Geochemistry of coal–bearing Permo−Triassic strata in Allan Hills, South Victoria Land, Antarctica: Implications for palaeoclimate

Authors

  • Sundeep K. Pandita Department of Geology, University of Jammu, Jammu 180006, India
  • N.S. Siddaiah Department of Environmental Science, Jawahar Lal Nehru University, New Delhi 110016, India
  • Rajni Tewari C–38, Alkapuri, Sector C, Aliganj, Lucknow 226 024, India
  • Sankar Chatterjee Texas Tech University, Lubbock, Texas, USA
  • Deepa Agnihotri Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India

DOI:

https://doi.org/10.54991/jop.2018.50

Keywords:

Geochemistry, Permian, Triassic, Allan Hills, Antarctica

Abstract

Major, trace and rare earth element (REE) geochemistry has been carried out in this paper to characterize source–rock weathering and climatic variability of the late Permian Weller Formation and the late Triassic Lashly Formation of Gondwana sequences which have yielded rich record of plant mega–and micro fossils associated with coal beds in post–glacial conditions in Allan Hills of South Victoria Land, Antarctica. The geochemistry suggests dominantly a felsic provenance with a volcanogenic input and role of weathering and hydrothermal alteration. The palaeoclimatic interpretation derived from geochemical analysis indicates warm, temperate and humid conditions during the late Permian, and warm and humid conditions during the late Triassic.

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Published

2018-12-31

How to Cite

Pandita, S. K., Siddaiah, N., Tewari, R., Chatterjee, S., & Agnihotri, D. (2018). Geochemistry of coal–bearing Permo−Triassic strata in Allan Hills, South Victoria Land, Antarctica: Implications for palaeoclimate. Journal of Palaeosciences, 67((1-2), 89–97. https://doi.org/10.54991/jop.2018.50

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