ReOs isotopes and major and trace element geochemistry of carbonaceous shales, Aravalli Supergroup, India: Impact of post-depositional processes

- Geochemical and ReOs isotopic study of weathered and apparently fresh black shales from Lower Aravalli Group, India.
- Results show open system behavior of Re and Os with preferential loss of Re relative to Os.
- Most of these shales are found to have Re < Os concentrations.
- Loss of Re and increase in 187Os/188Os ratios are observed during interaction of shales with hydrothermal fluids.

This study presents ReOs isotopes and major and trace elemental geochemistry of carbonaceous (black) shales and a weathering profile developed on them from the Paleoproterozoic deposits of the Jhamarkotra Formation, Lower Aravalli Group, India. These measurements provide information on the impact of post-depositional processes, particularly hydrothermal fluid interactions, on the 187Re187Os geochronology and element mobility in shales. In contrast to previously reported compositions for black shales, the Re concentrations of the Jhamarkotra shales are in general lower than their corresponding Os concentrations. The 187Os/188Os ratios of the black shales vary widely, from 3.5 to 10.5, without any discernible systematic trend with 187Re/188Os (range: 0.4 to 17.7; excluding an outlier); these 187Re/188Os ratios are lower by a few orders of magnitude than those generally reported for “fresh” black shales. These observations indicate that the Jhamarkotra shales, though they seem visually well preserved, have undergone post-depositional modification, resulting in “open system” behavior of Re and Os, with Re more mobile than Os.Higher SiO2/TiO2 and K2O/Na2O ratios of the Jhamarkotra shales compared to their sediment provenance suggest interaction of the shales with hydrothermal (possibly Si and K-rich) fluids. The SiO2/TiO2 ratios (an index for hydrothermal alteration) show negative correlation with Re/Corg and positive correlation with Corg/N ratios (42-154), indicating loss of Re and nitrogen during hydrothermal fluid interaction. Earlier studies have shown the presence of Re porphyrins (N-containing organic compounds) in black shales. Thus, the observed co-variations of SiO2/TiO2 with Re/Corg and Corg/N ratios suggest mobilization of Re from the porphyrins in the shales. Further, positive correlation between SiO2/TiO2 and 187Os/188Os ratios indicates that significant amounts of radiogenic Os component were re-distributed throughout the Jhamarkotra shales during the post-depositional processes.In the weathering profile developed on black shales, the Al2O3-normalized abundance ratios of mobile major elements are in general lower in the upper layers relative to those in deeper sections attesting to their preferential mobility during chemical weathering. On the contrary, the Al2O3-normalized ratios of trace elements mostly showed insignificant depth variations in the weathering profile, suggesting limited mobility over the depth of the profile. The depth profiles of Re/Al2O3 and 188Os/Al2O3 and 187Os/188Os ratios in the weathering profile by and large reflect compositions of their presumed parent shales, which have gone through significant post-depositional changes.