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  • 1
    Series available for loan
    Series available for loan
    San Diego [u.a.] : Academic Press
    Call number: ZS-002
    Type of Medium: Series available for loan
    Pages: 185 S
    ISBN: 012018835X
    Series Statement: Advances in geophysics v. 35
    Language: English
    Note: Front Cover; Advances in Geophysics, Volume 35; Copyright Page; Contents; Chapter 1. Seismological Constraints on the Velocity Structure and Fate of Subducting Lithospheric Slabs: 25 Years of Progress; 1. Introduction; 2. General Characterization of Slab and Wedge Structures; 3. Travel Time Pattern Constraints on Slab Velocity Structure; 4. Tomographical Imaging of Slab Velocity Structure; 5. Slab Boundaries: Converted and Reflected Phases; 6. Focusing, Multipathing, and Diffraction Effects of Slab Structure; 7. Future Directions in Slab Imaging and Summary; References; Index;.
    Location: Lower compact magazine
    Branch Library: PIK Library
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  • 2
    Series available for loan
    Series available for loan
    Warszawa : Panstw. Wyd. Naukowe
    Associated volumes
    Call number: SR 91.0236(86) / Regal 35
    In: Materialy i prace
    Type of Medium: Series available for loan
    Pages: 49 S.
    Series Statement: Materialy i prace 86
    Language: English
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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  • 3
    Description / Table of Contents: ing within the downgoing plate, and appears to be assoeiated with segmentation of the subdueting plate produeed by forees related to the subduetion of the Louisville Ridge. To analyze fault plane heterogeneities in the northern Solomon Islands subdue­ tion segment and their association with rupture eharaeteristics in general and the existenee of earthquake doublets in partieular, Xv and SCHWARTZ study in detail two sets of doublets, from 1974 and 1975, and then reloeate 85 underthrusting events in the area. The authors find that few smaller magnitude events overlap asperity regions, and that the majority of small magnitude underthrusting earth­ quak es oeeupy a segment that has never experieneed a magnitude greater than 7.0 earthquake in the historie times. It will be of great value to soeiety when seismologists and geophysieists are able to monitor and prediet the pattern of geophysieal phenomena assoeiated with subduetion; this issue presents a modest step towards this goal. PAGEOPH, Vol. 140, No. 2 (1993) 0033 ~4553;93;020 183 ~ 28$1.50 + 0.20;0 © 1993 Birkhäuser Verlag, Basel Slip Partitioning along Major Convergent Plate Boundaries 2 GUANG YU,l STEVEN G. WESNOUSKY,l and GÖRAN EKSTRÖM Abstract-Along plate boundaries characterized by oblique convergence, earthquake slip vectors are commonly rotated toward the normal of the trench with respect to predicted plate motion vectors. Consequently, relative plate motion along such convergent margins must be partitioned between displacements along the thrust plate interface and deformation within the foreare and back-are regions.
    Pages: Online-Ressource (V, 224 Seiten)
    ISBN: 9783034858465
    Language: English
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  • 4
    Description / Table of Contents: The 1957 great Aleutian earthquake.- The rupture process and tectonic implications of the great 1964 Prince William Sound earthquake.- Coseismic slip in the 1964 Prince William Sound earthquake A new geodetic inversion.- Seismicity trends and potential for large earthquakes in the Alaska-Aleutian region.- Rupture process of large earthquakes in the northern Mexico subduction zone.- Global variability in subduction thrust zone-forearc systems.- Large thrust earthquakes and volcanic eruptions.
