Equilibrium dihedral angles in the system H2O−CO2−NaCl-calcite, and implications for fluid flow during metamorphism
- 1 September 1991
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 108 (3), 368-383
- https://doi.org/10.1007/bf00285944
Abstract
No abstract availableKeywords
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