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  • 1
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    In:  Geophys. J. R. astr. Soc., London, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 81, no. 4, pp. 429-444, pp. B02206, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 1985
    Keywords: Moment tensor ; Statistical investigations ; Seismology ; GJRaS ; nokms
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  • 2
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    In:  Science, London, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 236, no. 4, pp. 1563-1567, pp. B02206, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 1987
    Keywords: Seismicity ; Earthquake precursor: prediction research ; Statistical investigations ; Fracture ; growth ; Fore-shocks
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  • 3
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    In:  Bull. Seism. Soc. Am., Wiesbaden, Bundesanstalt f. Geowissenschaften und Rohstoffe (BGR) und die Staatlichen Geologischen Dienste in der Bundesrepublik Deutschland, Vertrieb: E. Schweizerbart'sche Verlagsbuchhandlung (Nägele und Obermiller), Stuttgart, vol. 61, no. 3, pp. 893-912, pp. 1006, (ISSN: 1340-4202)
    Publication Date: 1991
    Keywords: Seismology ; Surface waves ; Inelastic ; Layers ; BSSA
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  • 4
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    In:  Geophys. J. RAS, DGG and EGS, Reykjavík, Icelandic Meteorological Office, Ministry for the Environment, University of Iceland, vol. 96, no. 5694, pp. 389-399, pp. 2212, (ISSN: 1340-4202)
    Publication Date: 1989
    Keywords: Earthquake precursor: statistical anal. of seismicity ; Earthquake precursor: prediction research ; Rock mechanics ; Stress ; Fore-shocks ; Statistical investigations
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  • 5
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    In:  J. Geophys. Res., Reykjavík, Icelandic Meteorological Office, Ministry for the Environment, University of Iceland, vol. 97, no. 5694, pp. 19873-19879, pp. 2212, (ISSN: 1340-4202)
    Publication Date: 1992
    Keywords: Earthquake precursor: prediction research ; Earthquake precursor: statistical anal. of seismicity ; Statistical investigations ; JGR
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  • 6
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 1987-06-19
    Description: A statistical procedure, derived from a theoretical model of fracture growth, is used to identify a foreshock sequence while it is in progress. As a predictor, the procedure reduces the average uncertainty in the rate of occurrence for a future strong earthquake by a factor of more than 1000 when compared with the Poisson rate of occurrence. About one-third of all main shocks with local magnitude greater than or equal to 4.0 in central California can be predicted in this way, starting from a 7-year database that has a lower magnitude cut off of 1.5. The time scale of such predictions is of the order of a few hours to a few days for foreshocks in the magnitude range from 2.0 to 5.0.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kagan, Y Y -- Knopoff, L -- New York, N.Y. -- Science. 1987 Jun 19;236(4808):1563-7.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17835741" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 133 (1990), S. 547-551 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 131 (1989), S. 551-576 
    ISSN: 1420-9136
    Keywords: Composite materials ; elastic waves ; cracked materials
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This paper will summarise the present state of knowledge concerning the elastic and dissipative properties of composite materials in the long wavelength or static approximation. In this case the material, although containing numerous inclusions or cracks or other types of microstructure, can be regarded as a continuum. Established results are listed for the elastic parameters following a review of approximate and exact methods of their derivation.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 96 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We have constructed a model for the occurrence of foreshocks and foreshock sequences. The foreshocks as well as the main shock are assumed to occur because of the abrupt coalescence of pre-existing cracks. Coalescence occurs if the stress intensity factors at the crack tips exceed a certain critical value. In the sub-critical state each crack undergoes accelerated extension quasi-statically due to stress corrosion, until it reaches the critical state, at which point growth becomes catastrophic.The rate of foreshock occurrence increases as the time of the main shock approaches and is described by a power law function of time. The exponent in the power law is independent of the distributions of crack sizes, spacings and fracture strengths. This universality implies that foreshock patterns should be useful identifiers for the prediction of the occurrence times of large earthquakes. However, we find that there is considerable diversity in the patterns of energy release. Nevertheless, there is some hope that the magnitudes of large earthquakes can be predicted from the magnitudes of the events in the foreshock sequences if one has a priori information describing the distributions of barrier strengths and geometries.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 335 (1988), S. 690-694 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Pattern recognition procedures for infrequent events are adapted to the problem of identifying patterns of clustering of small- and intermediate-scale seismicity before large earthquakes. Identification procedures derived from analysis of large California and Nevada earthquakes yield a high success ...
    Type of Medium: Electronic Resource
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