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Palynological Delimitation of the Coal Bearing Lower Gondwana Sediments in the Southern Part of Tatapani-Ramkola Coalfield, Chattisgarh, India


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1 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow-226007, India
     

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Coal and carbonaceous shale samples from bore-hole TRSS-1, located in the southern part of Tatapani Ramkola Coalfield have been palynologically analysed. Surface sediments exposed in the vicinity of the bore-hole, along Suknaiya nala, were also examined to ascertain their stratigraphic position vis-a-vis the bor' "oIe sediments. On the basis of quantitative dominance, three assemblage zones have been distinguished. which in ascending order are: (i) Parasaccites-Callumispora palynoassemblage zone, (ii) Scheuringipollenites maxim us palynoassemblage zone and (iii) Faunipollenites-Scheuringipollenites palynoassemblage zone. The first two assemblage zones have been demarcated in bore-hole TRSS-1 and represent Upper Karharbari and Lower Barakar palynozones respectively. The third assemblage zone has been recorded in Suknaiya nala and represents Upper Barakar palynozone.

Keywords

Palynology, Gondwana Sediments, Palynomorphs, Assemblage Zones, Tatapani-Ramkola Coalfield, Chattisgarh.
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  • Palynological Delimitation of the Coal Bearing Lower Gondwana Sediments in the Southern Part of Tatapani-Ramkola Coalfield, Chattisgarh, India

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Authors

Ratan kar
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow-226007, India
Suresh C. Srivastava
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow-226007, India

Abstract


Coal and carbonaceous shale samples from bore-hole TRSS-1, located in the southern part of Tatapani Ramkola Coalfield have been palynologically analysed. Surface sediments exposed in the vicinity of the bore-hole, along Suknaiya nala, were also examined to ascertain their stratigraphic position vis-a-vis the bor' "oIe sediments. On the basis of quantitative dominance, three assemblage zones have been distinguished. which in ascending order are: (i) Parasaccites-Callumispora palynoassemblage zone, (ii) Scheuringipollenites maxim us palynoassemblage zone and (iii) Faunipollenites-Scheuringipollenites palynoassemblage zone. The first two assemblage zones have been demarcated in bore-hole TRSS-1 and represent Upper Karharbari and Lower Barakar palynozones respectively. The third assemblage zone has been recorded in Suknaiya nala and represents Upper Barakar palynozone.

Keywords


Palynology, Gondwana Sediments, Palynomorphs, Assemblage Zones, Tatapani-Ramkola Coalfield, Chattisgarh.