The effect of water on high‐temperature deformation in olivine
- 1 September 1982
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 9 (9) , 1005-1008
- https://doi.org/10.1029/gl009i009p01005
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Oxygen self-diffusion in forsterite: Implications for the high-temperature creep mechanismEarth and Planetary Science Letters, 1980
- High temperature deformation of rocks and mineralsReviews of Geophysics, 1979
- Hydrolytic weakening in quartzTectonophysics, 1978
- High-temperature creep of Mt. Burnet DuniteTectonophysics, 1977
- Steady state flow of rocksReviews of Geophysics, 1976
- Plastic-deformati on mechanisms in quartz: The effect of waterTectonophysics, 1975
- Mechanisms of high-temperature, solid-state flow in minerals and ceramics and their bearing on the creep behavior of the mantleTectonophysics, 1973
- The Earth's Mantle: Evidence of Non-Newtonian FlowScience, 1973
- Laboratory observations of high-temperature rheology of rocksTectonophysics, 1972
- Hydrolytic Weakening of Quartz and Other Silicates*Geophysical Journal of the Royal Astronomical Society, 1967