Early Permian transgressive–regressive cycles: Sequence stratigraphic reappraisal of the coal-bearing Barakar Formation, Raniganj Basin, India

  • Biplab Bhattacharya
  • Joyeeta Bhattacharjee
  • Sandip Bandyopadhyay
  • Sudipto Banerjee
  • Kalyan Adhikari


The present research is an attempt to assess the Barakar Formation of the Raniganj Gondwana Basin, India, in the frame of fluvio-marine (estuarine) depositional systems using sequence stratigraphic elements. Analysis of predominant facies associations signify deposition in three sub-environments: (i) a river-dominated bay-head delta zone in the inner estuary, with transition from braided fluvial channels (FA-B1) to tide-affected meandering fluvial channels and flood plains (FA-B2) in the basal part of the succession; (ii) a mixed energy central basin zone, which consists of transitional fluvio-tidal channels (FA-B2), tidal flats, associated with tidal channels and bars (FA-B3) in the middle-upper part of the succession; and (iii) a wave-dominated outer estuary (coastal) zone (FA-B4 with FA-B3) in the upper part of the succession. Stacked progradational (P1, P2)–retrogradational (R1, R2) successions attest to one major base level fluctuation, leading to distinct transgressive–regressive (T–R) cycles with development of initial falling stage systems tract (FSST), followed by lowstand systems tract (LST) and successive transgressive systems tracts (TST-1 and TST-2). Shift in the depositional regime from regressive to transgressive estuarine system in the early Permian Barakar Formation is attributed to change in accommodation space caused by mutual interactions of (i) base level fluctuations in response to climatic amelioration and (ii) basinal tectonisms (exhumation/sagging) related to post-glacial isostatic adjustments in the riftogenic Gondwana basins.


Fluvio-marine estuary post-glacial transgression sequence stratigraphy Permian Gondwana 



Authors are grateful to the Mine Authorities of Ramnagar–Chapatoria open pit mines for necessary permissions to visit the mines. B Bhattacharya received financial support from Department of Science and Technology (DST)-SERB in the form of FAST TRACK Research Project (No. SR/FTP/ES-170/2010) for this work. All the authors acknowledge their respective departments for the infrastructural help. Authors are also thankful to both the reviewers for constructive suggestions, which enhanced the clarity of the paper.


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© Indian Academy of Sciences 2018

Authors and Affiliations

  • Biplab Bhattacharya
    • 1
  • Joyeeta Bhattacharjee
    • 1
  • Sandip Bandyopadhyay
    • 2
  • Sudipto Banerjee
    • 2
    • 3
  • Kalyan Adhikari
    • 3
  1. 1.Department of Earth SciencesIndian Institute of TechnologyRoorkeeIndia
  2. 2.Department of GeologyHooghly Mohsin CollegeChinsurah, HooghlyIndia
  3. 3.Department of Earth and Environmental StudiesNational Institute of TechnologyDurgapurIndia

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