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Absolute and Relative Ages

Encyclopedia of Astrobiology
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Definition

In geochronology, the absolute age of a rock is the age obtained from the measurement of spontaneous decay of radioactive nuclides contained in the rocks or its constituent minerals. It differs from the relative age. This latter is the age of a rock obtained from time and space relations between rock formations, giving only qualitative or semiquantitative information on the period when the rock formed.

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Correspondence to Daniele L. Pinti .

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© 2014 Springer-Verlag Berlin Heidelberg

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Pinti, D.L. (2014). Absolute and Relative Ages. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5155-1

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_5155-1

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  • Online ISBN: 978-3-642-27833-4

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Chapter history

  1. Latest

    Absolute and Relative Ages
    Published:
    07 December 2021

    DOI: https://doi.org/10.1007/978-3-642-27833-4_5155-2

  2. Original

    Absolute and Relative Ages
    Published:
    22 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_5155-1