Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles

Journal of Geophysical Research: Solid Earth

Volumn 107, Issue 2, 2002, Pages

  Bos, Bart ^a   Spiers, Christopher J ^a  

^a TNO   (Netherlands)

Author keywords

[No Author keywords available]

Indexed keywords

CRUSTAL DEFORMATION; FAULT; FRICTION; SHEAR STRENGTH; VISCOUS FLOW;

EID: 0036105578     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: None     Document Type: Article

References (67)

1. Silica transport during steam injection into oil sands, 1, dissolution and precipitation kinetics of quartz: New results and review of existing data
2. Pressure solution, phyllosilicates, and the strength of mature faults
3. Effect of phyllosilicates on fluid-assisted healing of gouge-bearing faults
4. Experimental investigation into the microstructural and mechanical evolution of phyllosilicate-bearing fault rock under conditions favouring pressure solution
5. Frictional-viscous flow of simulated fault gouge caused by the combined effects of phyllosilicates and pressure solution
6. Friction of rocks
7. A rheologic model for wet crust applied to strike-slip faults
8. Multimechanism friction constitutive model for ultrafine quartz gouge at hypocentral conditions
9. Uniaxial compaction creep of wet gypsum aggregates
10. Measurement of oxygen grain boundary diffusion in natural, fine grained, quartz aggregates
11. An equation correlating the solubility of quartz in water from 25° to 900°C at pressure up to 10,000 bars
12. Stress and temperature in the bending lithosphere as constrained by experimental rock mechanics
13. Extension of stable continental lithosphere and the initiation of lithosphere scale faults
14. Experimental pressure solution-deposition on quartz grains: The crucial effect of the nature of the fluid
15. Fractures and pressure solution in natural single-layer folds
16. The solid state flow of polymineralic rock
17. Frictional-viscous flow in mylonite with varied binimeralic composition and its effect on lithospheric strength
18. Introduction to special section: Mechanical involvement of fluids in faulting
19. Kinetics of pressure solution at halite-silica interfaces and intergranular clay films
20. Fault-zone weakening processes along the reactivated Outer Hebrides Fault Zone, Scotland
21. Adhesion forces between surfaces in liquids and condensable vapours
22. The strength profile for bimineralic shear zones: An insight from high-temperature shearing experiments on calcite-halite mixtures
23. Strength of the lithosphere: Constraints imposed by laboratory experiments
24. Basal slip and mechanical anisotropy of biotite
25. Heat flow and energetics of the San Andreas fault zone
26. Heat flow from Cajon Pass, fault strength, and tectonic implications
27. Thermodynamics of rock deformation by pressure solution
28. Nonequilibrium thermodynamics of pressure solution
29. Preparation and deformation of synthetic aggregates of quartz
30. Experimental deformation of muscovite
31. Pressure solution and Coble creep in rocks and minerals: A review
32. The effect of mineral bond strength and adsorbed water on fault gouge frictional strength
33. Diffusivity of ions in pore water as a quantitative basis for rock deformation rate estimates
34. A theory for granular flow accommodated by material transfer via an intergranular fluid
35. Creep in polycrystalline aggregates by matter transport through a liquid phase
36. On grain boundary sliding and diffusional creep
37. Solution-precipitation creep in glass ceramics
38. Rheology of the lithosphere in space and time
39. The frictional behavior of lizardite and antigorite serpentinites: Experiments, constitutive models, and implications for natural faults
40. Water films at grain-grain contacts: Debye-Hueckel, osmotic model of stress, salinity, and mineralogy dependence
41. Quartz solubility at low temperatures
42. The kinetics of rock deformation by pressure solution
43. The mechanical properties of kaolinite fault "gouge" at moderate confining pressure, 20°C
44. Pressure solution in nature, theory and experiment
45. On the mechanical properties of synthetic kaolinite/quartz fault gouge
46. Comparative microstructures of natural and experimentally produced clay-bearing fault gouges
47. On the possibility of slow fault slip controlled by a diffusive mass transfer process
48. Pressure solution in siliciclastic HP-LT metamorphic rocks: Constraints on the state of stress in deep levels of accretionary complexes
49. Rheology and deformation mechanisms of an isotropic mica schist
50. Strength and anisotropy of foliated rocks with varied mica contents
51. The origin of S-C mylonites and a new fault-zone model
52. Frictional constraints on thrust, wrench and normal faults
53. Fault rocks and fault mechanisms
54. Continental fault structure and the shallow earthquake source
55. Densification behaviour of wet granular salt: Theory versus experiment
56. Densification of crystalline aggregates by fluid phase diffusional creep
57. Experimental determination of constitutive parameters governing creep of rocksalt by pressure solution
58. Deformation processes and weakening mechanisms within the frictional-viscous transition zone of major crustal-scale faults: Insights from the Great Glen Fault Zone, Scotland
59. Low effective viscosity during high pressure metamorphism due to dissolution precipitation creep: The record of HP-LT metamorphic carbonates and siliciclastic rocks from Crete
60. On mylonites in ductile shear zones
61. Fluid-rock reaction weakening of fault zones