2001
DOI: 10.1306/8626c7cb-173b-11d7-8645000102c1865d
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Improved identification of pay zones through integration of geochemical and log data: A case study from Upper Assam basin, India

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Cited by 8 publications
(2 citation statements)
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“…The basin evolved as a passive margin platform with a history of the extension and normal faulting (Kent & Dasgupta, 2004; Mathur et al, 2001; Murty, 1984). The convergence of the Indian Plate and the Eurasian Plate, along with the collision by the Burmese Plate, endorsed intense flexure and complex structure in the central basement of the Upper Assam Basin, generating several basement highs and lows (Borgohain et al, 2017; Kumar et al, 2023) (Figure 1).…”
Section: Discussionmentioning
confidence: 99%
“…The basin evolved as a passive margin platform with a history of the extension and normal faulting (Kent & Dasgupta, 2004; Mathur et al, 2001; Murty, 1984). The convergence of the Indian Plate and the Eurasian Plate, along with the collision by the Burmese Plate, endorsed intense flexure and complex structure in the central basement of the Upper Assam Basin, generating several basement highs and lows (Borgohain et al, 2017; Kumar et al, 2023) (Figure 1).…”
Section: Discussionmentioning
confidence: 99%
“…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).…”
Section: Geological Settings Of the Basinmentioning
confidence: 99%