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  • 1
    Series available for loan
    Series available for loan
    Investigaciones gravimétricas en la región de Chillán (1959)
    Santiago de Chile
    Associated volumes
    Details Availability
    Call number: SR 90.1036(4)
    In: Boletín
    Type of Medium: Series available for loan
    Pages: 13 S. + 4 Beil.
    Series Statement: Boletin / Instituto de Investigaciones Geologicas, Chile 4
    Language: Spanish
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Global tectonics and earthquakes risk (1974)
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Details Availability
    Call number: 9/MR 90.1013
    In: Developments in geotectonics
    Type of Medium: Monograph available for loan
    Pages: XIV, 320 S.
    ISBN: 0444410767
    Series Statement: Developments in geotectonics 5
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Fundamentals of earthquake prediction (1994)
    New York [u.a.] : Wiley
    Details Availability
    Call number: M 94.0581
    Type of Medium: Monograph available for loan
    Pages: xi, 326 S.
    ISBN: 0471574198
    Classification:
    B.4.1.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
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    Three theorems of earthquake location (2006)
    In:  Bulletin of the Seismological Society of America, Kunming, China, 4, vol. 96, no. 1, pp. 306-312, pp. L13613, (ISSN: 1340-4202)
    Details
    Publication Date: 2006
    Keywords: Seismology ; Location ; Review article ; BSSA
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Huygens' Principle: The capture of seismic energy by a soft soil layer (2004)
    In:  Geophys. Res. Lett., Kunming, China, 4, vol. 31, no. 13, pp. 65 & 70, pp. L13613, (ISSN: 1340-4202)
    Details
    Publication Date: 2004
    Keywords: Site amplification ; Elasticity ; Waves ; Wave propagation ; GRL
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    Seismic Hazard of the Uttarakhand Himalaya, India, from Deterministic Modeling of Possible Rupture Planes in the Area (2013)
    Hindawi
    Details
    Publication Date: 2013-04-12
    Description: This paper presents use of semiempirical method for seismic hazard zonation. The seismotectonically important region of Uttarakhand Himalaya has been considered in this work. Ruptures along the lineaments in the area identified from tectonic map are modeled deterministically using semi empirical approach given by Midorikawa (1993). This approach makes use of attenuation relation of peak ground acceleration for simulating strong ground motion at any site. Strong motion data collected over a span of three years in this region have been used to develop attenuation relation of peak ground acceleration of limited magnitude and distance applicability. The developed attenuation relation is used in the semi empirical method to predict peak ground acceleration from the modeled rupture planes in the area. A set of values of peak ground acceleration from possible ruptures in the area at the point of investigation is further used to compute probability of exceedance of peak ground acceleration of values 100 and 200 gals. The prepared map shows that regions like Tehri, Chamoli, Almora, Srinagar, Devprayag, Bageshwar, and Pauri fall in a zone of 10% probability of exceedence of peak ground acceleration of value 200 gals.
    Print ISSN: 1687-885X
    Electronic ISSN: 1687-8868
    Topics: Geosciences
    Published by Hindawi
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  • 7
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    Seismic Hazard of the Uttarakhand Himalaya, India, from Deterministic Modeling of Possible Rupture Planes in the Area (2013)
    Hindawi
    Details
    Publication Date: 2013-10-30
    Description: This paper presents use of semiempirical method for seismic hazard zonation. The seismotectonically important region of Uttarakhand Himalaya has been considered in this work. Ruptures along the lineaments in the area identified from tectonic map are modeled deterministically using semi empirical approach given by Midorikawa (1993). This approach makes use of attenuation relation of peak ground acceleration for simulating strong ground motion at any site. Strong motion data collected over a span of three years in this region have been used to develop attenuation relation of peak ground acceleration of limited magnitude and distance applicability. The developed attenuation relation is used in the semi empirical method to predict peak ground acceleration from the modeled rupture planes in the area. A set of values of peak ground acceleration from possible ruptures in the area at the point of investigation is further used to compute probability of exceedance of peak ground acceleration of values 100 and 200 gals. The prepared map shows that regions like Tehri, Chamoli, Almora, Srinagar, Devprayag, Bageshwar, and Pauri fall in a zone of 10% probability of exceedence of peak ground acceleration of value 200 gals.
    Print ISSN: 1687-885X
    Electronic ISSN: 1687-8868
    Topics: Geosciences
    Published by Hindawi
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  • 8
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    Jaime Urrutia Fucugauchi Receives 2013 International Award: Citation (2014)
    Wiley
    Details
    Publication Date: 2014-01-15
    Description: Jaime Urrutia Fucugauchi was born in Chihuahua, Mexico. His surname Urrutia means “distant” in Basque, and Fucugauchi means roughly “Good luck—come in!” in Japanese. And Jaime, of course, is “James” in Spanish. Thus, Jaime was international from birth. There could hardly have been a better candidate for the AGU International Award.
    Print ISSN: 0096-3941
    Electronic ISSN: 2324-9250
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Electronic Resource
    Electronic Resource
    Tectonic feedback and the earthquake cycle (1985)
    Springer
    Pure and applied geophysics 123 (1985), S. 667-682 
    Details
    ISSN: 1420-9136
    Keywords: Earthquake cycles ; fault dynamics ; loading rates
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The occurrence of cyclical instabilities along plate boundaries at regular intervals suggests that the process of earthquake causation differs in some respects from the model of elastic rebound in its simplest forms. The model of tectonic feedback modifies the concept of this original model in that it provides a physical interaction between the loading rate and the state of strain on the fault. Two examples are developed: (a) Central Chile, and (b) Mexico. The predictions of earthquake hazards for both types of models are compared.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00878401
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  • 10
    Electronic Resource
    Electronic Resource
    The Oaxaca gap: A case history (1979)
    Springer
    Pure and applied geophysics 117 (1979), S. 1187-1194 
    Details
    ISSN: 1420-9136
    Keywords: Earthquake prediction ; Seismicity gap ; Tectonics of Mexico
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract An attempted use of seismic gap observations to predict a large earthquake in Oaxaca, Mexico is discussed. The observations were initially published in a scientific journal and were subsequently distorted by noncientists, who predicted a major earthquake and tsunami to take place at Pinotepa Nacional, Oaxaca on 23 April 1978. Public reactions and property losess sustained by individuals and communities were comparable to those expected from an actual earthquake. A revision of epicenter locations from the NOAA data file revealed that a number of earthquakes did occur in the alleged gap but had been excluded because their reported focal depth was in excess of 60 km. It is shown that the probability that the number of earthquakes in two consecutive time intervals of a stationary Poisson process differs by an amount which would be reported as a ‘seismic gap’ is of the order of 5% or more for Oaxaca. This means that spurious ‘seismic gaps’ would be observed in one out of 20 data runs. The possibility of detecting a true interval of abnormal quiescence in a random earthquake sequence appears to be fairly remote in this case.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00876214
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