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Weak-anisotropy approximations of P-wave phase and ray velocities for anisotropy of arbitrary symmetry

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    SYSNO ASEP0458982
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleWeak-anisotropy approximations of P-wave phase and ray velocities for anisotropy of arbitrary symmetry
    Author(s) Farra, V. (FR)
    Pšenčík, Ivan (GFU-E) ORCID, RID
    Source TitleStudia geophysica et geodaetica. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0039-3169
    Roč. 60, č. 3 (2016), s. 403-418
    Number of pages16 s.
    Publication formPrint - P
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsweak anisotropy ; P-wave ; phase velocity ; ray velocity
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    Institutional supportGFU-E - RVO:67985530
    UT WOS000382365100004
    EID SCOPUS84964199174
    DOI10.1007/s11200-015-1276-0
    AnnotationWe test the accuracy of the previously derived weak-anisotropy approximations of the P-wave phase and ray (group) velocities. The formulae are of varying accuracy, and are applicable to weak or moderate anisotropy of arbitrary symmetry and orientation. They have a form of expressions for squares of phase velocity depending on the phase-velocity direction and of ray velocity depending on the ray-velocity direction. Both velocities are expressed in terms of three elements of the rotated Christoffel matrix, which depend linearly on the parameters specifying the medium, the weak-anisotropy parameters. The least accurate formulae are fully independent of the choice of a reference isotropic medium and depend linearly on weak-anisotropy parameters. The most accurate formulae depend only slightly on the ratio of S- and P-wave velocities of a reference medium, their dependence on weak-anisotropy parameters being quadratic. We show that the accuracy of the formulae is quite high, in fact, in some cases, it is close to the accuracy of the socalled anelliptic approximations, very accurate approximations based on a perturbation of the elliptical anisotropy.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2017
Number of the records: 1  

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