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Calculation of the amplitudes of elastic waves in anisotropic media in Cartesian or ray-centred coordinates

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F19%3A10404493" target="_blank" >RIV/00216208:11320/19:10404493 - isvavai.cz</a>

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=7XUJJUg07N" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=7XUJJUg07N</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s11200-018-1251-7" target="_blank" >10.1007/s11200-018-1251-7</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Calculation of the amplitudes of elastic waves in anisotropic media in Cartesian or ray-centred coordinates

  • Original language description

    We derive various expressions for the amplitude of the ray-theory approximation of elastic waves in heterogeneous anisotropic media, and show their mutual relations. The amplitude of a wavefield with general initial conditions can be expressed in terms of two paraxial vectors of geometrical spreading in Cartesian coordinates, and in terms of the 2x2 matrix of geometrical spreading in ray-centred coordinates. The amplitude of the Green tensor can be expressed in six different ways: (a) in terms of the paraxial vectors corresponding to two ray parameters in Cartesian coordinates, (b) in terms of the 2x2 paraxial matrices corresponding to two ray parameters in ray-centred coordinates, (c) in terms of the 3x3 upper right submatrix of the 6x6 propagator matrix of geodesic deviation in Cartesian coordinates, (d) in terms of the 2x2 upper right submatrix of the 4x4 propagator matrix of geodesic deviation in ray-centred coordinates, (e) in terms of the 3x3 matrix of the mixed second-order spatial derivatives of the characteristic function with respect to the source and receiver Cartesian coordinates, and (f) in terms of the 2x2 matrix of the mixed second-order spatial derivatives of the characteristic function with respect to the source and receiver ray-centred coordinates. The step-by-step derivation of various equivalent expressions, both known or novel, elucidates the mutual relations between these expressions.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

    <a href="/en/project/GA16-05237S" target="_blank" >GA16-05237S: Seismic waves in inhomogeneous weakly anisotropic media</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2019

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Studia Geophysica et Geodaetica

  • ISSN

    0039-3169

  • e-ISSN

  • Volume of the periodical

    63

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    18

  • Pages from-to

    229-246

  • UT code for WoS article

    000469250500004

  • EID of the result in the Scopus database

    2-s2.0-85067649391