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  • 1
    Monograph available for loan
    Monograph available for loan
    Theorien zur mikroseismischen Bodenunruhe (1962)
    Leipzig : Geest & Portig
    Associated volumes
    Details Availability
    Call number: O 2453(3) ; 4041 ; 12569
    In: Geophysikalische Monographien
    Type of Medium: Monograph available for loan
    Pages: XIV, 302 S. : graph. Darst.
    Series Statement: Geophysikalische Monographien 3
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
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    Die Mikroseismik und ihre Anwendung zum Abschätzen der Dicke der Kontinentalschollen (1949)
    Springer
    Details
    Publication Date: 1949-04-01
    Print ISSN: 0033-4553
    Electronic ISSN: 1420-9136
    Topics: Geosciences , Physics
    Published by Springer
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    PAPER CURRENT
  • 3
    Electronic Resource
    Electronic Resource
    Die Mikroseismik und ihre Anwendung zum Abschätzen der Dicke der Kontinentalschollen (1949)
    Springer
    Pure and applied geophysics 14 (1949), S. 203-224 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary With the help of several weather-situations with particularty violent microseism the progress of amplitudes and periods as perceived at Stuttgart is examinated. The law of dependency between period and amplitude is found empirically, the spectrum of periods is drawn up. The period, which occurs most frequently is used for calculating the thickness of the swinging layer as this layer is supposed to be in loose connection with its support and as the sort of oscillations is not essentially different from Rayleight waves. Thus there is found the theoretical connection between periods and amplitudes and, on the other side, the thickness of layer of something more than 40 km for Norway.
    Notes: Zusammenfassung An Hand einiger Wetterlagen mit besonders starker Mikroseismik wird der Verlauf von Amplituden und Perioden in Stuttgart verfolgt. Das Gesetz der Abhängigkeit zwischen Periode und Amplitude wird empirisch ermittelt, das Periodenspektrum gezeichnet. Die am häufigsten auftretende Periode wird zur Berechnung der Dicke der schwingenden Schicht benutzt unter der Annahme, dass diese Schicht mit ihrer Unterlage lose verbunden ist und die Art der Schwingungen sich nicht wesentlich von Rayleighwellen unterscheidet. Es ergibt sich so der theore tische Zusammenhang zwischen Periode und Amplitude einerseits und der Schichtdicke andrerseits. Sie beträgt für Norwegen etwas über 40 km.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01981976
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