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  • Articles  (22)
  • Other Sources  (6)
  • 2000-2004  (8)
  • 1990-1994  (2)
  • 1985-1989  (17)
  • 1965-1969  (1)
Collection
  • Books  (1)
  • Articles  (22)
  • Other Sources  (6)
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Year
Journal
  • 1
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    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 17, no. 5, pp. 1509-1511, pp. B04313, (ISBN: 0-12-018847-3)
    Publication Date: 1990
    Keywords: Non-linear effects ; Three dimensional ; Seismics (controlled source seismology) ; Inversion ; Applied geophysics ; Cerveny ; GRL
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  • 2
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    In:  J. Geophys., Warszawa, Conseil de l'Europe, vol. 58, no. March, pp. 2-26, pp. 1095, (ISBN: 0-12-018847-3)
    Publication Date: 1985
    Keywords: Synthetic seismograms ; Two-dimensional ; Three dimensional ; Cerveny
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  • 3
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    In:  Geophys. J. Int., Warszawa, Conseil de l'Europe, vol. 107, no. March, pp. 219-229, pp. 1095, (ISBN: 0-12-018847-3)
    Publication Date: 1991
    Keywords: Anisotropy ; Seismology ; Travel time ; Inhomogeneity ; Simoes-Filho ; GJI ; Cerveny
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  • 4
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    In:  Izv. Phys. Solid Earth, Earth Physics Ser., Warszawa, Conseil de l'Europe, vol. 8, no. March, pp. 518, pp. 1095, (ISBN: 0-12-018847-3)
    Publication Date: 1965
    Keywords: Waves ; Reflectivity ; Head waves ; Cerveny
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  • 5
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    Cambridge Univ. Press, 713 pp.
    In:  Prague, 214 pp., Cambridge Univ. Press, 713 pp., vol. 42, no. 3, pp. 275-291, (0-596-00648-9, 3rd edition 2005. XXII, 509 pp.)
    Publication Date: 2001
    Keywords: Waves ; Textbook of geophysics ; Wave propagation ; Seismics (controlled source seismology) ; Seismology ; Ray seismics ; Ray tracing ; GJI ; Cerveny
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  • 6
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    In:  Pageoph, New York, Scientific American, vol. 159, no. 7-8, pp. 1401-1402, pp. B04305, (ISSN: 1340-4202)
    Publication Date: 2002
    Keywords: Waves ; Inhomogeneity ; Modelling ; Wave propagation ; Gauss ; beams ; Psencik ; Cerveny
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 99 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An approximate hybrid approach to computing high-frequency body wave synthetic seismograms in 2-D and 3-D laterally varying layered structures containing thin transition layers is suggested. It combines the ray method with the matrix (reflectivity) method. The ray method is applied to thick layers with smooth variations of velocity and the reflectivity method is applied to thin transition layers. Alternatively, the method of summation of Gaussian beams is used instead of the ray method in the hybrid code. An algorithm and the relevant program package BEAM87, designed for such hybrid computations in 2-D laterally varying layered structures containing one laterally varying thin transition layer, are briefly described. The thin transition layer may represent a region of a high velocity gradient, a laminated region, a region of a low Q, etc. It is simulated by a stack of very thin layers. The accuracy of the hybrid computations is tested on 1-D models by the comparison with reflectivity-method computations. The hybrid method yields sufficiently accurate results for transition layers, the thickness of which is smaller than one half of the prevailing wavelength of the wavefield under consideration, particularly for small angles of incidence. For reflected waves, the best accuracy is obtained for subcritical reflections, but the accuracy is lower for critical and overcritical reflections. The accuracy in the critical region is improved, if the Gaussian beam summation method is used instead of the ray method in the hybrid scheme. Numerical examples of synthetic body wave seismograms for a laterally varying model containing thin transition layers of various types are presented.