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Research Paper |
RODO
*Institute of Geological Sciences PAN, Senacka 1, 31-002 Kraków, Poland
* E-mail: ndsrodon{at}cyf-kr.edu.pl
(Received 11 November 1999; revised 23 February 2000)
As plots of K-Ar ages vs. percentage of the detrital component of mineral mixtures containing a detrital and a diagenetic illite (or illite-smectite) have different curved shapes, the linear extrapolation method of extracting the end-member ages is not justified. The curvature depends on the difference in K2O contents; thus it can be minimized if the percentage of detrital illite is normalized to the sum of detrital illite plus illitic fraction of diagenetic illite-smectite.
KEYWORDS: K-Ar ages, shale, end-member ages
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