Upper Vindhyan Gr
Type Locality and Naming
Upward succession of Kaimur Fm, Rewa Fm and Bhandar Fm (termed groups by Basu and Chakrabarti, 2020), but their internal members (or formations) differ between the West (Chambal Valley Sector) and the East (Son Valley Sector)
Synonym: Upper Vindhyan SuperGroup (used as SuperGroup by Basu and Chakrabarti, 2020; but as Group by Sarkar and Banerjee, 2020, which is used here).
Lithology and Thickness
Sandstone and shale are dominant
Relationships and Distribution
Lower contact
Major hiatus; overlies Lower Vindhyan Gr (Khorip Fm in West; Rohtas Fm in East)
Upper contact
In WEST - Overlain by Deccan Traps Fm. In EAST – Overlain by alluvial Lameta Fm or modern Laterite soil.
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
Kumar, S., 2012. Stratigraphy and correlation of the Neoproterozoic deposits of central and western India: an overview. In Bhat, G. M., Craig, J., Thurow, J. W., Thusu, B.&Cozzi, A. (eds) 2012. Geology and Hydrocarbon Potential of Neoproterozoic–Cambrian Basins in Asia. Geological Society, London, Special Publications, 366, 75–90.