Equilibrium dihedral angles in the system quartz-CO2H2ONaCl at 800°C and 1–15 kbar: the effects of pressure and fluid composition on the permeability of quartzites-Reference-Cited by-同舟云学术

Equilibrium dihedral angles in the system quartz-CO2H2ONaCl at 800°C and 1–15 kbar: the effects of pressure and fluid composition on the permeability of quartzites

Published:1992-12 Issue:1 Volume:114 Page:171-184
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Holness Marian B.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference24 articles.

1. Direct observation of near-equilibrium pore geometry in synthetic quartzites at 600–800°C and 2–10.5 kbar;Laporte;J. Geol.,1991

2. Solid-liquid interfacial tensions by the dihedral angle method. A mathematical approach;Passerone;Acta Metall.,1985

3. Fluids in the lithosphere, I: Experimentally-determined wetting characterisitcs of CO2H2O fluids and their implications for fluid transport, host rock physical properties, and fluid inclusion formation;Watson;Earth Planet. Sci. Lett.,1987

4. Intergranular distribution of pore fluid and the nature of high-angle grain boundaries in limestone and marble;Hay;J. Geophys. Res.,1988

5. The effect of fluid chemistry on wetting textures in novaculite;Lee;J. Geophys. Res.,1991

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