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About: Mineral hydration     Goto   Sponge   NotDistinct   Permalink

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Type: yago:WikicatChemicalReactionsyago:WikicatOrganicReactionsyago:ChemicalProcess113446390yago:ChemicalReaction113447361yago:NaturalProcess113518963yago:PhysicalEntity100001930yago:Process100029677yago:WikicatInorganicReactionsdisease New Facet based on Instances of this Class

In chemistry, mineral hydration is an inorganic chemical reaction which adds water to the crystal structure of a mineral, usually creating a new mineral, usually called a hydrate. In geological terms, the process of mineral hydration is known as retrograde alteration and is a process occurring in retrograde metamorphism. It commonly accompanies metasomatism and is often a feature of wall rock alteration around ore bodies. Hydration of minerals occurs generally in concert with hydrothermal circulation which may be driven by tectonic or igneous activity.