Microscale cavitation as a mechanism for nucleating earthquakes at the base of the seismogenic zone
暂无分享,去创建一个
[1] T. Shimamoto,et al. Mechanical Behavior of Halite and Calcite Shear Zones from Brittle to Fully-Plastic Deformation and A Revised Fault Model , 2018 .
[2] T. Mitchell,et al. The effect of water on strain localization in calcite fault gouge sheared at seismic slip rates , 2017 .
[3] Kelin Wang,et al. Rheological separation of the megathrust seismogenic zone and episodic tremor and slip , 2017, Nature.
[4] C. Spiers,et al. Shear localization in a mature mylonitic rock analog during fast slip , 2017 .
[5] A. Niemeijer,et al. Friction properties and deformation mechanisms of halite(-mica) gouges from low to high sliding velocities , 2017 .
[6] Jianye Chen,et al. Rate and state frictional and healing behavior of carbonate fault gouge explained using microphysical model , 2016 .
[7] R. Clayton,et al. Localized seismic deformation in the upper mantle revealed by dense seismic arrays , 2016, Science.
[8] Lei Zhang,et al. Frictional properties of phyllosilicate‐rich mylonite and conditions for the brittle‐ductile transition , 2015 .
[9] A. Niemeijer,et al. Mechanical behavior and microstructure of simulated calcite fault gouge sheared at 20–600°C: Implications for natural faults in limestones , 2015 .
[10] T. Mitchell,et al. Crystallographic preferred orientations may develop in nanocrystalline materials on fault planes due to surface energy interactions , 2015 .
[11] Jianye Chen,et al. Interseismic re-strengthening and stabilization of carbonate faults by "non-Dieterich" healing under hydrothermal conditions , 2015 .
[12] Steven A. Smith,et al. Strain localization and the onset of dynamic weakening in calcite fault gouge , 2015 .
[13] C. Spiers,et al. Superplastic nanofibrous slip zones control seismogenic fault friction , 2014, Science.
[14] H. Noda,et al. A friction to flow constitutive law and its application to a 2‐D modeling of earthquakes , 2014 .
[15] A. Niemeijer,et al. Frictional Properties and Microstructure of Calcite-Rich Fault Gouges Sheared at Sub-Seismic Sliding Velocities , 2014, Pure and Applied Geophysics.
[16] Xianghui Xiao,et al. Creep cavitation bands control porosity and fluid flow in lower crustal shear zones , 2014 .
[17] C. Spiers,et al. Influence of subduction zone conditions and gouge composition on frictional slip stability of megathrust faults , 2013 .
[18] C. Spiers,et al. A microphysical model for fault gouge friction applied to subduction megathrusts , 2013 .
[19] Y. Fialko,et al. Temperature dependence of frictional healing of Westerly granite: Experimental observations and numerical simulations , 2013 .
[20] J. White. Paradoxical pseudotachylyte – Fault melt outside the seismogenic zone , 2012 .
[21] D. Kohlstedt,et al. Grain boundary sliding in San Carlos olivine: Flow law parameters and crystallographic‐preferred orientation , 2011 .
[22] M. Cocco,et al. Fault lubrication during earthquakes , 2011, Nature.
[23] T. Tullis,et al. Porosity and particle shape changes leading to shear localization in small-displacement faults , 2010 .
[24] H. Noda,et al. A rate‐ and state‐dependent ductile flow law of polycrystalline halite under large shear strain and implications for transition to brittle deformation , 2010 .
[25] F. De Carlo,et al. Creep cavitation can establish a dynamic granular fluid pump in ductile shear zones , 2009, Nature.
[26] G. D. Toro,et al. Mantle earthquakes frozen in mylonitized ultramafic pseudotachylytes of spinel-lherzolite facies. , 2008 .
[27] Erik Rybacki,et al. High‐strain creep of feldspar rocks: Implications for cavitation and ductile failure in the lower crust , 2008 .
[28] A. Niemeijer,et al. A microphysical model for strong velocity weakening in phyllosilicate‐bearing fault gouges , 2006 .
[29] A. Niemeijer,et al. Velocity dependence of strength and healing behaviour in simulated phyllosilicate-bearing fault gouge , 2006 .
[30] J. Rice. Heating and weakening of faults during earthquake slip , 2006 .
