Revisiting the stratigraphy of the Mesoproterozoic Chhattisgarh Supergroup, Bastar craton, India based on subsurface lithoinformation

• Published in: Journal of Earth System Science Vol. 123; no. 3; pp. 617 - 632
• Main Authors: Mukherjee, Arunangshu, Ray, Ranjan Kumar, Tewari, Dinesh, Ingle, Vijay Kumar, Sahoo, Bikram Kumar, Y Khan, M W
• Format: Journal Article
• Language: English
• Published: India Springer India 01-04-2014; Springer Nature B.V
• Subjects: Cratons; Earth and Environmental Science; Earth Sciences; Formations; Gamma rays; Geologic mapping; Geological mapping; Geological maps; Geologists; Lithology; Lithosphere; Oil shale; Space Exploration and Astronautics; Space Sciences (including Extraterrestrial Physics; Stratigraphy; Water wells; India; Lithostratigraphy; black shale; Pandaria Formation; Chhattisgarh basin; subsurface lithologs; India
• ISSN: 0253-4126; 0973-774X
• DOI: 10.1007/s12040-014-0418-z

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.