Skip to main content

Anhydrite and gypsum

  • Reference work entry
  • First Online:

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

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...

This is a preview of subscription content, log in via an institution.

Buying options

Chapter
USD   29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD   329.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD   329.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Learn about institutional subscriptions

Bibliography

  • Ali, Y.A., and West, I.M., 1983. Relationships of modern gypsum nodules in sabkhas of loess to compositions of brines and sediments in northern Egypt. Journal of Sedimentary Petrology, 53: 1151–1168.

    Google Scholar 

  • Bebout, D.G., and Maiklem, W.R., 1973. Ancient anhydrite facies and environments, Middle Devonian Elk Point Basin, Alberta. Bulletin of Canadian Petroleum Geology, 21: 287–343.

    Google Scholar 

  • Butler, G.P., 1970. Holocene gypsum and anhydrite of the Abu Dhabi sabkha: an alternative explanation of origin. In Rau, J.L., and Dellwig, L.F. (eds.), Proceedings of the Third Salt Symposium. Cleveland: Northern Ohio Geological Society, pp. 120–152.

    Google Scholar 

  • Degens, E.T., and Ross, D.A. (eds.), 1969. Hot Brines and Recent Metal Deposits in the Red Sea. Springer-Verlag.

    Google Scholar 

  • Demicco, R.V., and Hardie, L.A., 1994. Sedimentary Structures and Early Diagenetic Features of Shallow Marine Carbonate Deposits. SEPM Atlas Series Number 1, 265pp.

    Google Scholar 

  • Garber, R.A., Levy, Y., and Friedman, G.M., 1987. The sedimentology of the Dead Sea. Carbonates and Evaporites, 2: 43–57.

    Google Scholar 

  • Hardie, L.A., 1967. The gypsum-anhydrite equilibrium at one atmosphere pressure. American Mineralogist, 52: 171–200.

    Google Scholar 

  • Hardie, L.A., and Eugster, H.P., 1971. The depositional environments of marine evaporites: a case for shallow clastic accumulation. Sedimentology, 16: 187–220.

    Google Scholar 

  • Hardie, L.A., and Shinn, E.A., 1986. Carbonate depositional environments modern and ancient, part 3: tidal flats. Colorado School of Mines Quarterly, 81: 1–74.

    Google Scholar 

  • Imlay, R.W., 1940. Lower Cretaceous and Jurassic formations of southern Arkansas and their oil and gas possibilites. Information Circular 12, Arkansas Resources and Development Commission, Little Rock, 64 pp.

    Google Scholar 

  • Jung, W., 1958. Zur Feinstratigrafie de Werraanhydrite (Zechstein 1) im Bereich der Sangerhauser und Mansfelder Mulde. Geologie, Beihefte, 24: 312–325.

    Google Scholar 

  • Murray, R.C., 1964. Origin and diagenesis of gypsum and anhydrite. Journal of Sedimentary Petrology, 34: 512–523.

    Google Scholar 

  • Neev, D., and Emery, K.O., 1967, The Dead Sea: depositional processes and environments of evaporites. Geological Survey of Israel Bulletin, 41: 147 pp.

    Google Scholar 

  • Parea, G.C., and Ricchi Lucchi, F., 1972. Resedimented evaporites in the Periadriatic trough. Israel Journal of Earth Science, 21: 125–141.

    Google Scholar 

  • Riley, C.M., and Byrne, J.V., 1961. Genesis of primary structures in anhydrite. Journal of Sedimentary Petrology, 31: 553–559.

    Google Scholar 

  • Warren, J.K., 1989. Evaporite Sedimentology, Prentice Hall.

    Google Scholar 

Cross-references

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 1978 Dowden, Hutchinson & Ross, Inc.

About this entry

Cite this entry

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

Download citation

  • DOI: https://doi.org/10.1007/978-1-4020-3609-5_7

  • Published:

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-1-4020-0872-6

  • Online ISBN: 978-1-4020-3609-5

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics