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Computation of rays in an inhomogeneous transverselly isotropic medium with a non-vertical axis of symmetry

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Нa основе меmо¶rt;uкu оnuсaнноŭ в [1], выве¶rt;ены ¶rt;uфференцuaльные урaвненuя сеŭсмuческого лучa в 2-D нео¶rt;норо¶rt;ноŭ, nоnеречно uзоmроnноŭ сре¶rt;е с нaклонноŭ осью сыммеmрuu. Оnuсaны резульmamы вычuсленuŭ ¶rt;ля некоmорых сnецuaльно оnре¶rt;еленных сре¶rt;.

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References

  1. V. Červený, I. A. Molotkov, I. Pšenčík: Ray Method in Seismology. Univ. Karlova, Praha 1977.

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  2. V. Červený, I. Pšenčík: Paprskové metody výzkumu seismických vln v nehomogenních anizotropních prostředích. Program AN2 — transversálně izotropní vertikálně nehomogenní prostředí bez rychlostních rozhraní. Výzk. zpr. č. 21, MFF KU, Praha 1975 (not published).

  3. E. M. Chesnokov: Private communication.

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Jech, J. Computation of rays in an inhomogeneous transverselly isotropic medium with a non-vertical axis of symmetry. Stud Geophys Geod 27, 114–121 (1983). https://doi.org/10.1007/BF01588984

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