Abstract
Two suites of experiments at 600°C and 200 MPa have been performed on samples of Arkansas Novaculite to investigate the effect of fluid chemistry on the local distribution of fluids amid grains of solid rock under crustal conditions. Analysis of texture before and after these experiments indicates that fluid chemistry has an effect on both equilibrium wetting angles and the degree of fluid connectivity along triple junctions. -from Authors
Original language | English (US) |
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Pages (from-to) | 10,023-10,037 |
Journal | Journal of Geophysical Research |
Volume | 96 |
Issue number | B6 |
DOIs | |
State | Published - 1991 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Oceanography
- Forestry
- Aquatic Science
- Ecology
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Space and Planetary Science
- Earth and Planetary Sciences (miscellaneous)
- Palaeontology