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  • GEOPHYSICS  (14)
  • Dislocation  (4)
  • BSSA  (1)
  • Earthquake precursor: models  (1)
  • 1985-1989  (9)
  • 1975-1979  (10)
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  • 1
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    A fractal approach to the clustering of earthquakes: applications to the seismicity of the New Hebrides (1987)
    In:  Bull Seism. Soc. Am., Minsk, Polish Geothermal Association, vol. 77, no. 7045, pp. 1368-1381, pp. 2339, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1987
    Schlagwort(e): Seismicity ; FractureT ; Fault zone ; BSSA
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 2
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    Stress accumulation and release on the San Andreas fault (1977)
    In:  Pageoph, Taipei, EGS, vol. 115, no. 2, pp. 413-427, pp. 8039, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1977
    Schlagwort(e): Fault zone ; Stress ; Geothermics ; Inelastic ; Seismicity ; Dislocation
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 3
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    Viscoelastic relaxation of cyclic displacements on the San Andreas fault (1979)
    In:  Proc. R. Soc. London, Roma, Polish Geothermal Association, vol. 365, no. 2, pp. 121-144, pp. L24301, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1979
    Schlagwort(e): Dislocation ; Recurrence of earthquakes ; Fault zone
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    BIBLIOGRAFIE SEISMOLOGIE
  • 4
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    An elastostatic model of stress accumulation on the San Andreas fault (1976)
    In:  Proc. R. Soc. London, Roma, Polish Geothermal Association, vol. 349, no. 2, pp. 319-341, pp. L24301, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1976
    Schlagwort(e): Fault zone ; Elasticity ; Dislocation
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    BIBLIOGRAFIE SEISMOLOGIE
  • 5
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    Models for the distribution of stress and strain adjacent to the San Andreas fault (1978)
    USGS
    In:  Proc. Conf. III, Fault Mechanics and its Relation to Earthquake Prediction, Nat. Earthq. Hazard Reduction Program, 1-3.12.1977, Los Angeles, USGS, vol. 10, no. 91-N-FA07-7-4, pp. 589-618, (ISBN 0 08 042822 3)
    Details
    Publikationsdatum: 1978
    Schlagwort(e): Fault zone ; Dislocation ; Earthquake precursor: prediction research ; Stress ; Earthquake precursor: deformation or strain ; Earthquake precursor: models ; Review article ; FROTH, ; FRUMMEL
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 6
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    Properties of the lithosphere and asthenosphere deduced from geoid observations (1985)
    In:  CASI
    Details
    Publikationsdatum: 2016-06-07
    Beschreibung: Data from the GEOS-3 and SEASAT Satellites provided a very accurate geoid map over the oceans. Broad bathymetric features in the oceans such as oceanic swells and plateaus are fully compensated. It is shown that the geoid anomalies due to the density structures of the lithosphere are proportional to the first moment of the density distribution. The deepening of the ocean basins is attributed to thermal isostasy. The thickness of the oceanic lithosphere increases with age due to the loss of heat to the sea floor. Bathymetry and the geoid provide constraints on the extent of this heat loss. Offsets in the geoid across major fracture zones can also be used to constrain this problem. Geoid bathymetry correlations show that the Hawaiian and Bermuda swells and the Cape Verde Rise are probably due to lithospheric thinning.
    Schlagwort(e): GEOPHYSICS
    Materialart: NASA, Washington Geopotential Res. Mission (GRM); p 44-45
    Format: application/pdf
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  • 7
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    A renormalization group approach to the stick-slip behavior of faults (1985)
    In:  Other Sources
    Details
    Publikationsdatum: 2019-06-28
    Beschreibung: A fault which is treated as an array of asperities with a perscribed statistical distribution of strengths is described. For a linear array the stress is transferred to a single adjacent asperity and for a two dimensional array to three adjacent asperities. It is shown that the solutions bifurcate at a critical applied stress. At stresses less than the critical stress virtually no asperities fail on a large scale and the fault is locked. At the critical stress the solution bifurcates and asperity failure cascades away from the nucleus of failure. It is found that the stick slip behavior of most faults can be attributed to the distribution of asperities on the fault. The observation of stick slip behavior on faults rather than stable sliding, why the observed level of seismicity on a locked fault is very small, and why the stress on a fault is less than that predicted by a standard value of the coefficient of friction are outlined.
    Schlagwort(e): GEOPHYSICS
    Materialart: Journal of Geophysical Research (ISSN 0148-0227); 90; 1894-190
    Format: text
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  • 8
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    Lithospheric instabilities (1977)
    In:  Other Sources
    Details
    Publikationsdatum: 2019-06-27
    Beschreibung: In this paper we define a mantle geoid. This is the height that hot solid mantle rock from the asthenosphere would attain if it were not confined by the lithosphere. The mantle geoid lies 3.25 km below the hydrogeoid (sea level). Hot mantle rock cannot entirely penetrate the continental lithosphere. One consequence of this partial penetration is rifting; as a result of rifting an accreting plate margin may be created. Hot mantle rock from the asthenosphere can penetrate through the oceanic lithosphere if the sea floor lies below the mantle geoid. Penetration of the oceanic lithosphere by this solid mantle rock is a necessary condition for the initiation of subduction. We argue that the same processes that are associated with rifting in continental lithosphere will be associated with behind arc spreading and the initiation of subduction in the oceanic lithosphere.
    Schlagwort(e): GEOPHYSICS
    Format: text
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  • 9
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    Geoid Anomalies and the Near-Surface Dipole Distribution of Mass (1978)
    In:  CASI
    Details
    Publikationsdatum: 2019-06-27
    Beschreibung: Although geoid or surface gravity anomalies cannot be uniquely related to an interior distribution of mass, they can be related to a surface mass distribution. However, over horizontal distances greater than about 100 km, the condition of isostatic equilibrium above the asthenosphere is a good approximation and the total mass per unit column is zero. Thus the surface distribution of mass is also zero. For this case we show that the surface gravitational potential anomaly can be uniquely related to a surface dipole distribution of mass. Variations in the thickness of the crust and lithosphere can be expected to produce undulations in the geoid.
    Schlagwort(e): GEOPHYSICS
    Materialart: Ohio State Univ. Appl. of Geodesy to Geodyn., an Intern. Symp.; p 257-260
    Format: application/pdf
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  • 10
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    Geoid anomalies and the thickness of the lithosphere (1979)
    In:  Other Sources
    Details
    Publikationsdatum: 2019-06-27
    Beschreibung: By using accepted crustal density distributions and either error function or linear temperature distributions the difference in geoid height between stable continental areas and deep ocean basins has been determined as a function of the continental lithospheric thickness. If the continental lithosphere were greater than 200 km thick, the geoid anomaly over the continents would be systematically negative in relation to that over the ocean basins. By using the GEM 9 satellite geoid the mean geoid anomalies over ocean basins and stable continental areas have been obtained. No systematic difference between continental and oceanic geoids is observed. It is concluded that the thickness of the continental lithosphere is near 180 km. This is in good agreement with various interpretations of the surface heat flow observations.
    Schlagwort(e): GEOPHYSICS
    Materialart: Journal of Geophysical Research; 84; May 10
    Format: text
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