Somanpalli Gr
Type Locality and Naming
A deformed mixed carbonate-siliciclastic succession occurring around the confluence of Indravati and Godavari rivers in the eastern Proterozoic belt and lying unconformably below the Albaka Gr has been designated as the Somanpalli Group
Lithology and Thickness
Sandstone, Chert and Claystone. Upward succession of Bodela Vagu Fm, Somnur Fm, Gutta Chert Fm, Tarur Nala Fm, Kopela Shale Fm and Po Gutta Sandstone
Relationships and Distribution
Lower contact
Unconformably underlain by Kotapalle Limestone Fm of upper Devalmari Gr
Upper contact
Unconformably overlain by Somandevra Quartzite Fm of lower Albaka Gr
GeoJSON
Fossils
Age
Depositional setting
Upward deepening from intertidal flats to deep shelf, then shallowing to shoreface. Although the mixed carbonate-siliciclastic successions of the Bodela Vagu Fm and the Somnur Fm represent tidal shelf deposition, the Tarur Nala Fm and the Pedda Gutta Chert Fm represent deep-shelf setting with common turbidite deposits. The thick succession of black shales of the Kopela Shale Fm has been interpreted as representing pelagic mud deposition indicating maximum sea-level rise; a reversal to tidal shelf environment of deposition is attested by the Po Gutta Fm.
Additional Information