Effects of deviatoric stress on undrained pore pressure response to fault slip
- 10 August 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 102 (B8) , 17943-17950
- https://doi.org/10.1029/97jb01358
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- Poroelastic Techniques in the Study of Earthquake-Related Hydrologic PhenomenaPublished by Elsevier ,1996
- Laboratory measurements of a complete set of poroelastic moduli for Berea sandstone and Indiana limestoneJournal of Geophysical Research, 1995
- Pore pressure buildup coefficient in synthetic and natural sandstonesInternational Journal of Rock Mechanics and Mining Sciences, 1993
- Hydrologic effects on water level changes associated with episodic fault creep near Parkfield, CaliforniaJournal of Geophysical Research, 1989
- Fluid pressure response to undrained compression in saturated sedimentary rockGeophysics, 1986
- Recent movement on the Garlock Fault as suggested by water level fluctuations in a well in Fremont Valley, CaliforniaJournal of Geophysical Research, 1985
- Coupled deformation-diffusion effects on water-level changes due to propagating creep eventsPure and Applied Geophysics, 1985
- Some basic stress diffusion solutions for fluid‐saturated elastic porous media with compressible constituentsReviews of Geophysics, 1976
- Aftershocks Caused by Pore Fluid Flow?Science, 1972
- The Pore-Pressure Coefficients A and BGéotechnique, 1954