Show simple item record

dc.contributor.authorCheng, N. Y.
dc.contributor.authorCheng, C. H.
dc.contributor.authorToksoz, M. N.
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-12-03T19:14:32Z
dc.date.available2012-12-03T19:14:32Z
dc.date.issued1990
dc.identifier.urihttp://hdl.handle.net/1721.1/75161
dc.description.abstractThe in situ permeability of a formation is obtained by the inversion of Stoneley wave phase velocity and attenuation, which are evaluated by applying the Extended Prony's method to the array sonic logging data. The Maximum Likelihood inversion is used together with logarithmic parameterization of the permeabilities. Formation shear wave velocity is also inverted for. This process is tested on both synthetic and field data. Logarithmic parameterization contributes to rapid convergence of the algorithm. Permeabilities estimated from field data are in good agreement with core measurements.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;1990-07
dc.titleInversion For Permeability From Stoneley Wave Velocity And Attenuationen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorCheng, N. Y.
dc.contributor.mitauthorCheng, C. H.
dc.contributor.mitauthorToksoz, M. N.
dspace.orderedauthorsCheng, N. Y.; Cheng, C. H.; Toksoz, M. N.en_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record