Badami Gr
Type Locality and Naming
Lithology and Thickness
Sandstone with a lower Kerur Fm and upper Katageri Fm. These flat-lying Badami Group sediments preserve signature of fluvial to shallow marine tidal environment (Fig. A and B).
[Figure: Kerur Fm, Badami Gr, field photographs illustrating lithology and sedimentary structures (A) Temple arenite. (B) Closeup view of the sandstone showing widely varying palaeocurrent direction. Lens cap as scale in the center of photo. (from Saha et al., 2016)]
Relationships and Distribution
Lower contact
Angular unconformity on Hoskatti Fm (uppermost formation of Kaladgi Gr) pelagic shale, overlain by Kerur Fm conglomerate at base of Badami Gr = Basement uplift, folding and a hiatus in deposition follow the first cycle (Kaladgi Gr) of sedimentation in the Kaladgi Basin.
Upper contact
Major unconformity; overlain by Deccan Traps Fm basalts (end-Cretaceous)
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Upward transition from fluvial to a tidal shelf.
Additional Information