Transition from Aegean back-arc extension to Corinth rifting. Miocene to Pleistocene interacting extensional regimes of the Northern Peloponnese.

Vincent Wicker; Mary Ford; Robert Gawthorpe; Haralambos Kranis; Emmanuel Skourtsos; Pierre Bouilhol; Martin Muravchik; Natacha Fabregas; Kévin Beaufumé; Hugo Beldame

doi:https://doi.org/10.5194/egusphere-egu22-9434

[Back] [Session TS6.3]

EGU22-9434

https://doi.org/10.5194/egusphere-egu22-9434

EGU General Assembly 2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Transition from Aegean back-arc extension to Corinth rifting. Miocene to Pleistocene interacting extensional regimes of the Northern Peloponnese.

Vincent Wicker¹, Mary Ford¹, Robert Gawthorpe², Haralambos Kranis³, Emmanuel Skourtsos³, Pierre Bouilhol¹, Martin Muravchik², Natacha Fabregas², Kévin Beaufumé⁴, and Hugo Beldame⁵

Vincent Wicker et al.

¹CRPG-CNRS, Université de Lorraine, Nancy, France (vincent.wicker@gmail.com)
²University of Bergen, Norway
³National and Kapodistrian University of Athens, Greece
⁴Perenco, UK
⁵ENSG Nancy, University of Lorraine, France

How to cite: Wicker, V., Ford, M., Gawthorpe, R., Kranis, H., Skourtsos, E., Bouilhol, P., Muravchik, M., Fabregas, N., Beaufumé, K., and Beldame, H.: Transition from Aegean back-arc extension to Corinth rifting. Miocene to Pleistocene interacting extensional regimes of the Northern Peloponnese. , EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9434, https://doi.org/10.5194/egusphere-egu22-9434, 2022.

This abstract has been withdrawn on 04 May 2022.