The brittle-plastic transition and the depth of seismic faulting

Geologische Rundschau

Volumn 77, Issue 1, 1988, Pages 319-328

  Scholz, C H ^a  

^a Department of Earth and Environmental Sciences   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 34250090620     PISSN: 00167853     EISSN: 14373262     Source Type: Journal    
DOI: 10.1007/BF01848693     Document Type: Article

References (49)

1. Cataclastic rocks of the San Gabriel fault — an expression of deformation at deeper crustal levels in the San Andreas fault zone
2. Limits on lithospheric stress imposed by laboratory experiments
3. Friction of rocks
4. Transient creep and semibrittle behavior of crystalline rocks
5. Appropriate boundary conditions for modeling very long earthquakes and physical consequences
6. Why large earthquakes do not nucleate at shallow depths
7. Time dependent friction and the mechanics of stick-slip
8. Depth of seismicity in the Imperial Valley region (1977–1983) and its relationship to heat flow, crustal structure, and the October 15, 1979 earthquake
9. Volume changes during the deformation of rocks at high pressures
10. High fluid pressures during regional metamorphism: implication for mass transport and deformation mechanisms
11. Interpretation of seismic reflection profiling data for the structure of the San Andreas fault zone
12. Earthquakes in the Ductile Regime?
13. Fluid infiltration into fault zones: chemical, isotopic, and mechanical effects
14. The transition between deformation regimes dominated by intercrystalline diffusion and intracrystalline creep evaluated by oxygen isotope thermometry
15. Tectonic stress in the lithosphere: constraints provided by the experimental deformation of rocks
16. Rheology of the lithosphere
17. S-C mylonites
18. Problems and progress on the Geologico-seismological frontier
19. Limits of stress in continental crust and their relation to the depth-frequency relation of shallow earthquakes
20. The generation of ductile and brittle deformation bands in a low-angle mylonite zone
21. Slip instability and state variable friction laws
22. On the nomenclature of mode of failure transitions in rocks
23. Microfracturing and the inelastic deformation of rock in compression
24. A discussion on the state of stress on faults
25. Wear and gouge formation in brittle faulting
26. role of asperity indentation and ploughing in rock friction, 1: asperity creep and stickslip
27. Fault rocks and fault mechanisms
28. Transient discontinuities in ductile shear zones
29. Fault zone models, heat flow, and the depth distribution of seismicity in the continental curst of the United States
30. Roughness at the base of the seismogenic zone: contributing factors
31. A transition between frictional slip and ductile flow undergoing large shearing deformation at room temperature
32. Intraplate extensional tectonics of the eastern Basin-Range: inferences on structural style from seismic reflection data, regional tectonics and thermal-mechanical models of brittle-ductile deformation
33. Crystal growth in cataclastites: diagnostic microstructures and implications
34. The effect of cyclic operation of brittle and ductile deformation on the metamorphic assemblage in cataclastites and mylonites
35. The mechanical behavior of faulted rock at high temperature and pressure
36. Mechanisms of high temperature frictional sliding in Westerly granite
37. Strain accumulation and release mechanism of the 1906 San Francisco earthquake
38. Crustal earthquake instability in relation to the depth variation of frictional slip properties
39. Experimental deformation of dry Westerly granite
40. Hydrolytic weakening of experimentally deformed Westerly granite and Hale albite rock
41. Recrystallization of quartz, biotite, and feldspars from Erstfeld to the Levantina nappe, Swiss Alps, and its geological implications
42. Al-rich calcic pyroxene in pseudotachylyte: an indicator of high pressure and high temperature?
43. Tectonic deformation and recrystallization of oligoclase