[31] Review and Future Directions , 2006, In Search of Consistency: Ethics and Animals.
[32] Wenxiong Huang,et al. A study of localized deformation pattern in granular media , 2004 .
[33] K. Fujimoto,et al. Ductile fracture of fine-grained plagioclase in the brittle–plastic transition regime: implication for earthquake source nucleation , 2004 .
[34] B. Evans,et al. The effect of dissolved magnesium on diffusion creep in calcite , 2003 .
[35] Nadia Lapusta,et al. Nucleation and early seismic propagation of small and large events in a crustal earthquake model , 2003 .
[36] J. D. Bresser. On the mechanism of dislocation creep of calcite at high temperature: Inferences from experimentally measured pressure sensitivity and strain rate sensitivity of flow stress , 2002 .
[37] C. Spiers,et al. Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles , 2002 .
[38] B. Evans,et al. A few remarks on the kinetics of static grain growth in rocks , 2001 .
[39] N. Shigematsu,et al. Ultramylonite bands derived from cataclasite and pseudotachylyte in granites, northeast Japan , 2000 .
[40] Kiyoshi Ito,et al. Seismogenic layer, reflective lower crust, surface heat flow and large inland earthquakes , 1999 .
[41] M. Handy,et al. Frictional–viscous flow in mylonite with varied bimineralic composition and its effect on lithospheric strength , 1999 .
[42] T. Shimamoto,et al. The strength profile for bimineralic shear zones: an insight from high-temperature shearing experiments on calcite–halite mixtures , 1998 .
[43] C. Scholz. Earthquakes and friction laws , 1998, Nature.
[44] T. Fliervoet,et al. Evidence for dominant grain-boundary sliding deformation in greenschist- and amphibolite-grade polymineralic ultramylonites from the Redbank Deformed Zone, Central Australia , 1997 .
[45] S. Covey-crump. The normal grain growth behaviour of nominally pure calcitic aggregates , 1997 .
[46] F. Chester. A rheologic model for wet crust applied to strike‐slip faults , 1995 .
[47] James D. Byerlee,et al. Frictional slip of granite at hydrothermal conditions , 1995 .
[48] Brian Kilgore,et al. Scaling of the critical slip distance for seismic faulting with shear strain in fault zones , 1993, Nature.
[49] J. Weeks,et al. Two‐mechanism model for frictional sliding of serpentinite , 1992 .
[50] Frederick M. Chester,et al. Multimechanism friction constitutive model for ultrafine quartz gouge at hypocentral conditions , 1992 .
[51] 김기석. 악관절 장애의 기여요인(Contributing Factors) , 1991 .
[52] Christopher H. Scholz,et al. The brittle-plastic transition and the depth of seismic faulting , 1988 .
[53] T. Shimamoto. Transition Between Frictional Slip and Ductile Flow for Halite Shear Zones at Room Temperature , 1986, Science.
[54] R. Sibson. Roughness at the base of the seismogenic zone: Contributing factors , 1984 .
[55] R. Sibson. Continental fault structure and the shallow earthquake source , 1983, Journal of the Geological Society.
[56] A. Ruina,et al. Stability of Steady Frictional Slipping , 1983 .
[57] R. Sibson. Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United States , 1982 .
[58] Richard H. Sibson,et al. Fault rocks and fault mechanisms , 1977, Journal of the Geological Society.
[59] S. D. Hartog,et al. Subduction megathrust creep governed by pressure solution and frictional-viscous flow , 2017 .
[60] C. Collettini,et al. Frictional-viscous flow, seismicity and the geology of weak faults: a review and future directions , 2008 .
[61] B. Evans,et al. On estimating the strength of calcite rocks under natural conditions , 2002, Geological Society, London, Special Publications.
[62] M. Stewart,et al. The structure and rheological evolution of reactivated continental fault zones: a review and case study , 2001, Geological Society, London, Special Publications.
[63] E. Rutter,et al. Experimental study of grain-size sensitive flow of synthetic, hot-pressed calcite rocks , 1990, Geological Society, London, Special Publications.
[64] T. Shimamoto. The origin of S-C mylonites and a new fault-zone model , 1989 .
[65] B. Hobbs,et al. Earthquakes in the ductile regime? , 1986 .
[66] R. Sibson. Transient discontinuities in ductile shear zones , 1980 .