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dc.contributor.advisorBradford H. Hager.en_US
dc.contributor.authorPeters, Teresa Baker, 1981-en_US
dc.contributor.otherMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences.en_US
dc.date.accessioned2018-03-27T14:17:14Z
dc.date.available2018-03-27T14:17:14Z
dc.date.copyright2003en_US
dc.date.issued2003en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/114317
dc.descriptionThesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2003.en_US
dc.descriptionCataloged from PDF version of thesis.en_US
dc.descriptionIncludes bibliographical references (page 22).en_US
dc.description.abstractGeologic deformation in three dimensions can be modeled using finite element analysis. In choosing the elements used to solve a model it is important to consider the accuracy of the solution and the computational intensity. The results for models using six element types and six element side lengths are compared for the accuracy of the displacements calculated by the solution and the number of nodes required, as a proxy for computational intensity. Elements that allow higher order solutions are much more accurate than elements that only allow linear interpolation of the stresses and displacements between nodes; however the number of nodes required is five times greater. Free-form meshes do not significantly improve the performance of tetrahedra for the models tested, but could be accurate enough to model curved problem geometries. Comparisons for other models, such as a thrust fault, can be made using a twodimensional simplification of the three-dimensional problem. If three-dimensional comparisons are required it is important to choose a model that has an analytical solution.en_US
dc.description.statementofresponsibilityby Teresa Baker.en_US
dc.format.extent22 pagesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsMIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectEarth, Atmospheric, and Planetary Sciences.en_US
dc.titleFinite element comparison for a geologically motivated benchmarken_US
dc.typeThesisen_US
dc.description.degreeS.B.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc1028737657en_US


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