pH buffering by metastable mineral-fluid equilibria and evolution of carbon dioxide fugacity during burial diagenesis
- 1 March 1993
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 57 (5), 1017-1027
- https://doi.org/10.1016/0016-7037(93)90037-w
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Organic acids and inorganic ions in waters from petroleum reservoirs, Norwegian continental shelf: a multivariate statistical analysis and comparison with American reservoir formation watersApplied Geochemistry, 1991
- Carboxylic acid anions in formation waters, San Joaquin Basin and Louisiana Gulf Coast, U.S.A.—Implications for clastic diagenesisApplied Geochemistry, 1990
- Sandstone diagenesis in the Pattani Basin (Gulf of Thailand): history of water-rock interaction and comparison with the Gulf of MexicoApplied Geochemistry, 1990
- Origin and evolution of formation waters from oil fields on the Norwegian shelfApplied Geochemistry, 1989
- Carbonate equilibria and pH buffering by organic acids — Response to changes in pCO2Chemical Geology, 1989
- Activity/Composition Relations among Silicates and Aqueous Solutions: II. Chemical and Thermodynamic Consequences of Ideal Mixing of Atoms on Homological Sites in Montmorillonites, Illites, and Mixed-Layer ClaysClays and Clay Minerals, 1983
- Active albitization of plagioclase, Gulf Coast TertiaryAmerican Journal of Science, 1982
- Buffering of pore fluids by metamorphic reactionsAmerican Journal of Science, 1975
- Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures; II, Debye-Huckel parameters for activity coefficients and relative partial molal propertiesAmerican Journal of Science, 1974
- Thermodynamics of hydrothermal systems at elevated temperatures and pressuresAmerican Journal of Science, 1969