An earthquake mechanism based on rapid sealing of faults
暂无分享,去创建一个
[1] A. Nur,et al. DESTRUCTION OF POROSITY THROUGH PRESSURE SOLUTION , 1977 .
[2] J. Behrmann. Conditions for hydrofracture and the fluid permeability of accretionary wedges , 1991 .
[3] D. Lockner,et al. Fault stability inferred from granite sliding experiments at hydrothermal conditions , 1991 .
[4] John G. Ramsay,et al. The crack–seal mechanism of rock deformation , 1980, Nature.
[5] S. Kirby. Localized polymorphic phase transformations in high‐pressure faults and applications to the physical mechanism of deep earthquakes , 1987 .
[6] R. Jeanloz,et al. Deep-Focus Earthquakes and Recycling of Water into the Earth's Mantle , 1991, Science.
[7] J. Byerlee,et al. Experimental studies of compaction and dilatancy during frictional sliding on faults containing gouge , 1989 .
[8] D. Turcotte,et al. Pressure solution lithification as a mechanism for the stick‐slip behavior of faults , 1982 .
[9] Robert O. Foumier. The transition from hydrostatic to greater than hydrostatic fluid pressure in presently active continental hydrothermal systems in crystalline rock , 1991 .
[10] M. Zoback,et al. New Evidence on the State of Stress of the San Andreas Fault System , 1987, Science.
[11] J. Holloway,et al. Thermodynamic properties of water to 1,000 C and 10,000 bars , 1969 .
[12] J. B. Walsh,et al. Permeability of granite under high pressure , 1968 .
[13] Frederick M. Chester,et al. Implications for mechanical properties of brittle faults from observations of the Punchbowl fault zone, California , 1986 .
[14] D. Lockner,et al. Effects of temperature and sliding rate on frictional strength of granite , 1986 .
[15] W. Power,et al. The relationship between slickenside surfaces in fine-grained quartz and the seismic cycle , 1989 .
[16] A. Lachenbruch,et al. Frictional heating, fluid pressure, and the resistance to fault motion , 1980 .
[17] C. Frohlich,et al. The Nature of Deep-Focus Earthquakes , 1989 .
[18] Alan G. Jones,et al. Resistivity cross section through the Juan de Fuca Subduction System and its tectonic implications , 1989 .
[19] D. Moore,et al. PERMEABILITY CHANGES IN CRYSTALLINE ROCKS DUE TO TEMPERATURE: EFFECTS OF MINERAL ASSEMBLAGE. , 1984 .
[20] D. E. Powley. Pressures and hydrogeology in petroleum basins , 1990 .
[21] D. Prior,et al. Faulting associated with the olivine to spinel transformation in Mg2GeO4 and its implications for deep‐focus earthquakes , 1991 .
[22] David L. Smith,et al. Diffusional crack healing in quartz , 1984 .
[23] James D. Byerlee,et al. Friction, overpressure and fault normal compression , 1990 .
[24] François Robert,et al. High-angle reverse faults, fluid-pressure cycling, and mesothermal gold-quartz deposits , 1988 .
[25] Amos Nur,et al. Porosity reduction and crustal pore pressure development , 1984 .
[26] Richard H. Sibson,et al. Interactions between Temperature and Pore-Fluid Pressure during Earthquake Faulting and a Mechanism for Partial or Total Stress Relief , 1973 .
[27] M. Paterson,et al. Experimental dissolution‐precipitation creep in quartz aggregates at high temperatures , 1991 .
[28] J. B. Walsh. Stiffness in faulting and in friction experiments , 1971 .
[29] S. Hickman,et al. Healing of microcracks in quartz: Implications for fluid flow , 1990 .
[30] J. Byerlee,et al. Permeability changes during the flow of water through westerly granite at temperatures of 100°–400°C , 1978 .
[31] Chris Marone,et al. The depth of seismic faulting and the upper transition from stable to unstable slip regimes , 1988 .
[32] James R. Rice,et al. Chapter 20 Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault , 1992 .