Diffusivity of ions in pore water as a quantitative basis for rock deformation rate estimates
- 27 January 2000
- journal article
- Published by Elsevier
- Vol. 245 (3-4) , 185-203
- https://doi.org/10.1016/0040-1951(94)00234-z
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Oxygen diffusion in a fine‐grained quartz aggregate with wetted and nonwetted microstructuresJournal of Geophysical Research, 1992
- Measurement of oxygen grain boundary diffusion in natural, fine-grained, quartz aggregatesGeochimica et Cosmochimica Acta, 1991
- Oxygen diffusion in quartz: Dependence on temperature and water fugacityChemical Geology, 1991
- “Pressure solution” creep: Some causes and mechanismsJournal of Geophysical Research, 1984
- Point defect chemistry of minerals under a hydrothermal environmentJournal of Geophysical Research, 1984
- Oxygen diffusion in quartzJournal of Geophysical Research, 1984
- The influence of metamorphic environment upon the deformation of mineralsTectonophysics, 1981
- Diffusion Flow Laws in Metamorphic RocksGSA Bulletin, 1973
- Hydrolytic Weakening of Quartz and Other Silicates*Geophysical Journal of the Royal Astronomical Society, 1967
- DIFFUSION OF IONS THROUGH INTERGRANULAR SPACES IN WATER-SATURATED ROCKSGSA Bulletin, 1949