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Anorthosite

Encyclopedia of Astrobiology
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Definition

Anorthosite is a magmatic intrusive rock. It is light colored (leucocratic) and has a medium to coarse grain size (phaneritic). It is mainly composed of plagioclase (andesine, labradorite, bytownite) and minor pyroxene, olivine, and iron-titanium oxides (ilmenite, magnetite). Proterozoic anorthosite forms large massifs associated with granitoids (North America, Scandinavia). Archean coarse-grained (megacrystic) anorthosite occurs in intrusions (dikes and sills) and flows of basaltic composition.

Anorthosite is a common constituent of the lighter surfaces of the Moon called lunar highlands or terrae. Formation of anorthosite requires the concentration of plagioclase from mafic magma by flotation in a magma ocean (as is proposed to have occurred on the Moon), ascent of plagioclase-rich mushes, or low-pressure crystallization in magma chambers.

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Correspondence to Nicholas Arndt .

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© 2014 Springer-Verlag Berlin Heidelberg

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Arndt, N. (2014). Anorthosite. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_81-3

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_81-3

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  • Online ISBN: 978-3-642-27833-4

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  1. Latest

    Anorthosite
    Published:
    27 December 2022

    DOI: https://doi.org/10.1007/978-3-642-27833-4_81-4

  2. Original

    Anorthosite
    Published:
    28 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_81-3