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The Deccan Trapps (India) and Cretaceous-Tertiary boundary events

  • Cretaceous/Tertiary Boundary
  • Conference paper
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Global Bio-Events

Abstract

It has been suggested that the eruption of the Deccan Trapps has contributed to the events of the Cretaceous-Tertiary transition as a possible cause of Iridium enrichment and/or other physicochemical disturbances. However, no precise chronological framework was available for the emplacement of these Trapps, which form one of the largest known occurrences of continental basalt flows. A joint Indian-French project, still under way, is providing more accurate informations about the chronology of the Deccan Trapps and its possible implications for Cretaceous-Tertiary boundary events.

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References

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Otto H. Walliser Prof. Dr.

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© 1986 Springer-Verlag

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Besse, J. et al. (1986). The Deccan Trapps (India) and Cretaceous-Tertiary boundary events. In: Walliser, O.H. (eds) Global Bio-Events. Lecture Notes in Earth Sciences, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0010219

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  • DOI: https://doi.org/10.1007/BFb0010219

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  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-17180-5

  • Online ISBN: 978-3-540-47244-5

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