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  • Fracture  (4)
  • Earthquake precursor: prediction research  (3)
  • Friction  (2)
  • 1
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    Unbekannt
    Strike slip faulting in a downward varying crust (1979)
    In:  J. Geophys. Res., San Francisco, Pergamon, vol. 84, no. 1-2, pp. 2296-2302, pp. 1447, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1979
    Schlagwort(e): Dislocation ; Earthquake precursor: prediction research ; JGR ; FROTH ; (abstract)
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 2
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    Unbekannt
    Earthquakes as a coupled shear stress-high pore pressure dynamical system (1996)
    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 23, no. 5564, pp. 197-200, pp. L24308, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1996
    Schlagwort(e): Stress ; Fluids ; Rock mechanics ; Earthquake ; Friction ; GRL
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 3
    facet.materialart.
    Unbekannt
    A complete solution of a one-dimensional propagating fault with nonuniform stress and strength (1979)
    In:  J. Geophys. Res., Amsterdam, Schweizerbart'sche Verlagsbuchhandlung, vol. 84, no. 44, pp. 2223-2234, pp. L12S09, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publikationsdatum: 1979
    Schlagwort(e): Fault zone ; Elasticity ; Inhomogeneity ; Dislocation ; Stress ; Fracture ; JGR
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 4
    facet.materialart.
    Unbekannt
    Elastic strain energy as a control in the evolution of asymmetric pressure-solution contacts (1998)
    In:  Geology, Warszawa, Pergamon, vol. 26, no. 7, pp. 663-665, pp. L11614, (ISBN: 0534351875, 2nd edition)
    Details
    Publikationsdatum: 1998
    Beschreibung: Subjecting a water-rock system to load can enhance the rock solubility by (1) increasing normal pressure at the dissolving surface and (2) raising the elastic energy of the rock. For pressure-solution surfaces such as grain contacts, solution seams, and stylolites, the pressure term in the chemical potential equation is orders of magnitude larger than the strain-energy term. Thus, the contribution of the strain energy to the overall solubility of the system is very small, and it is most often ignored. We show that the elastic strain energy at a pressure-solution interface can have a profound effect on the manner in which it evolves. The mechanism we propose is the following: inducing a discontinuity in elastic strain energy across a pressure-solution interface (e.g., by changing its curvature) can cause one side to become slightly more soluble than the other. Part of the material that is dissolved may diffuse the short distance across the fluid layer and raise the saturation in the vicinity of the less-soluble surface. If the fluid layer was already close to saturation, the dissolution at the less-soluble surface may be severely slowed down or even halted. Therefore, although the strain-energy difference across the interface has a negligible effect on the total amount of material that is dissolved there, it may cause only one side to dissolve. In this way, the formation of stylolites can be facilitated by heterogeneities in the elastic strain-energy difference along a pressure-solution interface.
    Schlagwort(e): Fracture ; Fluids ; STRArtificial intelligence (AI) ; Rock mechanics
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 5
    facet.materialart.
    Unbekannt
    Role of pore fluids in faulting (1973)
    In:  Phil. Trans. R. Soc. London, Dordrecht, Martinus Nijhoff Publishers, vol. 274, no. 3, pp. 297-304, pp. L11307, (ISSN: 1340-4202)
    Details
    Publikationsdatum: 1973
    Schlagwort(e): Fluids ; Rock mechanics ; Fracture ; Hydraulic fracturing ; PTRS ; in-situ ; Creep observations and analysis ; Aftershocks ; Dual Induction Latero logAT ; SAF ; Garm ; Laboratory measurements
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 6
    facet.materialart.
    Unbekannt
    A search for tectonomagnetic effects in California and western Nevada (1973)
    Stanford University Press
    In:  Bull., Polar Proj. OP-O3A4, Proceedings of Conference on Tectonic Problems of the San Andreas Fault System, Rotterdam, Stanford University Press, vol. 14, no. 16, pp. 225-239, (ISBN: 3-540-23712-7)
    Details
    Publikationsdatum: 1973
    Schlagwort(e): Geomagnetics ; Earthquake precursor: prediction research ; Earthquake precursor: magnetic ; Tectonics
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 7
    facet.materialart.
    Unbekannt
    Water, pore pressure, and seismic velocities in the crust and its fault zones (1997)
    Conseil de l'Europe
    In:  Bull., Polar Proj. OP-O3A4, Short Term Thermal and Hydrological Signatures Related to Tectonic Avtivities, Luxembourg, Conseil de l'Europe, vol. 14, no. Subvol. a, pp. 1-20, (ISBN 0080419208)
    Details
    Publikationsdatum: 1997
    Schlagwort(e): Fault zone ; Fluids ; Velocity ; Stress ; Friction ; Fracture ; Tectonics ; Ruymbeke
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 8
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    Unbekannt
    Depth constraints on dilatancy induced velocity anomalies (1978)
    Center for Akad. Publ. Japan
    In:  Professional Paper, Open-File Rept., Earthquake Precursors, Tokyo, Center for Akad. Publ. Japan, vol. 22, no. 16, pp. 231-241, (ISBN 0080419208)
    Details
    Publikationsdatum: 1978
    Schlagwort(e): Earthquake precursor: prediction research ; Dual Induction Latero logAT ; Earthquake precursor: Vp/Vs anomalies ; Hypocentral depth
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
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