Articles | Volume 3, issue 2
https://doi.org/10.5194/gchron-3-415-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-3-415-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Short communication/technical note
| 
02 Aug 2021
Short communication/technical note |
| 02 Aug 2021
| 02 Aug 2021
Short communication: Inverse isochron regression for Re–Os, K–Ca and other chronometers
Yang Li
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK
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Short summary
A conventional isochron is a straight-line fit to two sets of isotopic ratios, D/d and P/d, where P is the radioactive parent, D is the radiogenic daughter, and d is a second isotope of the daughter element. The slope of this line is proportional to the age of the system. An inverse isochron is a linear fit through d/D and P/D. The horizontal intercept of this line is inversely proportional to the age. The latter approach is preferred when d<D, which is the case in Re–Os and K–Ca geochronology.
A conventional isochron is a straight-line fit to two sets of isotopic ratios, D/d and P/d,...
