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Bandyopadhyay, Saswati
- Upper Gondwana Stratigraphy, North of the Pranhita-Godavari Confluence, Southern India
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Authors
Affiliations
1 Geological Studies Unit, Indian Statistical Institute, 203, Barrackpore Trunk Road, Calcutta 700035, IN
1 Geological Studies Unit, Indian Statistical Institute, 203, Barrackpore Trunk Road, Calcutta 700035, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 4 (1985), Pagination: 261-266Abstract
A revised geological map showing the Upper Gondwana stratigraphy of the area north of the Pranhita-Godavari confluence is presented. The early Upper Triassic (Carnian) Maleri Formation, is overlain conformably by the Dharmaram Formation of late Upper Triassic (Norian-Rhaetian) age. The two local sandstones, viz., the Sironcha sandstone and the Anaram sandstone, earlier believed to be the lithological constituents of the Lower Gondwana Kamthi Formation and the Upper Gondwana Kota Formation, respectively, are found to be inter-related. The two sandstones have been mapped within the Dharmaram Formation. It is suggested that the plant remains described from the Anaram sandstone are of late Upper Triassic age.
- Upper Gondwana Succession of the Rewa Basin, India: Understanding the Interrelationship of Lithologic and Stratigraphic Variables
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Authors
Affiliations
1 Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721 302, IN
2 Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata - 700 108, IN
1 Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721 302, IN
2 Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata - 700 108, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 79, No 6 (2012), Pagination: 563-575Abstract
The current work attempts to address a century old problem regarding the stratigraphic disposition of the Upper Gondwana succession of the Rewa basin based on geological mapping and litholog preparation along well exposed transects. The proposed Upper Gondwana stratigraphy of the Rewa basin comprises a continuous and thick package of Triassic sediments unconformably overlain by the Jurassic Parsora Formation. The Triassic succession consists of a basal Pali Formation, an intermediate and newly designated Karki Formation and the overlying mud-dominant Tiki Formation. These formations are well defined based on physical attributes such as lithology, textures and sedimentary structures, and are easily distinguishable in the field. Based on stratigraphic correlation and fossil content, a Lower-Middle Triassic age has been assigned for the Pali and Karki formations, while the Tiki Formation is Upper Triassic (Carnian) in age. Preliminary observations based on lithological characteristics, sand body geometry and sand: mud ratios suggest that within a fluvial setting there were considerable changes in environments of deposition through time, especially during Triassic to Jurassic transition.Keywords
Gondwana, Lithostratigraphy, Parsora Formation, Triassic, Rewa Basin.References
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