Boron isotope geochemistry during diagenesis. Part II. Applications to organic-rich sediments

The measured clay-water isotope fractionation for boron was applied to natural organic-rich sediments undergoing illitization. Two field areas were chosen that show illitization occurring over a range of temperatures (80-500 degreesC). Samples representing diagenetic temperatures of illitization (80-200 degreesC) are from the Gulf of Mexico sedimentary basin at 4 to 6-km depth in the Eocene Wilcox Fm and Jurassic Norphlet Fm. The higher temperatures of illitization (200-500 degreesC) occur in a contact metamorphic aureole of the Cretaceous Pierre shale near Walsenburg, Colorado. Here the kinetics of the illitization reaction are more rapid than in a slowly subsiding sedimentary basin, but the chemical and mineralogical variations are minimized as complete illitization occurs over a small lateral distance in a single bentonite layer. These studies indicate that B-isotopes provide a more sensitive indicator of fluid variations in sedimentary basins than O-isotopes, and that B-isotope analyses of authigenic illite can be a valuable geochemical tracer of fluid/rock interactions. Boron isotope ratios in authigenic illite (pore filling) and muscovite (stylolites) from reservoir sandstones in the Gulf of Mexico are distinct from adjacent illitic mudstones, whereas the oxygen isotopic ratios show little variation. Fluids in equilibrium with the mudstones cannot precipitate the authigenic clays with higher delta B-11 values measured in the hydrocarbon reservoirs. This suggests that the reservoir fluids were not in communication with the adjacent mudstone pore fluids but were introduced from another source area, perhaps carrying a B-isotopic label derived from the hydrocarbon source region. Authigenic illite formed in the Pierre shale meta-bentonite shows large isotopic fractionations of boron (20 parts per thousand) during illitization at high temperatures. incorporation of 500 ppm B in illite formed at 500 degreesC shows that illite is a host for B even at metamorphic temperatures. By using the experimentally derived B-isotope fractionation data for silicates the measured delta B-11 values of VS could be predicted by using a Rayleigh fractionation model. Oxygen isotopic variations were negligible over this temperature range and thus provide Little information on the mechanism of illitization. Copyright (C) 2001 Elsevier Science Ltd.