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Assessment of Thermal Maturity, Source Rock Potential and Paleodepositional Environment of the Paleogene Lignites in Barsingsar, Bikaner–Nagaur Basin, Western Rajasthan, India

  • Alok K. SinghEmail author
  • Alok Kumar
Original Paper
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Abstract

Investigations on the Paleogene lignites were carried out through geochemical, mineralogical and petrographic analyses to assess their paleodepositional environment, source rock potential and thermal maturity. The samples were collected from the Barsingsar lignite mines in the Bikaner–Nagaur Basin, Western Rajasthan, India. Huminite reflectance assigns these samples as lignite (low-rank coal). Barsingsar lignites are dominated by the huminite maceral group, while inertinites and liptinites occur in subordinated amount. The mineral matter is dominated by carbonates, pyrite and argillaceous (in descending order). Gelification index, tissue preservation index, groundwater index and vegetation index indicate the prevalence of a dry forest swamp having ombrotrophic to mesotrophic conditions in the paleomire. Rock–Eval pyrolysis indicates high hydrogen index relative to oxygen index and excellent hydrocarbon potential. The Barsingsar lignites are characterized by mixed type III and type II kerogens, which are thermally immature. Several minerals like quartz, coesite, siderite, aragonite and rutile minerals have been identified by XRD analysis, whereas selected trace elements primarily Sr, Zr, Cu, Pb, Zn, Cr, V, Ni, Rb and Co were also detected. Fourier-transform infrared spectroscopy pattern shows the dominance of clay minerals and the presence of aromatic, aliphatic and some oxygen functional groups in these lignites.

Keywords

Bikaner–Nagaur Barsingsar lignite Petrography Geochemistry Paleoenvironment Thermal maturity 

Notes

Acknowledgments

The authors graciously acknowledge the support and are thankful to the Director of RGIPT for allowing the use of existing research facilities. They also most graciously acknowledge the support in sample collection provided by the officials of the Neyveli Lignite Corporation posted at Barsingsar lignite mines. The funding has come from Project No. SB/S4/ES-681/2013 sanctioned by the Department of Science & Technology, Government of India, for which the authors are grateful. Authors express their sincere gratitude to Editor-in-Chief of Natural Resources Research for considering our manuscript for the publication. Authors also thank the two anonymous reviewers for their comments and suggestions on the manuscript, which have improved the work presented in the new submission.

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© International Association for Mathematical Geosciences 2019

Authors and Affiliations

  1. 1.Department of Petroleum Engineering and Geological ScienceRajiv Gandhi Institute of Petroleum TechnologyJais, AmethiIndia

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