dc.creatorAmazonas, D
dc.creatorAleixo, R
dc.creatorMelo, G
dc.creatorSchleicher, J
dc.creatorNovais, A
dc.creatorCosta, JC
dc.date2010
dc.dateSEP-OCT
dc.date2014-07-30T14:33:02Z
dc.date2015-11-26T18:06:28Z
dc.date2014-07-30T14:33:02Z
dc.date2015-11-26T18:06:28Z
dc.date.accessioned2018-03-29T00:48:40Z
dc.date.available2018-03-29T00:48:40Z
dc.identifierGeophysics. Soc Exploration Geophysicists, v. 75, n. 5, n. S175, n. S186, 2010.
dc.identifier0016-8033
dc.identifierWOS:000284254400027
dc.identifier10.1190/1.3481469
dc.identifierhttp://www.repositorio.unicamp.br/jspui/handle/REPOSIP/59976
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/59976
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1293363
dc.descriptionCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionIn heterogeneous media, standard one-way wave equations describe only the kinematic part of one-way wave propagation correctly. For a correct description of amplitudes, the one-way wave equations must be modified. In media with vertical velocity variations only, the resulting true-amplitude one-way wave equations can be solved analytically. In media with lateral velocity variations, these equations are much harder to solve and require sophisticated numerical techniques. We present an approach to circumvent these problems by implementing, approximate solutions based on the one-dimensional analytic amplitude modifications. We use these approximations to show how to modify conventional migration methods such as split-step and Fourier finite-difference migrations in such a way that they more accurately handle migration amplitudes. Simple synthetic data examples in media with a constant vertical gradient demonstrate that the correction achieves the recovery of true migration amplitudes. Applications to the SEG/EAGE salt model and the Marmousi data show that the technique improves amplitude recovery in the migrated images in more realistic situations.
dc.description75
dc.description5
dc.descriptionS175
dc.descriptionS186
dc.descriptionCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionPetrobras
dc.descriptionWave Inversion Technology (WIT) Consortium
dc.descriptionCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionFAPESP [proc. 06/04410-5]
dc.languageen
dc.publisherSoc Exploration Geophysicists
dc.publisherTulsa
dc.publisherEUA
dc.relationGeophysics
dc.relationGeophysics
dc.rightsaberto
dc.sourceWeb of Science
dc.subjectImage Gathers
dc.subjectApproximations
dc.subjectPropagation
dc.titleIncluding lateral velocity variations into true-amplitude common-shot wave-equation migration
dc.typeArtículos de revistas


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