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Inversion for weak triclinic anisotropy from acoustic axes

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F13%3A00397121" target="_blank" >RIV/67985530:_____/13:00397121 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.wavemoti.2012.11.003" target="_blank" >http://dx.doi.org/10.1016/j.wavemoti.2012.11.003</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.wavemoti.2012.11.003" target="_blank" >10.1016/j.wavemoti.2012.11.003</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Inversion for weak triclinic anisotropy from acoustic axes

  • Original language description

    Acoustic axes are directions in anisotropic elastic media, in which phase velocities of two or three plane waves (P, S1 or S2 waves) coincide. Acoustic axes are important, because they can cause singularities in the field of polarization vectors and anomalies in the shape of the slowness surface. The maximum number of acoustic axes in triclinic anisotropy is 16, and their directions depend on anisotropy parameters in a complicate way. Under weak anisotropy approximation this dependence simplifies and the directions of acoustic axes can be used for the inversion for anisotropy parameters. The maximum acoustic axes under weak anisotropy is 16, the minimum number of acoustic axes is zero. In the inversion, we can retrieve 13 combinations of anisotropy parameters provided we use directions of 7 acoustic axes at least. Under weak anisotropy approximation, the directions of acoustic axes are insensitive to strength of anisotropy; hence we cannot invert for absolute values of weak anisotropy

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DC - Seismology, volcanology and Earth structure

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/IAA300120801" target="_blank" >IAA300120801: Seismic waves and sources in anisotropic media II</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2013

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Wave Motion

  • ISSN

    0165-2125

  • e-ISSN

  • Volume of the periodical

    50

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    12

  • Pages from-to

    1271-1282

  • UT code for WoS article

    000326556200009

  • EID of the result in the Scopus database