dc.creatorDe Araujo Simoes-Filho I.
dc.date1993
dc.date2015-06-30T14:31:57Z
dc.date2015-11-26T14:43:37Z
dc.date2015-06-30T14:31:57Z
dc.date2015-11-26T14:43:37Z
dc.date.accessioned2018-03-28T21:51:51Z
dc.date.available2018-03-28T21:51:51Z
dc.identifier
dc.identifierGeophysical Research Letters. , v. 20, n. 14, p. 1491 - 1494, 1993.
dc.identifier948276
dc.identifier
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-0027871017&partnerID=40&md5=c00894c69926801cc3ffc87dd0316a2f
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/99689
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/99689
dc.identifier2-s2.0-0027871017
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1251759
dc.descriptionThe accuracy of perturbation methods for traveltime computations in anisotropic media is investigated as a function of the medium deviation from isotropy. The traveltime perturbation equations are briefly reviewed and a method for the choice of the isotropic background is proposed. The perturbed traveltimes are then compared with results of exact ray tracing for four different anisotropic models with orthorhombic symmetry and increasing anisotropy. The accuracy of the perturbed traveltimes is very good for media with small perturbations and decreases rapidly for perturbations larger than 15%. -Author
dc.description20
dc.description14
dc.description1491
dc.description1494
dc.languageen
dc.publisher
dc.relationGeophysical Research Letters
dc.rightsaberto
dc.sourceScopus
dc.titleThe Accuracy Of Traveltime Perturbations From Isotropic To Anisotropic Medium
dc.typeArtículos de revistas


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