Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1313-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-1313-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
Paul Angrand
CORRESPONDING AUTHOR
Geosciences Environnement Toulouse (GET), Université de Toulouse, UPS, Univ. Paul Sabatier, CNRS, IRD, 14 av. Edouard Belin, 31400 Toulouse, France
Frédéric Mouthereau
Geosciences Environnement Toulouse (GET), Université de Toulouse, UPS, Univ. Paul Sabatier, CNRS, IRD, 14 av. Edouard Belin, 31400 Toulouse, France
Emmanuel Masini
M&U sas, 38120 Saint-Égrève, France
ISTerre, Université Grenoble Alpes, 38000 Grenoble, France
Riccardo Asti
Université de Rennes, CNRS, Géosciences Rennes‐UMR 6118, 35000 Rennes, France
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- Reconstructing the Iberian Salt‐Bearing Rifted Margin of the Southern Pyrenees: Insights From the Organyà Basin G. Casini et al. 10.1029/2022TC007715
- Late Palaeozoic tectonics in Central Mediterranean: a reappraisal G. Molli et al. 10.1186/s00015-020-00375-1
Latest update: 01 Nov 2024
Short summary
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time...