K–Ar dating
Potassium–Argon dating or K–Ar dating is a radiometric dating method used in geochronology, which is part of geology. It is based on measurement of the product of the radioactive decay of an isotope of potassium (K) into argon (Ar).
Potassium is a common element found in many materials, such as micas, clay, tephra, and evaporites. In these materials, the decay product 40Ar is able to escape the liquid (molten) rock, but starts to build up when the rock solidifies (recrystallises). Time since recrystallization is calculated by measuring the ratio of the amount of 40Ar to the amount of 40K remaining. The long half-life of 40K is more than a billion years, so the method is used to calculate the absolute age of samples much older than a few thousand years.[1]
Quickly cooled lavas make nearly ideal samples for K–Ar dating. They also preserve a record of the direction and intensity of the local magnetic field at that time.[2] The geomagnetic reversal time scale was calibrated largely using K–Ar dating.[1]
References
change- ↑ 1.0 1.1 McDougall, Ian and T. Mark Harrison 1999. Geochronology and thermochronology by the 40Ar/39Ar method. Oxford. ISBN 0-19-510920-1
- ↑ Because the sample cooled past the Curie point of iron.
