Petrography and geochemistry of the Upper Cretaceous Gryphaea Limestones, Kallankurichi Formation, Ariyalur Group, Trichinopoly, Southern India: Implication for palaeoenvironment

Authors

  • M Senthiappan PG and Research Department of Geology, VO Chidambaram College,Thoothukudi
  • V. Stephen Pitchaimani Department of Geology, V.O. Chidambaram College, Thoothukudi, Tamil Nadu, India
  • A.V. Udayanapillai Department of Geology & Quantum Material Research Laboratory, Department of Nano-Science & Technology, Alagappa University, Karaikudi, Tamil Nadu, India
  • Perumal Velmayil Department of Geology & Quantum Material Research Laboratory, Department of Nano-Science & Technology, Alagappa University, Karaikudi, Tamil Nadu, India
  • Bangarupriyanga Sundaram Department of Geology & Quantum Material Research Laboratory, Department of Nano-Science & Technology, Alagappa University, Karaikudi, Tamil Nadu, India
  • G. Ramalingam Department of Geology & Quantum Material Research Laboratory, Department of Nano-Science & Technology, Alagappa University, Karaikudi
  • John S Armstrong Altrin Unidad de Procesos Oceánicos Y Costeros, Universidad Nacional Autónoma de México, Instituto de Ciencias del MarYLimnología, Unidad de ProcesosOceánicos Y Costeros, Ciudad Universitaria, Mexico City, Mexico

DOI:

https://doi.org/10.51710/jias.v40iII.309

Abstract

Sub-surface Kallankurichi gryphaea limestone formation is observed between Archaean and Quaternary outcrops.  Petrographic observation reveals that mega fossils are absent and it contains abundant skeletal fragments of pelecypods, gastropods, foraminifera, bryozoa, and symbiotic algae. X-ray diffraction (XRD) analyses reveal the mineralogical components of both carbonate and clay minerals. Carbonate minerals include calcite, siderite, witherite, malachite, smithsonite, and rhodochrosite. Clay minerals detected are kaolin, montmorillonite, and palygorskite. Major element composition represents predominance of CaO, SiO2, Al2O3, and Fe2O3 oxides, while MgO, MnO, Na2O, K2O, TiO2, and P2O5 oxides are depleted. Statistical analyses of correlation coefficient, principal component analysis, and cluster analysis represent the geochemical affinities and aerial distribution similarities among major elements. Palaeoclimate inferred through biotic proxies, major element geochemistry, and clay minerals represents arid and semi-arid climate.

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Published

2023-12-31

How to Cite

Senthiappan, M., V. Stephen Pitchaimani, A.V. Udayanapillai, Perumal Velmayil, Bangarupriyanga Sundaram, G. Ramalingam, & Armstrong Altrin, J. S. (2023). Petrography and geochemistry of the Upper Cretaceous Gryphaea Limestones, Kallankurichi Formation, Ariyalur Group, Trichinopoly, Southern India: Implication for palaeoenvironment. Journal of The Indian Association of Sedimentologists (peer Reviewed), 40(II), 14–26. https://doi.org/10.51710/jias.v40iII.309
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