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dc.contributor.advisorN. Nafi Toksöz.en_US
dc.contributor.authorGrandi Karam, Samantha, 1973-en_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.en_US
dc.date.accessioned2006-03-24T18:22:17Z
dc.date.available2006-03-24T18:22:17Z
dc.date.copyright2003en_US
dc.date.issued2003en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/30130
dc.descriptionThesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2003.en_US
dc.descriptionIncludes bibliographical references (leaves 145-150).en_US
dc.description.abstractIn this thesis we analyze the effects of borehole irregularities on well logs and develop methods to obtain reliable formation properties from such logs. Data from a well in eastern Venezuela are analysed. Borehole irregularities in this well consist mainly of borehole enlargements perpendicular to the borehole axis due to rock failure under high horizontal stresses. They are observed in three forms: as small scale irregularities of the borehole wall, as-near elliptical shapes oriented along the minimum in situ stress direction, and as an increase of borehole diameter at all azimuths due to large scale failure. Breakout data suggest that maximum stress is oriented NNW-SSE. The suite of logs analyzed include lithology, density, dipmeter and full waveform acoustic logs. The standard log processing and interpretation methods fail because of the effects of irregularities. The analysis of the density log indicates that standard corrections are not enough when diameter is severly elongated. Similarly, acoustic logs processed commercially give unreasonable formation velocities. Guided by theoretical models we evaluate the effects of irregularities on different wave types recorded by full waveforms acoustic logs, i.e refracted P and S, pseudo Rayleigh, Stoneley, flexural etc. We obtain P and S wave velocities from the least affected waves. The density profile is derived from P wave data (Vp-[rho] correlation), with the aid of lithology logs. From the above parameters we obtain the dynamic elastic moduli and then, through known empirical relationships, the static quantities. These values will be used in the next phase of this study as input to finite element models to determine the magnitude of the in situ stress that caused the borehole failures.en_US
dc.description.statementofresponsibilityby Samantha Grandi Karam.en_US
dc.format.extent150 leavesen_US
dc.format.extent5098661 bytes
dc.format.extent5098470 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypeapplication/pdf
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582
dc.subjectEarth, Atmospheric, and Planetary Sciences.en_US
dc.titleEffects of borehole stability on well log dataen_US
dc.typeThesisen_US
dc.description.degreeS.M.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc55878740en_US


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