Problems in the extrapolation of laboratory rheological data

Tectonophysics

Volumn 133, Issue 1-2, 1987, Pages 33-43

  Paterson, M S ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION REGIMES; EXPERIMENTAL WORK; RHEOLOGICAL BEHAVIOUR;

EID: 0023088855     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(87)90278-2     Document Type: Article

References (56)

1. Hydrogen speciation in synthetic quartz
2. A universal law for high-temperature diffusion controlled transient creep
3. A first report on deformation-mechanism maps
4. Effect of water on the experimental deformation of olivine
5. Water diffusion in quartz at high pressure; tectonic implications
6. Plasticity and hydrolytic weakening of quartz single crystals
7. Origin of some mylonites by superplastic flow
8. Limits on lithospheric stress imposed by laboratory experiments
9. High temperature flow of dunite and peridotite
10. Transient creep and semi-brittle behaviour of crystalline rocks
11. Creep and creep rupture of granitic rock
12. The experimental deformation of dunite
13. The role of water in the deformation of dunite
14. Plastic deformation of quartz single crystals
15. High fluid pressures during metamorphism and deformation Implications for mass transport and deformation mechanisms
16. Dilatancy and permeability in rock during deformation at high temperature and pressure (abstr.)
17. Improved procedures for diffusing “water” into quartz at high temperatures and pressures (abstr.)
18. Pressure dependence of creep in dry polycrystalline olivine (abstr.)
19. The strength of quartz in the ductile regime (abstr.)
20. Quartz—anomalous weakness of synthetic crystals
21. Effects of large changes in strain rate in the experimental deformation of Yale marble
22. Steady-state flow in marble at 500–800°C
23. The effect of varying water contents on the behaviour of Heavitree quartzite
24. Rheology of synthetic olivine aggregates effect of grain size and of water
25. Hydrolytic weakening in quartz
26. An experimental study of the role of water in quartz deformation
27. Tectonic stresses in the lithosphere: constraints provided by the experimental deformation of rocks
28. Rheology of the lithosphere
29. Hydrolytic weakening of quartz: uptake of molecular water and the role of microfracturing (abstr)
30. Flow law of “wet” quartzite in the α-quartz field (abstr.)
31. Flow strengths of quartz aggregates grain size and pressure effects due to hydrolytic weakening
32. Water-related diffusion and deformation effects in quartz at pressures of 1500 and 300 MPa
33. Experimental studies of the role of water in the plasticity of quartzites
34. The mechanisms of the formation and growth of water bubbles and associated dislocation loops in synthetic quartz
35. Textures and fabrics of upper-mantle peridotites as illustrated by xenoliths from basalts
36. Creep stresses in a rotating disc
37. Experimental control of the water-weakening effect in quartz
38. Finite element folds of similar geometry
39. Dislocations and geological deformation
40. The thermodynamics of water in quartz
41. The role of water in quartz deformation
42. New constraints on transient lower mantle rheology and internal mantle buoyancy from glacial rebound data
43. High-temperature creep of Mt. Burnet dunite
44. Activation volume for creep in the upper mantle
45. Solubility of hydroxyl in natural quartz annealed in water at 900°C and 1.5 GPa
46. The influence of temperature, strain rate and interstitial water in the experimental deformation of calcite rocks
47. The effects of transient rheology on the interpretation of lower mantle viscosity
48. Super-plastic flow in finegrained limestone
49. High temperature flow and dynamic recrystallization in Carrara marble
50. On the rheology of the upper mantle
51. Pressure dependence of rock strength: implications for hydrolytic weakening
52. Transient mantle rheology