Anhydrite (CaSO4) and gypsum (CaSO4·2H2O) are the two most abundant minerals of ancient marine evaporite deposits and are also common in non-marine evaporite deposits. Sedimentary gypsum forms by direct precipitation out of evaporating seawater under arid climatic conditions in hydrologically restricted marine and marginal marine environments (e.g., tidal flats, coastal lagoons, “inland seas”, etc.). In non-marine, arid closed basin systems, gypsum precipitates from evaporating meteoric waters with chemical compositions dependent on the bedrock types and their proportions in the drainage areas. In contrast, at temperatures and pressures typical of sedimentary environments, anhydrite does not precipitate directly from evaporating waters but, as discussed in the next section, forms by dehydration of precursor gypsum precipitates. Sedimentary anhydrite is, in essence, a diagenetic mineral.
Stability fields of anhydrite and gypsum
In modern arid sedimentary environments gypsum readily...
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© 1978 Dowden, Hutchinson & Ross, Inc.
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Hardie, L.A. (1978). Anhydrite and gypsum. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_7
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