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  • 1
    Monograph available for loan
    Monograph available for loan
    Subduction zones; Part I (1988)
    Basel : Birkhäuser
    Associated volumes
    Details Availability
    Call number: G 9097/1
    In: Subduction zones
    Type of Medium: Monograph available for loan
    Pages: Seiten 449 - 800 , Illustrationen, Diagramme
    ISBN: 3-7643-1928-3 , 0-8176-1928-3
    URL: https://link.springer.com/journal/24/128/3
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Subduction zones; Part II (1989)
    Basel : Birkhäuser
    Associated volumes
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    Call number: G 9097/2
    In: Subduction zones
    Type of Medium: Monograph available for loan
    Pages: 282 Seiten , Illustrationen, Diagramme
    ISBN: 3-7643-2272-1 , 0-8176-2272-1
    URL: https://link.springer.com/journal/24/129/1
    Language: English
    Location: Upper compact magazine
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  • 3
    Monograph available for loan
    Monograph available for loan
    Earthquake seismology; Vol. 4.
    Associated volumes
    Details Availability
    Call number: 5/M 08.0033/4
    In: Treatise on geophysics
    Type of Medium: Monograph available for loan
    Pages: xii, 700 S.
    ISBN: 9780444519320
    Location: Reading room
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Earthquakes : observation, theory and interpretation (1983)
    Amsterdam [u.a.] : North-Holland Publ.
    Associated volumes
    Details Availability
    Call number: 14382
    In: Proceedings of the International School of Physics Enrico Fermi
    Type of Medium: Monograph available for loan
    Pages: XVI, 608 S. : Ill., graph. Darst.
    ISBN: 0444866795
    Series Statement: Proceedings of the International School of Physics "Enrico Fermi" 85
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 5
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    Subduction Zones, Part II (1989)
    Basel, Boston, Berlin : Birkhäuser
    Details
    Description / Table of Contents: Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, subduction zones are a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa­ tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC.
    Pages: Online-Ressource (V, 282 Seiten)
    ISBN: 9783034891400
    URL: http://link.springer.com/journal/24/129/1/
    Language: English
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  • 6
    Electronic Resource
    Electronic Resource
    REAL-TIME SEISMOLOGY AND EARTHQUAKE DAMAGE MITIGATION (2005)
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 33 (2005), S. 195-214 
    Details
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Real-time seismology refers to a practice in which seismic data are collected and analyzed quickly after a significant seismic event, so that the results can be effectively used for postearthquake emergency response and early warning. As the technology of seismic instrumentation, telemetry, computers, and data storage facility advances, the real-time seismology for rapid postearthquake notification is essentially established. Research for early warning is still underway. Two approaches are possible: (a) regional warning and (b) on-site (or site-specific) warning. In (a), the traditional seismological method is used to locate an earthquake, determine the magnitude, and estimate the ground motion at other sites. In (b), the beginning of the ground motion (mainly P wave) observed at a site is used to predict the ensuing ground motion at the same site. An effective approach to on-site warning is discussed in light of earthquake rupture physics.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1146/annurev.earth.33.092203.122626
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  • 7
    Electronic Resource
    Electronic Resource
    Reply to comment by J. Trampert (1990)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 103 (1990), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1990.tb05686.x
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  • 8
    Electronic Resource
    Electronic Resource
    Comparison of Iterative Back-Projection Inversion and Generalized Inversion Without Blocks: Case Studies In Attenuation Tomography (1989)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 97 (1989), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Iterative back-projection tomography and generalized inversion without blocks (‘no-block’) are two different inversion techniques developed recently for 3-D studies, and are commonly applied to the inversion of travel-time data. In this study, we compare the two methods and derive one from the other under certain assumptions. We then apply these two methods to the attenuation problem, inverting for the quality factor, Q, of the medium. Usually, travel-time inversion involves large data sets and fine resolution is not possible if generalized inversion is applied. A relatively small data set with little redundancy enables us to apply both techniques with similar resolution. We applied the methods to the data sets obtained for two areas in southern California, the Coso-Indian Wells region and Imperial Valley. the results obtained by the two methods are very similar. Back-projection tomography is a direct and fast method for this type of problem. However, it does not provide formal error estimates and resolution. the no-block inversion requires more computational time, but formal errors and resolution can be directly computed for the final model. Thus, application of the two methods to the same data set enhances the objectivity of the final result.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1989.tb00481.x
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  • 9
    Electronic Resource
    Electronic Resource
    Quantification of Earthquakes (1978)
    [s.l.] : Nature Publishing Group
    Nature 271 (1978), S. 411-414 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Because earthquakes are the result of complex geophysical processes, it is not a simple matter to find a single measure of the size of an earthquake. Further, extremely large earthquakes saturate the conventional magnitude scale. Recent estimates of energy released by such earthquakes suggest ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/271411a0
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  • 10
    Electronic Resource
    Electronic Resource
    The wake of a legendary earthquake (1996)
    [s.l.] : Nature Publishing Group
    Nature 379 (1996), S. 203-204 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] WHETHER a giant earthquake could occur in the Cascadia subduction zone, off the Oregon and Washington coast of North America, has been a subject of hot debate for the past decade because of the tremendous destructive potential of such an event. Many lines of evidence, from plate tectonics to ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/379203a0
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