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A note on two-point paraxial travel times

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F13%3A10172680" target="_blank" >RIV/00216208:11320/13:10172680 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1007/s11200-012-0373-6" target="_blank" >http://dx.doi.org/10.1007/s11200-012-0373-6</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s11200-012-0373-6" target="_blank" >10.1007/s11200-012-0373-6</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    A note on two-point paraxial travel times

  • Original language description

    Recently, several expressions for the two-point paraxial travel time in laterally varying, isotropic or anisotropic layered media were derived. The two-point paraxial travel time gives the travel time from point S' to point R', both these points being situated close to a known reference ray Omega, along which the ray-propagator matrix was calculated by dynamic ray tracing. The reference ray and the position of points S' and R' are specified in Cartesian coordinates. Two such expressions for the two-point paraxial travel time play an important role. The first is based on the 4 x 4 ray propagator matrix, computed by dynamic ray tracing along the reference ray in ray-centred coordinates. The second requires the knowledge of the 6 x 6 ray propagator matrixcomputed by dynamic ray tracing along the reference ray in Cartesian coordinates. Both expressions were derived fully independently, using different methods, and are expressed in quite different forms. In this paper we prove that the two

  • 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

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

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)

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

    Studia Geophysica et Geodaetica

  • ISSN

    0039-3169

  • e-ISSN

  • Volume of the periodical

    57

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    9

  • Pages from-to

    267-275

  • UT code for WoS article

    000319008000007

  • EID of the result in the Scopus database