Palynology of the Talchir Formation from Betul Coalfield, Satpura Basin, India

Authors

  • S.C. Srivastava Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow 226007, India
  • Anand-Prakash Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow 226007, India
  • O.S. Sarate Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow 226007, India

DOI:

https://doi.org/10.54991/jop.1988.1601

Keywords:

Palynology, Betul Coalfield, Talchir Formation, Satpura Basin (India)

Abstract

The palynoflora recovered from the sediments of Talchir Formation of Mura Kuppa area in Betul Coalfield, Satpura Basin is rich in Plicatipollenites, followed by Parasaccites and Virkkipollenites, Potonieisporites and Rugasaccites occur consistently but in low percentages. This palynoflora is closely comparable with the known older palynofloras of the Talchir Formation of India.

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References

Bharadwaj DC & Anand-Prakash 1972. Geology and palynostratigraphy of Lower Gondwana Formation in Mohpani Coalfield, Madhya Pradesh, India. Geophytology 1(2): 103-115.

Bharadwaj DC, Navale GKB & Anand-Prakash 1974. Palynostratigraphy and petrology of Lower Gondwana coals in Pench-Kanhan Coalfield, Satpura Gondwana Basin, M. P., India. Geophytology 4(1): 7-24.

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Published

1988-12-31

How to Cite

Srivastava, S., Anand-Prakash, & Sarate, O. (1988). Palynology of the Talchir Formation from Betul Coalfield, Satpura Basin, India. Journal of Palaeosciences, 37((1-3), 81–84. https://doi.org/10.54991/jop.1988.1601

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