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SEISMIC SURFACE WAVES IN A LATERALLY INHOMOGENEOUS EARTH By V I Keilis-borok
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SEISMIC SURFACE WAVES IN A LATERALLY INHOMOGENEOUS EARTH By V I Keilis-borok
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SEISMIC SURFACE WAVES IN A LATERALLY INHOMOGENEOUS EARTH By V I Keilis-borok

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    Características del artículo

    Estado
    Nuevo: Libro nuevo, sin usar y sin leer, que está en perfecto estado; incluye todas las páginas sin ...
    ISBN-10
    9401068852
    Book Title
    Seismic Surface Waves in a Laterally Inhomogeneous Earth (Modern
    Item Height
    9.25 inches
    ISBN
    9789401068857
    Categoría

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    Product Identifiers

    Publisher
    Springer Netherlands
    ISBN-10
    9401068852
    ISBN-13
    9789401068857
    eBay Product ID (ePID)
    175979338

    Product Key Features

    Number of Pages
    304 Pages
    Publication Name
    Seismic Surface Waves in a Laterally Inhomogeneous Earth
    Language
    English
    Publication Year
    2011
    Subject
    Physics / Geophysics, Earth Sciences / Geology
    Type
    Textbook
    Author
    T. Yanovskaya
    Subject Area
    Science
    Series
    Modern Approaches in Geophysics Ser.
    Format
    Trade Paperback

    Dimensions

    Item Weight
    16.7 Oz
    Item Length
    9.3 in
    Item Width
    6.1 in

    Additional Product Features

    Intended Audience
    Scholarly & Professional
    Preface by
    Its, E. N., Yanovskaya, T., Lander, A. V.
    Dewey Edition
    19
    Series Volume Number
    9
    Number of Volumes
    1 vol.
    Illustrated
    Yes
    Dewey Decimal
    551.2/2
    Table Of Content
    1. Theory.- 1. Surface waves in vertically inhomogeneous media.- 2. Surface waves in media with weak lateral inhomogeneity.- 3. Surface waves in media involving vertical contacts.- 4. Computation techniques for surface waves.- 2. Interpretation of Surface Wave Observations.- 5. Recording, identification, and measurement of surface wave parameters.- 6. Methods for quantitative interpretation of observations.- 7. Some results from studies of regional lithospheric structure by surface waves.- References.
    Synopsis
    Surface waves form the longest and strongest portion of a seismic record excited by explosions and shallow earthquakes. Traversing areas with diverse geologic structures, they 'absorb' information on the properties of these areas which is best retlected in dispersion, the dependence of velocity on frequency. The other prop­ erties of these waves - polarization, frequency content, attenuation, azimuthal variation of the amplitude and phase - arc also controlled by the medium between the source and the recording station; some of these are affected by the properties of the source itself and by the conditions around it. In recent years surface wave seismology has become an indispensable part of seismological practice. The maximum amplitude in the surface wave train of virtually every earthquake or major explosion is being measured and used by all national and international seismological surveys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M,. The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded every year are being analysed to estimate the seismic moment tensor of earthquake sources, to determine the periods of free oscillations of the Earth, to construct regional dispersion curves from which in turn the crustal and upper mantle structure in various areas is derived, and to evaluate the dissipative parameters of the mantle material., Surface waves form the longest and strongest portion of a seismic record excited by explosions and shallow earthquakes. Traversing areas with diverse geologic structures, they 'absorb' information on the properties of these areas which is best retlected in dispersion, the dependence of velocity on frequency. The other prop- erties of these waves - polarization, frequency content, attenuation, azimuthal variation of the amplitude and phase - arc also controlled by the medium between the source and the recording station; some of these are affected by the properties of the source itself and by the conditions around it. In recent years surface wave seismology has become an indispensable part of seismological practice. The maximum amplitude in the surface wave train of virtually every earthquake or major explosion is being measured and used by all national and international seismological surveys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M, . The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded every year are being analysed to estimate the seismic moment tensor of earthquake sources, to determine the periods of free oscillations of the Earth, to construct regional dispersion curves from which in turn the crustal and upper mantle structure in various areas is derived, and to evaluate the dissipative parameters of the mantle material.
    LC Classification Number
    QC801-809

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