文摘
Soil isotopic dating is important for understanding mass transfers related to rock weathering. Here we evaluate a method including TIMS analyses of (234U/238U) activity ratios on < 0.2 μm fractions of a Cameroon laterite. Variations of the (234U/238U) ratios with depth show (1) significant (234U/238U) disequilibrium at the bottom of the pedological units, and (2) progressive returns towards secular equilibrium above. These results suggest that U fractionation occurs at the base of the units and that the analysed fractions probably evolve as closed/restricted systems within each unit. From these data, an overall age of 1.5 Ma may be proposed for the development of this laterite.