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Rare Earth Elements

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Encyclopedia of Astrobiology
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Synonyms

Lanthanides; Rare earth metals; Rare earth oxides

Acronyms

REE

Definition

The rare earth elements (or REE) comprise the family of lanthanides (atomic number Z = 57-71), corresponding to the progressive filling of the 4f orbitals, together with the elements scandium (Sc, Z = 21) and yttrium (Y, z = 39) (Table 1). Their abundance in geological materials is usually less than 0.1 wt. %, that is, the term “rare” compared to abundances of rock-composing major oxides (SiO2, K2O, CaCO3, etc.). They are an extremely consistent group in terms of chemical behavior, making them suitable tracers of numerous geological processes. Rare earth elements are considered particularly informative on the conditions prevailing during the formation of rocks, and REE studies have important applications in petrology and in oceanography, where these elements are derived from the weathering of continental masses and mid-ocean ridges hydrothermalism.

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Correspondence to Daniele L. Pinti .

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Pinti, D.L. (2022). Rare Earth Elements. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1348-4

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_1348-4

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  • Print ISBN: 978-3-642-27833-4

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Chapter history

  1. Latest

    Rare Earth Elements
    Published:
    21 December 2021

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1348-4

  2. Original

    Rare Earth Elements
    Published:
    18 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1348-3