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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Section 2: Text Books
Dalrymple, G.B., Lanphere, M.A.: Potassium-Argon-Dating. San Francisco: Freeman, 1966
Schaeffer, O.A., Zähringer, J. (eds.): Potassium Argon Dating. Berlin-Heidelbereg New York: Springer, 1966
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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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