Introduction
Cementation is the process of precipitation of mineral matter (cements) in pores within sediments or rocks. It is one of several processes, including mechanical and chemical compaction and mineral replacement, that constitute diagenesis and, taken collectively, produce progressive porosity reduction and lithification of sedimentary strata with increasing age and/or depth of burial. Cementation occurs in open intergranular or intragranular pores (i.e., between or within grains), and also takes place in larger openings such as vugs, caves or fractures. Cements even form crusts on surfaces at sediment-water or sediment-air interfaces. Precipitation of cements can occur at any stage from deposition, through burial, to uplift and re-exposure.
Cements occur in all types of siliciclastic, carbonate and evaporite strata and include an enormous variety of minerals. The most common cements are carbonates (especially calcite, aragonite, dolomite, and siderite), silicates (primarily...
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Cross-references
AnkeriteBeachrockCaliche–CalcreteCathodoluminescenceChalk Chert, Chalcedony and Flint Compaction (Consolidation) of SedimentsDiagenetic StructuresDiffusion, ChemicalDolomites and DolomitizationEvaporitesGlaucony and VerdineGypsum Hardground (and Firmground) Hydrocarbons in SedimentsKaolin Group MineralsLateritesLepisphereMicritizationPorewaters in SedimentsPressure SolutionQuartz, DetritalRed BedsSabkha, Salar, Salt FlatSand and Sandstones (Siliciclastics)SeawaterSeptarian ConcretionsSilcreteSiliceous SedimentsSmectite GroupSpeleothemsStylolitesTravertineZeolites in Sedimentary Rocks
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Scholle, P.A., Ulmer-Scholle, D. (1978). Cements and cementation. 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_40
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