A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic
International audience The western European kinematic evolution results from the opening of the western Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological evidence shows that the Iberian domain recorded the propagation of these two oceanic systems well and is the...
Published in: | Solid Earth |
---|---|
Main Authors: | , , , |
Other Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2020
|
Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296/document https://hal.archives-ouvertes.fr/hal-03106296/file/se-11-1313-2020.pdf https://doi.org/10.5194/se-11-1313-2020 |
id |
ftccsdartic:oai:HAL:hal-03106296v1 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU]Sciences of the Universe [physics] |
spellingShingle |
[SDU]Sciences of the Universe [physics] Angrand, Paul Mouthereau, Frédéric Masini, Emmanuel Asti, Riccardo A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
International audience The western European kinematic evolution results from the opening of the western Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological evidence shows that the Iberian domain recorded the propagation of these two oceanic systems well and is therefore a key to significantly advancing our understanding of the regional plate reconstructions. The late-Permian-Triassic Iberian rift basins have accommodated extension, but this tectonic stage is often neglected in most plate kinematic models, leading to the overestimation of the movements between Iberia and Europe during the subsequent Mesozoic (Early Cretaceous) rift phase. By compiling existing seismic profiles and geological constraints along the North Atlantic margins, including well data over Iberia, as well as recently published kinematic and paleogeographic reconstructions, we propose a coherent kinematic model of Iberia that accounts for both the Neotethyan and Atlantic evolutions. Our model shows that the Europe-Iberia plate boundary was a domain of distributed and oblique extension made of two rift systems in the Pyrenees and in the Iberian intra-continental basins. It differs from standard models that consider left-lateral strike-slip movement localized only in the northern Pyrenees in introducing a significant strike-slip movement south of the Ebro block. At a larger scale it emphasizes the role played by the late-Permian-Triassic rift and magmatism, as well as strike-slip faulting in the evolution of the western Neotethys Ocean and their control on the development of the Atlantic rift. |
author2 |
Géosciences Environnement Toulouse (GET) Centre National d'Études Spatiales Toulouse (CNES)-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Grenoble Alpes (UGA)-Université Gustave Eiffel-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) Géosciences Rennes (GR) Université de Rennes 1 (UR1) Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Centre National de la Recherche Scientifique (CNRS) Centre National de la Recherche Scientifique (CNRS-INSU)Centre National de la Recherche Scientifique (CNRS); French Geological Survey (BRGM); Total through the OROGEN project |
format |
Article in Journal/Newspaper |
author |
Angrand, Paul Mouthereau, Frédéric Masini, Emmanuel Asti, Riccardo |
author_facet |
Angrand, Paul Mouthereau, Frédéric Masini, Emmanuel Asti, Riccardo |
author_sort |
Angrand, Paul |
title |
A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
title_short |
A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
title_full |
A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
title_fullStr |
A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
title_full_unstemmed |
A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic |
title_sort |
reconstruction of iberia accounting for western tethys-north atlantic kinematics since the late-permian-triassic |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.archives-ouvertes.fr/hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296/document https://hal.archives-ouvertes.fr/hal-03106296/file/se-11-1313-2020.pdf https://doi.org/10.5194/se-11-1313-2020 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 1869-9510 EISSN: 1869-9529 Solid Earth https://hal.archives-ouvertes.fr/hal-03106296 Solid Earth, European Geosciences Union, 2020, 11 (4), pp.1313-1332. ⟨10.5194/se-11-1313-2020⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/se-11-1313-2020 hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296/document https://hal.archives-ouvertes.fr/hal-03106296/file/se-11-1313-2020.pdf doi:10.5194/se-11-1313-2020 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/se-11-1313-2020 |
container_title |
Solid Earth |
container_volume |
11 |
container_issue |
4 |
container_start_page |
1313 |
op_container_end_page |
1332 |
_version_ |
1766128887293542400 |
spelling |
ftccsdartic:oai:HAL:hal-03106296v1 2023-05-15T17:31:22+02:00 A reconstruction of Iberia accounting for Western Tethys-North Atlantic kinematics since the late-Permian-Triassic Angrand, Paul Mouthereau, Frédéric Masini, Emmanuel Asti, Riccardo Géosciences Environnement Toulouse (GET) Centre National d'Études Spatiales Toulouse (CNES)-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Grenoble Alpes (UGA)-Université Gustave Eiffel-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) Géosciences Rennes (GR) Université de Rennes 1 (UR1) Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Centre National de la Recherche Scientifique (CNRS) Centre National de la Recherche Scientifique (CNRS-INSU)Centre National de la Recherche Scientifique (CNRS); French Geological Survey (BRGM); Total through the OROGEN project 2020 https://hal.archives-ouvertes.fr/hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296/document https://hal.archives-ouvertes.fr/hal-03106296/file/se-11-1313-2020.pdf https://doi.org/10.5194/se-11-1313-2020 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/se-11-1313-2020 hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296 https://hal.archives-ouvertes.fr/hal-03106296/document https://hal.archives-ouvertes.fr/hal-03106296/file/se-11-1313-2020.pdf doi:10.5194/se-11-1313-2020 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1869-9510 EISSN: 1869-9529 Solid Earth https://hal.archives-ouvertes.fr/hal-03106296 Solid Earth, European Geosciences Union, 2020, 11 (4), pp.1313-1332. ⟨10.5194/se-11-1313-2020⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2020 ftccsdartic https://doi.org/10.5194/se-11-1313-2020 2021-04-10T22:27:08Z International audience The western European kinematic evolution results from the opening of the western Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological evidence shows that the Iberian domain recorded the propagation of these two oceanic systems well and is therefore a key to significantly advancing our understanding of the regional plate reconstructions. The late-Permian-Triassic Iberian rift basins have accommodated extension, but this tectonic stage is often neglected in most plate kinematic models, leading to the overestimation of the movements between Iberia and Europe during the subsequent Mesozoic (Early Cretaceous) rift phase. By compiling existing seismic profiles and geological constraints along the North Atlantic margins, including well data over Iberia, as well as recently published kinematic and paleogeographic reconstructions, we propose a coherent kinematic model of Iberia that accounts for both the Neotethyan and Atlantic evolutions. Our model shows that the Europe-Iberia plate boundary was a domain of distributed and oblique extension made of two rift systems in the Pyrenees and in the Iberian intra-continental basins. It differs from standard models that consider left-lateral strike-slip movement localized only in the northern Pyrenees in introducing a significant strike-slip movement south of the Ebro block. At a larger scale it emphasizes the role played by the late-Permian-Triassic rift and magmatism, as well as strike-slip faulting in the evolution of the western Neotethys Ocean and their control on the development of the Atlantic rift. Article in Journal/Newspaper North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Solid Earth 11 4 1313 1332 |