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Rohtas Formation
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Rohtas Fm base reconstruction

Rohtas Fm


Period: 
Calymmian

Age Interval: 
earliest Calymmian


Province: 
Proterozoic N.India Vindhyan Basin east

Type Locality and Naming

Uppermost formation (5 of 5) Lower Vindhyan Gr in East


Lithology and Thickness

Upward succession of Rampur Shale Member and Rohtas Limestone Member. The Rohtas Limestone shows rhythmite-like intercalations between thin bedded limestone and shale. Poorly developed columnar stromatolites are also reported.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Overlies the Kheinjua Fm

Upper contact

Major unconformity. Overlain by Lower Quartzite member at base of Kaimur Fm (base of Upper Vindhyan Gr in East)

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[78.94,23.85],[81.15,24.8],[84.23,24.42],[83.66,23.71],[79.58,22.73],[78.94,23.85]]]]}}

Fossils


Age 

1599 +/- 8Ma in middle of Rampur Shale Mbr. See discussion in Lower Vindhyan Gr; for graphic purposes 1600-1580 Ma

Age Span: 

    Beginning stage: 
Calymmian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
1,600.00

    Ending stage: 
Calymmian

    Fraction up in the ending stage: 
0.1

    Ending date (Ma):  
1,580.00

Depositional setting

The Rohtas Limestone Member was deposited under subtidal to intertidal conditions.


Depositional pattern:  


Additional Information


Compiler:  

Main sources: S. Sarkar and S. Banerjee (2020), A Synthesis of Depositional Sequence of the Proterozoic Vindhyan Supergroup in Son Valley, Springer Geology, https://doi.org/10.1007/978-981-32-9551-3_2

Basu, P., and Chakrabarti, R. 2020. Origin and evolution of the Vindhyan Basin: A geochemical perspective. Proc. Indian Natn. Sci. Acad., 86: 111-126.