Solid Earth
Solid Earth
SE
Articles | Volume 11, issue 4
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.
https://doi.org/10.5194/se-11-1313-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 11, issue 4
Short communication
 | 
21 Jul 2020
Short communication |  | 21 Jul 2020

A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic

Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti

Viewed

Total article views: 6,095 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,730 1,265 100 6,095 225 108 134
  • HTML: 4,730
  • PDF: 1,265
  • XML: 100
  • Total: 6,095
  • Supplement: 225
  • BibTeX: 108
  • EndNote: 134
Views and downloads (calculated since 06 Mar 2020)
Cumulative views and downloads (calculated since 06 Mar 2020)

Viewed (geographical distribution)

Total article views: 6,095 (including HTML, PDF, and XML) Thereof 5,482 with geography defined and 613 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 15 Nov 2025
Download
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.
Read more
Share