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dc.contributor.authorMikhailov, Oleg V.
dc.contributor.authorBurns, Daniel R.
dc.contributor.authorToksoz, M. Nafi
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-12-11T16:43:57Z
dc.date.available2012-12-11T16:43:57Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/1721.1/75385
dc.description.abstractA Stoneley wave propagating in a borehole generates pore fluid flow within the permeable zones intersected by the borehole. In turn, the fluid flow induces a streaming electrical potential. This electrical potential induced by the Stoneley wave can be -measured in the field at frequencies from 100Hz to 4000Hz. Measurements of this Stoneley-wave-induced electrical potential can be used to detect fractures and permeable zones. The amplitude-versus-frequency dependence of this electroseismic phenomenon provides a new way to test theories of the acoustics and the electrokinetics of porous media against field measurements in real :oeks.en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Borehole Acoustics and Logging Consortiumen_US
dc.description.sponsorshipMassachusetts Institute of Technology. Earth Resources Laboratory. Reservoir Delineation Consortiumen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;1998-09
dc.titleElectroseismic Logging For The Detection And Characterization Of Permeable Zones: Field Measurements And Theoryen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorMikhailov, Oleg V.
dc.contributor.mitauthorBurns, Daniel R.
dc.contributor.mitauthorToksoz, M. Nafi
dspace.orderedauthorsMikhailov, Oleg V.; Burns, Daniel R.; Toksoz, M. Nafien_US


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