EGU25-1131, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-1131
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Stress-induced permeability anisotropy and fluid flow dynamics in a Mesozoic fractured carbonate aquifer of southern Italy
Ian Bala Abdallah1, Cathy Hollis2, David Healy3, Jeffrey De'Haven Hyman4, Giacomo Prosser1, and Fabrizio Agosta
Ian Bala Abdallah et al.
  • 1University of Basilicata, Sciences, Geosciences, Potenza, Italy (ian.abdallah@unibas.it)
  • 2The Department of earth and environmental sciences, University of Manchester, UK.
  • 3Geosolutions, University of Leeds, UK.
  • 4Computational Earth Science Group (EES‐16), Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA.

How to cite: Abdallah, I. B., Hollis, C., Healy, D., Hyman, J. D., Prosser, G., and Agosta, F.: Stress-induced permeability anisotropy and fluid flow dynamics in a Mesozoic fractured carbonate aquifer of southern Italy, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-1131, https://doi.org/10.5194/egusphere-egu25-1131, 2025.

This abstract has been withdrawn on 23 Apr 2025.