The influence of water on the development of lattice preferred orientation in olivine aggregates

Geophysical Research Letters

Volumn 29, Issue 12, 2002, Pages 17-1-17-4

  Kaminski, E ^a  

^a UNIVERSITÉ PARIS DESCARTES   (France)

Author keywords

[No Author keywords available]

Indexed keywords

ANISOTROPY; CRYSTAL ORIENTATION; CRYSTALLIZATION; CRYSTALS; SHEAR STRESS;

SUBDUCTION ZONES;

SEISMOLOGY;

AGGREGATE; CRYSTALLINITY; LATTICE DYNAMICS; OLIVINE; ORIENTATION;

EID: 0037098821     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2002GL014710     Document Type: Article

References (40)

1. High-temperature creep of olivine single crystals, 2. Dislocation structures
2. High-temperature creep of olivine single crystals. 1. Mechanical results for buffered samples
3. An olivine fabric database: An overview of upper mantle fabrics and seismic anisotropy
4. Teleseismic imaging of subaxial flow at mid-ocean ridge
5. High shear strain of olivine aggregates: Rheological and seismic consequences
6. High-temperature flow of dunite and peridotite
7. Anisotropic convection with implications for the upper mantle
8. The role of water in the deformation of dunite
9. Plastic flow of oriented single crystals of olivine. 1. Mechanical data
10. A plane kinematic model of progressive deformation in a polycrystalline aggregate
11. The influence of plate motions on three-dimensional back arc mantle flow and shear wave splitting
12. Transient creep in natural and synthetic, iron-bearing olivine single crystals: Mechanical results and dislocation microstructure
13. Water in the oceanic upper mantle: Implications for rheology, melt extraction and the evolution of the lithosphere
14. High temperature creep of olivine crystals from four localities
15. Water-induced fabric transition in olivine
16. A kinematic model for recrystallization and texture development in olivine polycrystals
17. Time scales for the evolution of seismic anisotropy in mantle flow
18. Seismic anisotropy due to lattice preferred orientation of minerals: Kinematic or dynamic
19. Rheology of synthetic olivine aggregates: Influence of grain size and water
20. Low-stress high-temperature creep in olivine single crystals
21. Strength of the lithosphere: Constraints imposed by laboratory experiments
22. The role of water in the deformation of olivine single crystals
23. Influence of water on plastic deformation of olivine aggregates 2. Dislocation creep regime
24. Can seismology tell us anything about convection in the mantle?
25. Formation of anisotropy in upper mantle peridotites: A review
26. Mechanisms of flow in naturally and experimentally deformed peridotites
27. Deformation induced recrystallization of minerals
28. Seismic anisotropy and mantle flow
29. On the relation between seismic anisotropy and finite strain
30. A theory for plastic deformation and textural evolution of olivine polycrystals
31. Trench-parallel flow beneath the Nazca plate from seismic anisotropy
32. Simple 2-d models for melt extraction at mid-ocean ridges and island arcs
33. Forward modeling of the development of seismic anisotropy in the upper mantle
34. Viscoplastic self-consistent and equilibrium-based modelling of olivine lattice preferred orientations, 1. Implications for the upper mantle seismic anisotropy
35. Dynamic recrystallization in minerals
36. Modeling dynamic recrystallization of olivine aggregates deformed in simple shear
37. Modelling plastic deformation of peridotite with the self-consistent theory
38. Lattice preferred orientation of olivine aggregates deformed in simple shear
39. Simple shear deformation of olivine aggregates