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dc.contributor.authorImhof, Matthias G.
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-12-11T16:09:38Z
dc.date.available2012-12-11T16:09:38Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/1721.1/75376
dc.description.abstractWell-logs show that heterogeneities occur at many different spatial scales. In this paper, we want to characterize how waves are affected by these heterogeneities, and we study how reflection and transmission coefficients depend on temporal frequency and spatial scale. We use wavelet transformations to filter certain spatial scales from the velocity logs. The scale-filtered logs serve as input for a numerical layer-stack model to calculate reflection and transmission coefficients as functions of frequency and scale. We find that transmission coefficients are largely independent of frequency or scale. They depend mostly on average slowness. Contrarily, reflection coefficients are extremely sensitive to the perturbations of the slownesses, even at low frequencies.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;1998-03
dc.titleScale And Frequency Dependence Of Reflection And Transmission Coefficientsen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorImhof, Matthias G.
dspace.orderedauthorsImhof, Matthias G.en_US


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