    Pages: Online-Ressource (VI, 237 Seiten)
    ISBN: 9783034858465
    Language: English
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  • 5
    Unknown
    Basel, Boston, Berlin : Birkhäuser
    Keywords: geophysics ; seismology
    Description / Table of Contents: Earthquakes in shallow subduction zones account for the greatest part of seismic energy release in the Earth and often cause significant damage; in some cases they are accompanied by devastating tsunamis. Understanding the physics of seismogenic and tsunamigenic processes in such zones continues to be a challenging focus of ongoing research. The seismologic and geodetic work reported in this volume highlights the recent advances made toward quantifying and understandig the role of shallow plate coupling in the earthquake generation process. The relation between regional seismotectonics, features in the downgoing plate, and the slip distribution in earthquakes are examined for recent and great historical events. In addition to papers reporting new results, review articles on tsunami and tsunamigenic earthquakes and depth dependent plate interface properties are presented. These observational results, along with complementary laboratory and theoretical studies, can assist in assessing the seismic potential of a given region.
    Pages: Online-Ressource (372 Seiten)
    ISBN: 9783764361464
    Language: English
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  • 6
    facet.materialart.
    Unknown
    In:  J. Geophys. Res., Helsinki, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 108, no. B5, pp. ESE 13-1 to ESE 13-21, pp. 2265, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 2003
    Keywords: Stress ; Fracture ; Fault zone ; JGR
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  • 7
    Publication Date: 2011-10-22
    Description: Material juxtapositions across mature faults are a common occurrence. Previous work has found that this elastic mismatch results in a rupture that will preferentially propagate in the direction of slip displacement on the more compliant side of the fault, with more off-fault damage in the stiffer material. This result has implications for inferring preferred rupture directions based on observations of damage zone asymmetry. We perform a complete numerical investigation of the role of the stress state on the distribution of plastic deformation and the direction of preferred rupture propagation. We show that there are important factors, in addition to the elastic mismatch, which control the preferred direction of propagation as well as the side of the fault in which damage predominately accumulates. The orientation of the most compressive principal stress is the controlling factor in determining the location of plastic deformation. For different orientations, plastic deformation can accumulate in either the stiffer or the more compliant material. For high angles of most compressive stress, the aforementioned preferred rupture direction prediction holds true. However, the off-fault plastic response can reverse that direction for low angles of most compressive stress so that rupture will preferentially propagate in the direction of slip displacement in the stiffer material.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 8
    Publication Date: 2011-07-26
    Description: Material contrasts across faults are a common occurrence, and it is important to understand if these material contrasts can influence the path of rupture propagation. Here we examine models, solved numerically, of rupture propagation through one type of geometric complexity, that of a fault branch stemming from a planar main fault on which rupture initiates. This geometry, with a material contrast across the main fault, could be representative of either a mature strike-slip fault or a subduction zone interface. We consider branches in both the compressional and extensional quadrants of the fault, and material configurations in which the branch fault is in either the stiffer or the more compliant material as well as configurations with no material contrast. We find that there are regimes in which this elastic contrast can influence the rupture behavior at a branching junction, but there are also stress states for which the branch activation will not depend on the orientation of the mismatch. For the scenarios presented here, both compressional and extensional side branches are more likely to rupture if the branch is on the side of the fault with the more compliant material versus the stiffer material. The stresses induced on the branch fault, by rupture traveling on the main fault, are different for the two orientations of material contrast. We show how the interactions between rupture on the two faults determine which faults are activated.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 149 (1997), S. 1-2 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Surveys in geophysics 3 (1977), S. 157-174 
    ISSN: 1573-0956
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This article reviews the field, laboratory, and theoretical investigations made concerning different electromechanical phenomena associated with earthquakes. It discusses laboratory measurements of electrical resistivity of rocks stressed up to fracture, particular attention being paid to the interpretation of results according to the diffusion-dilatancy theory. This is followed by the discussion of field measurements of electrical characteristics of rocks in seismic areas in connections with seismic activity in these regions. Piezoelectric and electrostrictive phenomena are briefly discussed, and also a theoretical model of electro-elastic effects associated with an earthquake source. The last part concerns electrokinetic phenomena in porous rocks, caused by the diffusion of fluids into the dilatant focal region. The divergence of opinion about the physical models of the earthquake process is emphasized.
    Type of Medium: Electronic Resource
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