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Weak-anisotropy approximation of P-wave reflection coefficient in anisotropic media of arbitrary symmetry and tilt

dc.contributor.authorPšenčík, Ivan
dc.contributor.authorFarra, Veronique
dc.date.accessioned2023-01-23T12:40:45Z
dc.date.available2023-01-23T12:40:45Z
dc.date.issued2022
dc.identifier.urihttps://hdl.handle.net/20.500.14178/1669
dc.description.abstractApplicability of the approximate expression for the P-wave reflection coefficient at a weak-contrast reflector separating two weakly anisotropic half-spaces of arbitrary symmetry is extended to media of arbitrary symmetry and tilt. The reflection coefficient consists of the approximate P-wave reflection coefficient at a weak-contrast interface separating two reference isotropic half-spaces and a correction term due to anisotropy. Along an arbitrarily chosen profile, the "isotropic" term depends on the density and P- and S-wave contrasts, and the correction term depends linearly on the contrasts of four profile weak-anisotropy (WA) parameters specifying anisotropy along the profile. In addition, both terms depend on the polar angle of incidence. In each half-space, the four profile WA parameters can be expressed as a linear combination of 12 of 21 global WA parameters specifying anisotropy of the half-space. Coefficients of this linear combination are functions of the azimuth of the profile. WA parameters are a generalization of Thomsen parameters to arbitrary anisotropy and represent an alternative to 21 independent elements of the stiffness tensor. WA parameters can be used for the approximation of other related concepts such as the reflection moveout or the geometric spreading. Presented tests illustrate high accuracy and flexibility of the proposed formula for the P-wave reflection coefficient. They also show that very accurate results can be obtained for contrasts and anisotropy, which cannot be considered weak.en
dc.language.isoen
dc.relation.urlhttps://doi.org/10.1190/GEO2021-0471.1
dc.rightsIvan Pšenčík and Véronique Farra, (2022), "Weak-anisotropy approximation of P-wave reflection coefficient in anisotropic media of arbitrary symmetry and tilt," GEOPHYSICS 87: C39-C48. To view the published open abstract, go to http://dx.doi.org and enter the DOI. https://library.seg.org/page/policies/open-access
dc.titleWeak-anisotropy approximation of P-wave reflection coefficient in anisotropic media of arbitrary symmetry and tilten
dcterms.accessRightsopenAccess
dcterms.licensehttps://doi.org/10.1190/geo2021-0471.1
dc.date.updated2023-10-02T06:12:32Z
dc.subject.keywordtransmission coefficientsen
dc.subject.keywordcontrast approximationen
dc.relation.fundingReferenceinfo:eu-repo/grantAgreement/GA0/GA/GA20-06887S
dc.date.embargoStartDate2023-10-02
dc.type.obd73
dc.type.versioninfo:eu-repo/semantics/publishedVersion
dc.identifier.doi10.1190/GEO2021-0471.1
dc.identifier.utWos000793467000004
dc.identifier.eidScopus2-s2.0-85125855544
dc.identifier.obd620128
dc.identifier.rivRIV/00216208:11320/22:10452469
dc.subject.rivPrimary10000::10500
dcterms.isPartOf.nameGeophysics
dcterms.isPartOf.issn0016-8033
dcterms.isPartOf.journalYear2022
dcterms.isPartOf.journalVolume87
dcterms.isPartOf.journalIssue3
uk.faculty.primaryId116
uk.faculty.primaryNameMatematicko-fyzikální fakultacs
uk.faculty.primaryNameFaculty of Mathematics and Physicsen
uk.department.primaryId1276
uk.department.primaryNameKatedra geofyzikycs
uk.department.primaryNameDepartment of Geophysicsen
dc.description.pageRangeC39-C48
dc.type.obdHierarchyCsČLÁNEK V ČASOPISU::článek v časopisu::původní článekcs
dc.type.obdHierarchyEnJOURNAL ARTICLE::journal article::original articleen
dc.type.obdHierarchyCode73::152::206en
uk.displayTitleWeak-anisotropy approximation of P-wave reflection coefficient in anisotropic media of arbitrary symmetry and tilten


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