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Estimation of parameters and thickness of a horizontal layer of arbitrary anisotropy from P-wave moveout

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F21%3A00547522" target="_blank" >RIV/67985530:_____/21:00547522 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11320/21:10438478

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0926985121002214" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0926985121002214</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.jappgeo.2021.104473" target="_blank" >10.1016/j.jappgeo.2021.104473</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Estimation of parameters and thickness of a horizontal layer of arbitrary anisotropy from P-wave moveout

  • Original language description

    We present an inversion scheme to estimate anisotropy parameters and thickness of a homogeneous layer of arbitrary anisotropy from traveltimes of a reflected P wave. The scheme is based on the weak-anisotropy approximation of P-wave moveout formula. For the description of anisotropy, we use the so-called A-parameters, which represent an alternative to standard elastic moduli specifying anisotropic media, and allow specification of anisotropy of any symmetry, orientation and strength. The proposed scheme allows estimation of, at most, nine of fifteen A-parameters, which describe P-wave propagation in the weak-anisotropy approximation. Therefore, generally, the reconstruction of the P-wave phase-velocity surface from the estimated parameters is impossible. If we deal, however, with higher-symmetry anisotropy (transversely isotropic, orthorhombic) and if information about the orientation of its symmetry elements is available, reconstruction of the phase-velocity surface is possible. Synthetic tests indicate that the inversion scheme works well even in situations, in which the use of other commonly used moveout formulae leads to unsatisfactory results.

  • 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

    10507 - Volcanology

Result continuities

  • Project

    <a href="/en/project/GA20-06887S" target="_blank" >GA20-06887S: Seismic waves in heterogeneous anisotropic viscoelastic media</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Journal of Applied Geophysics

  • ISSN

    0926-9851

  • e-ISSN

    1879-1859

  • Volume of the periodical

    195

  • Issue of the periodical within the volume

    December

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    12

  • Pages from-to

    104473

  • UT code for WoS article

    000731732200001

  • EID of the result in the Scopus database

    2-s2.0-85118491714