“…The overburden Palaeogene–Neogene–Quaternary deposits comprise of the Lakadong, Prang and Narpuh Formations (Palaeocene to Mid‐Eocene), Kopili Formation (Upper Eocene), Barail Formation (Oligocene), Tipam and Girujan Formations (Miocene), Namsang and Dhekiajuli Formations (Pliocene to Pleistocene) and the alluvium cover (Pleistocene to Recent). The lithological composition of these deposits consists of limestone, alternate shale‐coal, intercalated sands, sandstone and thick alluvium cover (Mandal & Dasgupta, 2013; Mathur et al, 2001; Sahoo & Gogoi, 2009; Sahoo & Gogoi, 2011; Wandrey, 2004). The Oligocene to Upper Miocene period witnessed southward tilt of the basin (Mandal & Dasgupta, 2013; Nandy, 2017).…”