Tetraphenylborate-assisted extraction of K and Ar from micaceous clay minerals: A promising method for the geochronology of diagenetic illite

Abstract

Tetraphenylborate (TPB)-assisted exchange of Na + for structural K was explored to establish the extent to which K and radiogenic Ar were removed from mixed-layer illite-smectite (Ilt-Sme) and detrital muscovite in various clay fractions (<1, 1–2 and 2–5 µm) of three Illinois Basin palaeosols and of Ilt-Sme from a K-bentonite (<2 µm) clay. The K–Ar age value of the treated Ilt-Sme was virtually the same as that of the untreated material regardless of TPB exchange duration in the K-bentonite. Interlayer K is extracted quickly but not completely from fine illitic material. Interlayer K is extracted more slowly but more completely from coarser clay-sized muscovite based on changes in X-ray diffraction traces, K contents and K–Ar age values of the palaeosol size fractions upon TPB treatment. One hour of TPB treatment revealed that (1) detrital Ilt-Sme was predominant over diagenetic Ilt-Sme in one palaeosol and (2) relatively more of the K in R0 Ilt-Sme is resistant to TPB treatment than in illite-rich, ordered Ilt-Sme, which indicates that the single illite layers hold K + against TPB exchange in the fine Ilt-Sme. The age values of all palaeosol size fractions treated for several weeks converged into a narrow range (mean value 247 ± 5 Myr), consistent with the remaining K and Ar being predominantly in illitic interlayers of diagenetic origin. TPB treatment is a promising technique to isolate diagenetic (or pedogenic) illite in clay fractions containing detrital components for K–Ar age determinations.