Permeability changes during the flow of water through westerly granite at temperatures of 100°–400°C
- 10 January 1978
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 83 (B1), 339-344
- https://doi.org/10.1029/jb083ib01p00339
Abstract
No abstract availableKeywords
This publication has 4 references indexed in Scilit:
- Reduction of porosity by pressure solution: Experimental verificationGeology, 1976
- The effect of microcrack dilatancy on the permeability of westerly graniteJournal of Geophysical Research, 1975
- Stimulation of geothermal energy resourcesPublished by Office of Scientific and Technical Information (OSTI) ,1975
- Permeability of granite under high pressureJournal of Geophysical Research, 1968