EGU22-4194
https://doi.org/10.5194/egusphere-egu22-4194
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Paleocene stage boundaries and hyperthermal events (Wadi Nukhul and Gebel El Beida, Egypt): a possible link to global volcanism

Hassan Khozyem1,2, Abdullah Mahmoud1, Thierry Adatte2, Gerta Keller3, and Jorge Spangenberg4
Hassan Khozyem et al.
  • 1Department of Geology, Faculty of Sciences, Aswan University, Aswan, Egypt (ammma12691@aswu.edu.eg)
  • 2Institute of Earth Sciences (ISTE), University of Lausanne, 1015 Lausanne, Switzerland (thierry.adatte@unil.ch)
  • 3Department of Geosciences, Princeton University, Princeton, NJ 08544, USA (gkeller@princeton.edu)
  • 4Institute of Earth Surface Dynamics (IDYST), University of Lausanne, Switzerland, 1015 Lausanne, Switzerland (Jorge.Spangenberg@unil.ch)

How to cite: Khozyem, H., Mahmoud, A., Adatte, T., Keller, G., and Spangenberg, J.: Paleocene stage boundaries and hyperthermal events (Wadi Nukhul and Gebel El Beida, Egypt): a possible link to global volcanism, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-4194, https://doi.org/10.5194/egusphere-egu22-4194, 2022.

This abstract has been withdrawn on 17 May 2022.