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 99 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A concept of a factorized anisotropic inhomogeneous (FAI) medium is introduced. In the FAI medium, the position dependent density normalized elastic parameters aijkl(Xi) can be factorized in the following sense: aijkl(Xi) =f2(xi)Aijkl, where Aijkl are constants, independent of Cartesian coordinates xi, and f(xi) is an arbitrary continuous function of xi. Thus, all the density normalized elastic parameters aijkl(xi) in the FAI medium depend on the coordinates xi in the same way, but the generality of anisotropy and of inhomogeneity is not restricted. The factorization of aijkl(xi) leads to a factorization of certain important ray theory expressions and equations (eikonal equation, etc.), and to particularly simple ray tracing and dynamic ray tracing. For certain types of FAI media, these equations may even be solved analytically or semianalytically.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 29 (1985), S. 228-237 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Description / Table of Contents: Summary A method of spectral analysis based on the prediction of the signal by means of AR parameters is proposed. The essence of this method ranks it between the classical methods of spectral analysis and the method of maximum entropy. For sufficiently high SNR its resolution is higher than that of the classical methods. The new method enables power and phase spectra of the signal to be determined, and provides a better determination of the power spectrum amplitude. than the method of maximum entropy. A regularization procedure is presented which abolished the instability of the prediction filter, obtained by the least-squares method.
    Notes: Резюме Пре¶rt;ложен сnособ сnекmрaльного aнaлuзa, основaнняыŭ нa nре¶rt;скaзaнuu сuгнaлa с nомощью aвmорегрессuонных naрaмеmров. Эmоm сnособ являеmся ¶rt;aльнеŭшuм рaзвumuем клaссuческuх мзmо¶rt;ов сnекmрaльного aнaлuзa с nрuвлеченuем u¶rt;еŭ uз меmо¶rt;a мaксuмaльноŭ энmроnuu. Сnособ облa¶rt;aеm nовышенноŭ рaэрешaющеŭ сnособносmью nо срaвненuю с клaссuческuмu меmо¶rt;aмu nрu aнaлuэе nроцессов с ¶rt;осmamочно хорошuм оmношенuем сuгнaл шум. Сnекmр мощносmu сuгнaлов оnре¶rt;еляеmср более нa¶rt;ежно, чем в меmо¶rt;е мaксuмaльноŭ энmроnuu. Воmлuчuе оm меmо¶rt;a мaксuмaльноŭ энmроnuu nре¶rt;ложенныŭ сnособ сnекmрaльного aнaлuзa nозволяеm оnре¶rt;еляmь mоже фaзовыŭ сnекmр сuгнaлов. Пaрaмеmры nре¶rt;скaзывaющего фuльmрa вычuсляюmся меmо¶rt;ом нauменьшuх квa¶rt;рamов, в коmором uсnользовaнa регулярuзaцuя ¶rt;ля вы¶rt;еленuя усmоŭчuвых облaсmеŭ решенuя.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 30 (1986), S. 242-256 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Description / Table of Contents: Summary The algorithm of iterative geophysical tomography is presented. The medium is approximated smoothly by means of B-splines. The tww-point problem of ray computation is solved with the aid of paraxial approximation. The parameters of the medium are obtained from the iterative algorithm of minimizing the quadratic form. Two numerical 2-D examples are given.
    Notes: Резюме Прuве¶rt;еи aлгорuфм umерamuвноŭгеофuзuческоŭ mомогрaфuu. Сре¶rt;a annроксuмuровaнa сnлощно nрu nомощu Б-сnлaŭнов. Пвухmочнaя nроблеммa рaсчемa лучеŭ рещенa nрu nомощu naрaксuaлноŭ annроксuмaцuu. Пaрaмеmры сре¶rt;ы nолучены иa основе umерamuвного aлгорuфмa мuнuмaлuзaцuu квa¶rt;рamuческоŭ формы. В рaбоmе nрuве¶rt;ены ¶rt;вa 2-D чuсленных nрuмерa.
    Type of Medium: Electronic Resource
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