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dc.contributor.authorToksoz, M. Nafi
dc.contributor.authorGuler, Fatih
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-11-29T19:41:08Z
dc.date.available2012-11-29T19:41:08Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/1721.1/75102
dc.description.abstractThe effects of fractures on full waveform acoustic logs are studied on the basis of field observations, available theoretical models, and a series of ultrasonic laboratory experiments. Results from diffusion models applicable to fine microfractures and finite difference models of isolated fractures are reviewed. Laboratory experiments are carried out with fine microfractures around the borehole in a Lucite model, and isolated single fractures in aluminum models. Cases of horizontal and inclined (45°) fractures are studied as a function of fracture aperture and frequency of Stoneley waves. A vertical fracture model is also studied. Results indicate that the effect of different fractures are manifested differently on P, S, pseudo-Rayleigh, and Stoneley waves. Micro-fractures surrounding a borehole attenuate Stoneley waves most strongly. Vertical fractures attenuate Stoneley waves more strongly than other phases in the wave train. Horizontal and inclined fractures have a greater effect on P and S waves than on Stoneley waves.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;1988-07
dc.titleFracture Detection And Characterizationen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorToksoz, M. Nafi
dc.contributor.mitauthorGuler, Fatih
dspace.orderedauthorsToksoz, M. Nafi; GuIer, Fatihen_US


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