Pore pressure diffusion and the mechanism of reservoir-induced seismicity
- 1 November 1984
- journal article
- Published by Springer Nature in Pure and Applied Geophysics
- Vol. 122 (6), 947-965
- https://doi.org/10.1007/bf00876395
Abstract
No abstract availableKeywords
This publication has 36 references indexed in Scilit:
- Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gougeTectonophysics, 1984
- Permeability of crystalline rocks: New in situ measurementsJournal of Geophysical Research, 1984
- Permeability and frictional properties of San Andreas Fault GougesGeophysical Research Letters, 1981
- Limits on lithospheric stress imposed by laboratory experimentsJournal of Geophysical Research, 1980
- Permeability of crystalline and argillaceous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1980
- Strength changes due to reservoir‐induced pore pressure and stresses and application to Lake OrovilleJournal of Geophysical Research, 1978
- Time evolution of stress under an artificial lake and its implication for induced seismicityCanadian Journal of Earth Sciences, 1978
- Friction of rocksPure and Applied Geophysics, 1978
- Stress corrosion theory of crack propagation with applications to geophysicsReviews of Geophysics, 1977
- Confined fluids as strain metersJournal of Geophysical Research, 1970