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Sökning: id:"swepub:oai:DiVA.org:oru-79880" > Multi-proxy approac...

Multi-proxy approach on the hydrocarbon generation perspective of Barjora Basin, India

Misra, Satabdi (författare)
Coal Geology and Organic Petrology Lab, Department of Applied Geology, Indian Institute of Technology (Indian School of Mines), Dhanbad, Jharkhand, India
Das, Supriyo Kumar (författare)
Department of Geology, Presidency University, Kolkata, West Bengal, India
Varma, Atul Kumar (författare)
Coal Geology and Organic Petrology Lab, Department of Applied Geology, Indian Institute of Technology (Indian School of Mines), Dhanbad, Jharkhand, India
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Mani, Devleena (författare)
Centre for Earth, Ocean and Atmospheric Sciences, University of Hyderabad, Telengana, India
Kalpana, M. S. (författare)
National Geophysical Research Institute, Hyderabad, Telengana, India
Ekblad, Alf, 1957- (författare)
Örebro universitet,Institutionen för naturvetenskap och teknik
Biswas, Sanki (författare)
Coal Geology and Organic Petrology Lab, Department of Applied Geology, Indian Institute of Technology (Indian School of Mines), Dhanbad, Jharkhand, India
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 (creator_code:org_t)
Elsevier, 2020
2020
Engelska.
Ingår i: Marine and Petroleum Geology. - : Elsevier. - 0264-8172 .- 1873-4073. ; 112
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Barjora Basin in India is a small basin characterized by a high organic richness of early mature nature. The present study aims to find the source of organic matter (OM) and hydrocarbon generation potential of Barjora Basin. Systematically collected coal and shale samples from R-II seam of the basin were used for proximate and ultimate analyses, Rock Eval pyrolysis along with total organic carbon (TOC) content, organo-micropetrographic framework, thermal maturity, carbon isotopic signature, biomarker composition, functional group studies and estimation of relative aliphaticity and aromaticity through Fourier Transform infrared spectroscopy (FTIR). The novelty of the present work lies in the application of multiple proxies such as stable isotope ratio of organic carbon (delta C-13), biomarker signatures, thermal maturity parameters, organo-micropetrography and estimation and quantification of functional groups for palaeoenvironmental reconstruction and to assess the hydrocarbon productivity of the basin. A dominant terrestrial OM input in Barjora Basin is indicated by the TOC to total nitrogen ratio (C/N), delta C-13 and biomarker compositions. High gelification index (GI), tissue preservation index (TPI), and carbon preference index (CPI) values indicate that coals are deposited in wet swamp forest regime under high rainwater conditions and shales are formed in upper delta plain regime under high groundwater activity. In addition, large liptinite content, TPI and GI designate short transportation of the OM before burial leading to organic richness of the Barjora Basin. Moreover, high liptinite content, type II-III admixed kerogen input, S-2/S-3 ratio, TPI and index for hydrocarbon generation (I-HG) signify higher potential of the basin for hydrocarbon generation.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Nyckelord

Stable isotope
Biomarker
Rock Eval pyrolysis
Organo-micropetrographic constituents
Hydrocarbon generation potential
Palaeoenvironmental reconstruction
Gondwana organic sediments
Barjora Basin India

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