the Poisson's ratio and thus can be used to estimate the shear velocity once the P wave velocity is known. These phenomena are demonstrated with both numerical and field examples.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;1983-02
dc.titleDetermination of Shear Wave Velocities in "Slow" Formationsen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorCheng, C. H.
dc.contributor.mitauthorToksoz, M. Nafi
dspace.orderedauthorsCheng, C. H.; Toksoz, M. Nafien_US


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