Pressure solution lithification as a mechanism for the stick‐slip behavior of faults

Tectonics

Volumn 1, Issue 2, 1982, Pages 151-160

  Angevine, C L ^a   Turcotte, D L ^a   Furnish, M D ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84982683408     PISSN: 02787407     EISSN: 19449194     Source Type: Journal    
DOI: 10.1029/TC001i002p00151     Document Type: Article

References (40)

1. Stick‐slip as a mechanism for earthquakes
2. Heat flow, stress, and rate of slip along the San Andreas Fault, California
3. Friction of rocks
4. Structures developed in fault gouge during stable sliding and stick‐slip
5. Deformation of porous aggregates of calcite and quartz using the isostatic hot‐pressuring technique
6. Pressure solution: Theory and experiments
7. Time‐dependent friction in rocks
8. Time‐dependent friction as a possible mechanism for aftershocks
9. Time‐dependent friction and the mechanics of stick‐slip
10. Pressure‐solution and crystallization deformation
11. Incremental strains measured by syntectonic crystal growths
12. The energy balance and deformation mechanisms of thrust sheets
13. A natural example of the simultaneous operation of free‐face dissolution and pressure solution (abstract)
14. The role of asperity indentation and ploughing in rock friction, II, Influence of relative hardness and normal load
15. The sliding characteristics of sandstone on quartz fault‐gouge
16. Quantitative theory for metamorphic differentiation in development of crenulation cleavage
17. Experimental study of sandstone cementation
18. Heat flow near major strike‐slip faults in California
19. Frictional properties of ultrafine quartz in upper‐crustal earthquake environments (abstract)
20. Frictional heating, fluid pressure, and the resistance to fault motion
21. Heat flow and energetics of the San Andreas fault zone
22. Consolidation and rebound processes in one‐dimensional porous columns
23. Pressure solution at grain‐to‐grain contacts
24. The kinetics of rock deformation by pressure solution
25. On the possibility of slow fault slip controlled by a diffusive mass transfer process
26. The role of asperity indentation and ploughing in rock friction, I, Asperity creep and stick‐slip
27. Detailed studies of fractional sliding of granite and implications for the earthquake mechanism
28. Energy transport in thick sequences of compacting sediment
29. Effects of simulated fault gouge on the sliding behavior of Tennessee sandstone: Nonclay gouges
30. Silica solubility, 0°–200°C, and the diagenesis of siliceous sediments
31. Viscoelastic relaxation of cyclic displacements on the San Andreas Fault
32. Destruction of porosity through pressure solution
33. Earthquake instability on a strike‐slip fault
34. Localization of deformation along faults: Implications to fault zone permeability (abstract)
35. Effect of shortening rate on the real area of contact and temperatures generated during frictional sliding
36. Stress accumulation and release on the San Andreas fault
37. A steady state model for the distribution of stress and temperature on the San Andreas fault
38. Pressure solution and the force of crystallization‐A phenomenological theory