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Potassium Argon Dating

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Lectures in Isotope Geology

Abstract

The main principle of the conventional K-Ar method is very simple. 40K decays to 40Ar, and assuming we know the decay constants and are capable of measuring parent and daughter isotopes rather precisely, we should succeed in calculating an age.

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References

Section 1: References

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© 1979 Springer-Verlag Berlin Heidelberg

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Hunziker, J.C. (1979). Potassium Argon Dating. In: Jäger, E., Hunziker, J.C. (eds) Lectures in Isotope Geology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-67161-6_5

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  • DOI: https://doi.org/10.1007/978-3-642-67161-6_5

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-09158-5

  • Online ISBN: 978-3-642-67161-6

  • eBook Packages: Springer Book Archive

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