Oblique continental rifting. Insights from 3-D forward geodynamic modelling coupled with surface processes and application to the Equatorial passive margins formation.

Ritske S. Huismans; Thomas Theunissen; Delphine Rouby; Sebastian G. Wolf; Dave May

doi:https://doi.org/10.5194/egusphere-egu22-9052

[Back] [Session TS6.1]

EGU22-9052

https://doi.org/10.5194/egusphere-egu22-9052

EGU General Assembly 2022

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

Oblique continental rifting. Insights from 3-D forward geodynamic modelling coupled with surface processes and application to the Equatorial passive margins formation.

Ritske S. Huismans¹, Thomas Theunissen¹, Delphine Rouby², Sebastian G. Wolf¹, and Dave May³

Ritske S. Huismans et al.

¹Bergen University, Earth Sciences, Bergen, Norway (ritske.huismans@geo.uib.no)
²GET, Université de Toulouse, CNRS, IRD, UPS, Toulouse, France
³Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography, UC San Diego

How to cite: Huismans, R. S., Theunissen, T., Rouby, D., Wolf, S. G., and May, D.: Oblique continental rifting. Insights from 3-D forward geodynamic modelling coupled with surface processes and application to the Equatorial passive margins formation., EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9052, https://doi.org/10.5194/egusphere-egu22-9052, 2022.

This abstract has been withdrawn on 16 May 2022.