dc.creatorVivas, Flor A.
dc.creatorPestana, Reynam da Cruz
dc.creatorUrsin, Bjorn
dc.creatorVivas, Flor A.
dc.creatorPestana, Reynam da Cruz
dc.creatorUrsin, Bjorn
dc.date.accessioned2022-10-07T18:34:38Z
dc.date.available2022-10-07T18:34:38Z
dc.date.issued2009
dc.identifier1742-2132
dc.identifierhttp://repositorio.ufba.br/ri/handle/ri/13798
dc.identifierv. 126, n. 3
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/4011726
dc.description.abstractThe classical deconvolution imaging condition consists of dividing the upgoing wave field by the downgoing wave field and summing over all frequencies and sources. The least-squares imaging condition consists of summing the cross-correlation of the upgoing and downgoing wave fields over all frequencies and sources, and dividing the result by the total energy of the downgoing wave field. This procedure is more stable than using the classical imaging condition, but it still requires stabilization in zones where the energy of the downgoing wave field is small. To stabilize the least-squares imaging condition, the energy of the downgoing wave field is replaced by its average value computed in a horizontal plane in poorly illuminated regions. Applications to the Marmousi and Sigsbee2A data sets show that the stabilized least-squares imaging condition produces better images than the least-squares and cross-correlation imaging conditions.
dc.languageen
dc.rightsAcesso Aberto
dc.sourcehttp://dx.doi.org/10.1088/1742-2132/6/3/005
dc.subjectOne-way wave equation migration
dc.subjectImaging condition
dc.subjectSeismic migration
dc.subjectAcoustic wave
dc.subjectLeast-square imaging condition
dc.subjectDeconvolution imaging condition
dc.titleA new stabilized least-squares imaging condition
dc.typeArtigo de Periódico


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