The transition from hydrostatic to greater than hydrostatic fluid pressure in presently active continental hydrothermal systems in crystalline rock
- 1 May 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (5), 955-958
- https://doi.org/10.1029/91gl00966
Abstract
No abstract availableKeywords
This publication has 6 references indexed in Scilit:
- Trapping of aqueous fluids in the deep crustGeophysical Research Letters, 1990
- Flow properties of continental lithosphereTectonophysics, 1987
- Geophysical evidence for the locations, shapes and sizes, and internal structures of magma chambers beneath regions of Quaternary volcanismPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Constraints on geological strain rates: Arguments from finite strain states of naturally deformed rocksJournal of Geophysical Research, 1982
- Permeability of crystalline and argillaceous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1980
- Friction of rocksPure and Applied Geophysics, 1978