In situ permeability and fluid pressure measurements at ∼2 km depth in the Cajon Pass research well
- 1 August 1988
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 15 (9), 1029-1032
- https://doi.org/10.1029/gl015i009p01029
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- Permeability of rock samples from Cajon Pass, CaliforniaGeophysical Research Letters, 1988
- State of stress, permeability, and fractures in the Precambrian granite of northern IllinoisJournal of Geophysical Research, 1983
- Acoustic characterization of fracture permeability at Chalk River, OntarioCanadian Geotechnical Journal, 1983
- In situ study of the physical mechanisms controlling induced seismicity at Monticello Reservoir, South CarolinaJournal of Geophysical Research, 1982
- Geochemical evidence for water‐rock interaction along the San Andreas and Garlock Faults of CaliforniaJournal of Geophysical Research, 1980
- Heat flow and energetics of the San Andreas Fault ZoneJournal of Geophysical Research, 1980
- Permeability of crystalline and argillaceous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1980
- Heat flow near major strike-slip faults in CaliforniaJournal of Geophysical Research, 1971
- Response of a finite‐diameter well to an instantaneous charge of waterWater Resources Research, 1967