Rate laws for water‐assisted compaction and stress‐induced water‐rock interaction in sandstones
- 10 July 1995
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 100 (B7) , 13093-13112
- https://doi.org/10.1029/95jb00912
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Solution-precipitation enhanced diffusional creep of partially molten olivine-basalt aggregates during hot-pressingPublished by Elsevier ,2003
- Kinetics of pressure solution at halite‐silica interfaces and intergranular clay filmsJournal of Geophysical Research, 1995
- Magnetic and electric fields associated with changes in high pore pressure in fault zones: Application to the Loma Prieta ULF emissionsJournal of Geophysical Research, 1995
- Ductile creep, compaction, and rate and state dependent friction within major fault zonesJournal of Geophysical Research, 1995
- Experimental pressure solution in halite: the effect of grain/interphase boundary structureJournal of the Geological Society, 1991
- Solution-transfer compaction of quartzites: Progress toward a rate lawGeology, 1991
- Marine diagenesis of feldspathic sand: A flow-through experimental study at 200°C, 1 kbarChemical Geology, 1991
- Geochemical self-organization; III, A mechano-chemical model of metamorphic differentiationAmerican Journal of Science, 1990
- Healing of microcracks in quartz: Implications for fluid flowGeology, 1990
- Experimental pressure solution-deposition on quartz grains: the crucial effect of the nature of the fluidJournal of Structural Geology, 1986