Permeability changes during the flow of water through westerly granite at temperatures of 100°–400°C

Author:

Summers R.,Winkler K.,Byerlee J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference7 articles.

1. Permeability of granite under high pressure;Brace;J. Geophys. Res.,1968

2. Keenan, J. H., , F. G., Keys, , P. G., Hill, , J. G., Moore, , Steam Tables—Thermodynamic Properties of Water Including Vapor, Liquid and Solid Phases, int. ed., 114 John Wiley, New York, 1969,

3. Stimulation of geothermal energy resources;Kruger,1975

4. Los Alamos dry geothermal source demonstration project;Smith,1975

5. Reduction of porosity by pressure solution: Experimental verification;Sprunt;Geology,1976

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