Definition
Alteration in geochemistry refers to processes by which the mineralogy, composition, and texture of a rock are changed as a result of re-equilibration under conditions of lower temperature and pressure or through interaction with aqueous or CO2-rich fluids. The minerals of the original rock, which may be magmatic, sedimentary, or metamorphic, are transformed into an assemblage of low-temperature, usually finer-grained minerals. A typical example is the replacement of magmatic minerals such as olivine, pyroxene, and feldspar by chlorite, clay minerals, or carbonates. Weathering is a type of alteration that takes place close to the surface through interaction of rock with the atmosphere and with ground- or surface waters. Alteration is also used in chemistry and biology (e.g., DNA alterations).
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© 2014 Springer-Verlag Berlin Heidelberg
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Arndt, N. (2014). Alteration. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_56-2
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DOI: https://doi.org/10.1007/978-3-642-27833-4_56-2
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Publisher Name: Springer, Berlin, Heidelberg
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