High‐temperature creep of forsterite single crystals
- 10 July 1981
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 86 (B7), 6219-6234
- https://doi.org/10.1029/jb086ib07p06219
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Deformation Processes in the Upper MantlePublished by Wiley ,2013
- Oxygen self-diffusion in forsterite: Implications for the high-temperature creep mechanismEarth and Planetary Science Letters, 1980
- Decorated dislocations in forsteritePhysics and Chemistry of Minerals, 1979
- Transient and steady-state creep of pure forsterite at low stressPhysics of the Earth and Planetary Interiors, 1979
- High temperature olivine creep: Evidence for control by edge dislocationsGeophysical Research Letters, 1979
- Plastic flow of oriented single crystals of olivine: 2. Observations and interpretations of the dislocation structuresJournal of Geophysical Research, 1977
- Plastic flow of oriented single crystals of olivine: 1. Mechanical dataJournal of Geophysical Research, 1977
- A comparison of the creep properties of pure forsterite and iron-bearing olivineTectonophysics, 1977
- Fe-Mg lattice diffusion in olivineJournal of Geophysical Research, 1973
- High Temperature Flow of Dunite and PeridotiteGSA Bulletin, 1970