All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Comparison of the anisotropic-ray-theory rays and anisotropic common S-wave rays with the SH and SV reference rays in a velocity model with a split intersection singularity

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F18%3A10385078" target="_blank" >RIV/00216208:11320/18:10385078 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.1007/s11200-015-0381-4" target="_blank" >https://doi.org/10.1007/s11200-015-0381-4</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s11200-015-0381-4" target="_blank" >10.1007/s11200-015-0381-4</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Comparison of the anisotropic-ray-theory rays and anisotropic common S-wave rays with the SH and SV reference rays in a velocity model with a split intersection singularity

  • Original language description

    We describe the behaviour of the anisotropic-ray-theory S-wave rays in a velocity model with a split intersection singularity. The anisotropic-ray-theory S-wave rays crossing the split intersection singularity are smoothly but very sharply bent. While the initial-value rays can be safely traced by solving Hamilton&apos;s equations of rays, it is often impossible to determine the coefficients of the equations of geodesic deviation (paraxial ray equations, dynamic ray tracing equations) and to solve them numerically. As a result, we often know neither the matrix of geometrical spreading, nor the phase shift due to caustics. We demonstrate the abrupt changes of the geometrical spreading and wavefront curvature of the fast anisotropic-ray-theory S wave. We also demonstrate the formation of caustics and wavefront triplication of the slow anisotropic-ray-theory S wave. Since the actual S waves propagate approximately along the SH and SV reference rays in this velocity model, we compare the anisotropic-ray-theory S-wave rays with the SH and SV reference rays. Since the coupling ray theory is usually calculated along the anisotropic common S-wave rays, we also compare the anisotropic common S-wave rays with the SH and SV reference rays.

  • 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

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

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

Others

  • Publication year

    2018

  • 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

    62

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    23

  • Pages from-to

    57-79

  • UT code for WoS article

    000424035200004

  • EID of the result in the Scopus database

    2-s2.0-85041748929