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Revisiting the stratigraphy of the Mesoproterozoic Chhattisgarh Supergroup,Bastar craton,India based on subsurface lithoinformation
Authors:Arunangshu Mukherjee  Ranjan Kumar Ray  Dinesh Tewari  Vijay Kumar Ingle  Bikram Kumar Sahoo  M W Y Khan
Institution:1. Rajiv Gandhi National Ground Water Training and Research Institute, Central Ground Water Board, Bhu Jal Bhawan, NH-IV, Faridabad, 121 001, India.
6. Upper Yamuna River Board, R K Puram, New Delhi, 110 066, India.
2. Central Ground Water Board, Bhu Jal Bhawan, NH-IV, Faridabad, 121 001, India.
3. Central Ground Water Board, Sector 27A, Madhya Marg, Chandigarh, 160 019, India.
4. Rajiv Gandhi National Ground Water Training and Research Institute, Central Ground Water Board, Tagore Nagar, Raipur, 492 001, India.
5. School of Studies in Geology, Pt. Ravishankar Shukla University, Raipur, 492 007, India.
Abstract:In the last 10 years, several teams of geologists from different institutions in India and abroad have vigorously investigated the Chhattisgarh basin (Bastar craton, India). Based on the new results and the lithologs of more than 350 water wells, resistivity and gamma-ray logs, and extensive geological traverses, we present a revised geological map, relevant cross sections, a new comprehensive stratigraphic column and a discussion of the new findings. Major outcomes of this revision are: (1) confirming the existence of two sub-basins (Hirri and Baradwar) and two depocentres; (2) establishing the age of the basin to be essentially Mesoproterozoic; (3) discarding the ‘unclassified Pandaria Formation’ and classifying the package of Pandaria rock units into Chandi, Tarenga, Hirri and Maniari formations in the Hirri sub-basin; (4) accepting the ‘group’ status of the Singhora Group and the newly proposed Kharsiya Groups in the Baradwar sub-basin; (5) establishing an intrabasinal correlation of formations; (6) reappraising the thicknesses of the different formations; and (7) finding that the geometry of the basin is ‘bowl-shaped’, which is compatible with a sag model for the origin and evolution of the basin.
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