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dc.contributor.authorAl Muhaidib, Abdulaziz
dc.contributor.authorFehler, Michael
dc.contributor.authorToksoz, M. Nafi
dc.contributor.authorZhang, Yang
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratory
dc.date.accessioned2014-09-29T14:44:45Z
dc.date.available2014-09-29T14:44:45Z
dc.date.issued2011
dc.identifier.urihttp://hdl.handle.net/1721.1/90428
dc.description.abstractSurface topography and the weathered zone (i.e., heterogeneity near the earth’s surface) have great effects on elastic wave propagation. Both surface waves and body waves are contaminated by scattering and conversion by the irregular surface topographic features. In this paper, we present a 2D numerical solver for the elastic wave equation that combines a 4th-order ADER scheme (Arbitrary high-order accuracy using DERivatives) with the characteristic variable method at the free surface boundary. The method is based on the velocity-stress formulation. We demonstrate the method by calculating synthetic seismograms for simple features.en_US
dc.language.isoen_USen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;2011-16
dc.subjectModeling
dc.subjectScattering
dc.titleFinite Difference Elastic Wave Modeling Including Surface Topographyen_US
dc.typeTechnical Reporten_US


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