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  • 1
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    Birkhäuser
    In:  Basel, 348 pp., Birkhäuser, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 1-58488-323-5)
    Publication Date: 1996
    Keywords: Waves ; Seismology ; Inhomogeneity ; Wave propagation ; Modelling ; Synthetic seismograms ; Textbook of geophysics ; Psencik ; Cerveny
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  • 2
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    In:  Geophys. J. Int., Dordrecht, National Academy of Sciences of the USA, vol. 121, no. 4, pp. 459-474, pp. TC5003, (ISSN: 1340-4202)
    Publication Date: 1995
    Keywords: Three dimensional ; Inversion ; Waves ; Source ; Psencik ; GJI
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  • 3
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    Birkhäuser
    In:  Basel, 376 pp., Birkhäuser, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 1-58488-323-5)
    Publication Date: 1996
    Keywords: Waves ; Seismology ; Inhomogeneity ; Wave propagation ; Modelling ; Synthetic seismograms ; Textbook of geophysics ; Psencik ; Cerveny
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 151 (1998), S. 699-718 
    ISSN: 1420-9136
    Keywords: Key words: Weak anisotropy, weak contrast interface, plane wave reflection and transmission coeffi cients.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract —Approximate PP plane wave displacement coefficients of reflection and transmission for weak contrast interfaces separating weakly but arbitrarily anisotropic elastic media are presented. The PP reflection coefficient for such an interface has been derived recently by Vavryčuk and Pšenčík (1997). The PP transmission coefficient presented in this paper was derived by the same approach. The coefficients are given as a sum of the coefficient for the weak contrast interface separating two nearby isotropic media and a term depending linearly on contrasts of the so-called weak anisotropy (WA) parameters (parameters specifying deviation of properties of the medium from isotropy), across the interface. While the reflection coefficient depends only on 8 of the complete set of the WA parameters describing P-wave phase velocity in weakly anisotropic media, the transmission coefficient depends on their complete set. The PP reflection coefficient depends on "shear-wave splitting parameter" γ. Tests of accuracy of the approximate formulae are presented on several models.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1573-8795
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mathematics
    Notes: Abstract An algorithm for computing the second term of the series of the ray method in the case of elastic inhomogeneous isotropic media is proposed. The main idea of the approach to the problem can be formulated as follows. Let a central (or support) ray of a ray tube be known. If we inroduce the ray-centered coordinates s, q1, q2 in the vicinity of the central ray, then the rays of the ray tube can be described by functions qi=qi(s, γ1, γ2), i=1,2, where s is the are length of the central ray and γj, j=1, 2, are the ray parameters. On the one hand, we show that the integrand of the second term of the series of the ray method can be expressed via the derivatives of the functions qi with respect to γj of the first, second, and third orders. On the other hand, additional differential equations for the derivatives as functions of s can be obtained from Euler's equations for the rays. This paper also contains initial conditions for the derivatives in the case of a point source. Thus, we obtain an algorithm involving additional differential equations for the derivatives $$\frac{{\partial q_i }}{{\partial \gamma _j }},\frac{{\partial ^2 q_i }}{{\partial \gamma _j \gamma _k }},\frac{{\partial ^3 q_i }}{{\partial \gamma _j \gamma _k \gamma _1 }}$$ , and the initial conditions for them at the source. The algorithm for calculating the mixed components of a vector of displacement is elaborated in detail. Unfortunately, the Russian version of this paper contains some errors, which have been corrected in the English translation of the paper.
    Type of Medium: Electronic Resource
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