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Badami Gr
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Badami Gr base reconstruction

Badami Gr


Period: 
Tonian

Age Interval: 
late Tonian


Province: 
Proterozoic S.India Kaladgi Basin

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)]


Lithology Pattern: 
Sandstone


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

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[74.23,16.22],[75.43,16.48],[76.18,16.14],[76,15.84],[74.49,15.82],[74.23,16.22]]]]}}

Fossils


Age 


Age Span: 

    Beginning stage: 
Tonian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
804.00

    Ending stage: 
Tonian

    Fraction up in the ending stage: 
0.86

    Ending date (Ma):  
759.20

Depositional setting

Upward transition from fluvial to a tidal shelf.


Depositional pattern:  


Additional Information


Compiler:  

From: Saha D. (Dilip), Patranabis-Deb, S., and Colllins, A.S. (2016) Proterozoic stratigraphy of southern Indian cratons and global context. In: Stratigraphy & Timescales, 1: 1-59.