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  • PANGAEA  (3)
  • Wiley  (2)
  • London [u.a.] : Academic Press  (1)
  • 1
    Signatur: 5/M 95.0219 ; 5/M 92.0622
    In: International geophysics series
    Materialart: Monographie ausleihbar
    Seiten: xxiii, 524 S.
    ISBN: 0-12-243780-2
    Serie: International geophysics series 51
    Klassifikation:
    Tektonik
    Sprache: Englisch
    Anmerkung: Contents: Contributors. - Introduction: William F. Brace. - The Brace Symposium and this Volume. - Bibliography: William F. Brace. - Acknowledgments. - BRITTLE FAILURE OF ROCKS. - 1 Observations of Quasistatic Fault Growth from Acoustic Emissions / D.A. Lockner, J.D. Byerlee, V. Kuksenko, A. Ponomarev, A. Sidorin. - 2 Fabrics of Experimental Fault Zones: Their Development and Relationship to Mechanical Behavior / J.M. Logan, C.A. Dengo, N.G. Higgs, Z.Z. Wang. - 3 Frictional Strength and the Effective Pressure Law of Montmorillonite and lllite Clays / C. Morrow, B. Radney, J. Byerlee. - 4 The Brittle-Ductile Transition in Feldspar Aggregates: An Experimental Study / J. Tullis, R. Yund. - 5 Stabilization of Faulting by Cumulative Slip / Teng-fong Wong, Yaojun Gu, Takashi Yanagidani, Yusheng Zhao. - PERMEABILITY AND FLUID FLOW IN ROCKS. - 6 On the Measurement of Permeability in Anisotropic Rocks / Yves Bernabé. - 7 Permeability and Relative Permeability in Rocks / Stephen C. Blair, James G. Berryman. - 8 The Determination of Permeability and Storage Capacity: Pore Pressure Oscillation Method / G.J. Fischer. - 9 Measurement of Permeability and Storage Capacity in Rocks During Deformation at High Temperature and Pressure / G.J. Fischer, M.S. Paterson. - 10 Growth of Grain Contacts in Halite by Solution-transfer: Implications for Diagenesis, Lithification, and Strength Recovery / Stephen H. Hickman, Brian Evans. - 11 The Influence of H2O and CO2 on Melt Migration in Two Silicate Liquid-Olivine Systems / G.N. Riley Jr., D.L. Kohlstedt. - FRACTURE CHARACTERIZATION AND PHYSICAL PROPERTIES OF ROCK. - 12 Fluid-driven Cyclic Propagation of a Joint in the Ithaca Siltstone, Appalachian Basin, New York / Alfred Lacazette, Terry Engelder. - 13 The Influence of Hydrostatic and Uniaxial Stress on Remanent Magnetization / Randolph J. Martin. - 14 The Correlation between Fracture-toughness Anisotropy and Crack-surface Morphology of Siltstones in the Ithaca Formation, Appalachian Basin / Paul A. Scott, Terry Engelder, John J. Mecholsky Jr. - 15 CT Imaging of Electrical Resistivity Measurements: Nonuniform Water Saturation Can Be a Problem / Eve S. Sprunt. - 16 Fracture Detection and Characterization from Hydrophone Vertical Seismic Profiling Data / M.N. Toksöz, C.H. Cheng, R.D. Cicerone. - IMPLICATIONS OF ROCK MECHANICS ON CRUSTAL TECTONICS. - 17 Role of Elastic Stiffness and Fault Damping during Thrust-sheet Emplacement in a Foreland Belt / E.G. Bombolakis. - 18 Brace-Goetze Strength Profiles, The Partitioning of Strike-slip and Thrust Faulting at Zones of Oblique Convergence, and the Stress-Heat Flow Paradox of the San Andreas Fault / Peter Molnar. - 19 Hydraulic Pulses in the Earth's Crust / Amos Nor, Joseph Walder. - 20 Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault / James R. Rice. - 21 Paradigms or Small Change in Earthquake Mechanics / C.H. Scholz. - Index.
    Standort: Lesesaal
    Standort: Lesesaal
    Zweigbibliothek: GFZ Bibliothek
    Zweigbibliothek: GFZ Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Meng, Fanbao; Baud, Patrick; Ge, Hongkui; Wong, Teng-fong (2019): The Effect of Stress on Limestone Permeability and Effective Stress Behavior of Damaged Samples. Journal of Geophysical Research: Solid Earth, 124(1), 376-399, https://doi.org/10.1029/2018JB016526
    Publikationsdatum: 2023-01-13
    Beschreibung: The evolution of permeability and its effective stress behavior is related to inelastic deformation and failure mode. This was systematically investigated in Indiana and Purbeck limestones with porosities of 16% and 14%, respectively. High‐pressure compression tests were conducted at room temperature on water‐saturated samples. At relatively high confinement shear‐enhanced compaction was observed to initiate at a critical stress, accompanied by significant permeability reduction of up to a factor of ~3. Overall, the permeability reduction due to inelastic compaction in our limestones is smaller than that observed in sandstones. At relatively low confinement, dilatant failure was observed, which was accompanied by a decrease and increase of permeability in Indiana and Purbeck limestones, respectively. There seems to be a trend for the correlation between porosity and permeability changes to switch from positive to negative with increasing porosity. The void space of both limestones has significant proportions of macropores and micropores. The effective stress behavior of such a limestone with dual porosity has been documented to be different from the prediction for a microscopically homogeneous assemblage, in that its effective stress coefficients for permeability and pore volume change may attain values significantly 〉1. In contrast, our investigation of damaged samples consistently showed effective stress coefficients for both permeability and pore volume change with values 〈1. This suggests that the behavior in the damaged samples is akin to that of a microscopically homogeneous assemblage, possibly due to pervasive collapse of macropores that would effectively homogenize the initially bimodal pore size distribution.
    Materialart: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 5.4 MBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-01-13
    Materialart: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 56 kBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-04-20
    Beschreibung: The samples are cylinders of Adamswiller and Rothbach sandstones of nominal length 80 mm and diameter 40 mm. The average porosities for our Adamswiller and Rothbach sandstone samples are 25.8% and 24.3%, respectively. The permeability and strain were measured under hydrostatic loading.
    Schlagwort(e): clay; confining pressure; fluid flow; mechanical anisotropy; pore pressure; pore volume
    Materialart: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 150.5 kBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2004-12-01
    Print ISSN: 0017-467X
    Digitale ISSN: 1745-6584
    Thema: Energietechnik , Geologie und Paläontologie
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2001-11-01
    Print ISSN: 0017-467X
    Digitale ISSN: 1745-6584
    Thema: Energietechnik , Geologie und Paläontologie
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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