Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins
International audience The North Pyrenean Zone (NPZ) belongs to the northern flank of the Pyrenean chain and continuously outcrops to the north of the AZ from Perpignan to the Basque Country. It is essentially composed of Mesozoic sediments associated with Paleozoic basement massifs (North Pyrenean...
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ftunivrennes2hal:oai:HAL:insu-03690603v1 2024-02-11T10:05:57+01:00 Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins Lagabrielle, Yves Géosciences Rennes (GR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS) 2022 https://insu.hal.science/insu-03690603 https://doi.org/10.1002/9781119986959.ch9 en eng HAL CCSD Wiley info:eu-repo/semantics/altIdentifier/doi/10.1002/9781119986959.ch9 ISBN: 9781789450620 insu-03690603 https://insu.hal.science/insu-03690603 doi:10.1002/9781119986959.ch9 Continental Rifted Margins 2: Case Examples https://insu.hal.science/insu-03690603 Continental Rifted Margins 2: Case Examples, 1, Wiley, pp.203-234, 2022, 9781789450620. ⟨10.1002/9781119986959.ch9⟩ [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics info:eu-repo/semantics/bookPart Book sections 2022 ftunivrennes2hal https://doi.org/10.1002/9781119986959.ch9 2024-01-23T23:47:52Z International audience The North Pyrenean Zone (NPZ) belongs to the northern flank of the Pyrenean chain and continuously outcrops to the north of the AZ from Perpignan to the Basque Country. It is essentially composed of Mesozoic sediments associated with Paleozoic basement massifs (North Pyrenean massifs) and results from the inversion and northward thrusting of the basins formed during the Cretaceous rifting phase. The geology of the NPZ is unique in the world and of major interest for the study of the formation of passive continental margins and, in particular, for better constraining the thermal conditions of crustal thinning. The NPZ is the result of the inversion of extensional and transcurrent structures distributed along the Iberian–Eurasian plate boundary. Along the Iberia–Eurasia boundary itself, the Basque–Cantabrian basin was connected to the North Pyrenean basins (future NPZ). The evolution of the Pyrenean smooth-slope basins contrasts with brittle-dominated models of crustal thinnings, as exemplified along the Iberian–Newfoundland passive margins. Book Part Newfoundland Archive Ouverte de l'Université Rennes (HAL) 203 234 |
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Archive Ouverte de l'Université Rennes (HAL) |
op_collection_id |
ftunivrennes2hal |
language |
English |
topic |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
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[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics Lagabrielle, Yves Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
topic_facet |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
description |
International audience The North Pyrenean Zone (NPZ) belongs to the northern flank of the Pyrenean chain and continuously outcrops to the north of the AZ from Perpignan to the Basque Country. It is essentially composed of Mesozoic sediments associated with Paleozoic basement massifs (North Pyrenean massifs) and results from the inversion and northward thrusting of the basins formed during the Cretaceous rifting phase. The geology of the NPZ is unique in the world and of major interest for the study of the formation of passive continental margins and, in particular, for better constraining the thermal conditions of crustal thinning. The NPZ is the result of the inversion of extensional and transcurrent structures distributed along the Iberian–Eurasian plate boundary. Along the Iberia–Eurasia boundary itself, the Basque–Cantabrian basin was connected to the North Pyrenean basins (future NPZ). The evolution of the Pyrenean smooth-slope basins contrasts with brittle-dominated models of crustal thinnings, as exemplified along the Iberian–Newfoundland passive margins. |
author2 |
Géosciences Rennes (GR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS) |
format |
Book Part |
author |
Lagabrielle, Yves |
author_facet |
Lagabrielle, Yves |
author_sort |
Lagabrielle, Yves |
title |
Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
title_short |
Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
title_full |
Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
title_fullStr |
Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
title_full_unstemmed |
Chapter 9 Cretaceous Rifting at the Pyrenean Iberia-Eurasia Border: Crustal Thinning under a Pre-rift Cover - Application to Passive Margins |
title_sort |
chapter 9 cretaceous rifting at the pyrenean iberia-eurasia border: crustal thinning under a pre-rift cover - application to passive margins |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://insu.hal.science/insu-03690603 https://doi.org/10.1002/9781119986959.ch9 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Continental Rifted Margins 2: Case Examples https://insu.hal.science/insu-03690603 Continental Rifted Margins 2: Case Examples, 1, Wiley, pp.203-234, 2022, 9781789450620. ⟨10.1002/9781119986959.ch9⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/9781119986959.ch9 ISBN: 9781789450620 insu-03690603 https://insu.hal.science/insu-03690603 doi:10.1002/9781119986959.ch9 |
op_doi |
https://doi.org/10.1002/9781119986959.ch9 |
container_start_page |
203 |
op_container_end_page |
234 |
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1790603307795873792 |