Subduction of active spreading ridges and the disappearance of Andean-type cordilleras

We address the possible link between the age of subducting oceanic lithosphere and growth of elevated cordilleras versus extension-dominated arc regions. Singularity exists in South America: the lowest elevated Andean segments are found in Patagonia where the active Chile Ridge enters the trench. Su...

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Main Authors: Scalabrino, Bruno, Lagabrielle, Yves, Faccenna, Claudio
Format: Article
Language:English
Published: Académie des sciences 2024-03-01
Series:Comptes Rendus. Géoscience
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Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.250/
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author Scalabrino, Bruno
Lagabrielle, Yves
Faccenna, Claudio
author_facet Scalabrino, Bruno
Lagabrielle, Yves
Faccenna, Claudio
author_sort Scalabrino, Bruno
collection DOAJ
description We address the possible link between the age of subducting oceanic lithosphere and growth of elevated cordilleras versus extension-dominated arc regions. Singularity exists in South America: the lowest elevated Andean segments are found in Patagonia where the active Chile Ridge enters the trench. Subduction of active ridge triggers thermal doming, crustal extension and attenuation of former cordilleras. At the Antarctica–South America connection, three active ridge subductions induced the disruption of a former continuous cordillera during the opening of Drake Passage. Active ridge subduction induces lithosphere thermal erosion and related crustal extension in the upper plate. Evolution of regions worldwide experiencing ridge subduction confirms this hypothesis.
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publisher Académie des sciences
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spelling doaj-art-478d9103852045a0a2a93200be0ad0052025-02-07T10:41:48ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252024-03-01356S27911410.5802/crgeos.25010.5802/crgeos.250Subduction of active spreading ridges and the disappearance of Andean-type cordillerasScalabrino, Bruno0Lagabrielle, Yves1Faccenna, Claudio2Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, 250 rue Albert Einstein, Sophia Antipolis 06560 Valbonne, France35 Allée du Pargo, 56000 Vannes, FranceDepartement of Science, Roma Tre University, Roma, Italy; GFZ, German Research Center for Geoscience, GermanyWe address the possible link between the age of subducting oceanic lithosphere and growth of elevated cordilleras versus extension-dominated arc regions. Singularity exists in South America: the lowest elevated Andean segments are found in Patagonia where the active Chile Ridge enters the trench. Subduction of active ridge triggers thermal doming, crustal extension and attenuation of former cordilleras. At the Antarctica–South America connection, three active ridge subductions induced the disruption of a former continuous cordillera during the opening of Drake Passage. Active ridge subduction induces lithosphere thermal erosion and related crustal extension in the upper plate. Evolution of regions worldwide experiencing ridge subduction confirms this hypothesis.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.250/CordillerasActive spreading subductionSlab windowExtensional tectonicsAttenuation
spellingShingle Scalabrino, Bruno
Lagabrielle, Yves
Faccenna, Claudio
Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
Comptes Rendus. Géoscience
Cordilleras
Active spreading subduction
Slab window
Extensional tectonics
Attenuation
title Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
title_full Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
title_fullStr Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
title_full_unstemmed Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
title_short Subduction of active spreading ridges and the disappearance of Andean-type cordilleras
title_sort subduction of active spreading ridges and the disappearance of andean type cordilleras
topic Cordilleras
Active spreading subduction
Slab window
Extensional tectonics
Attenuation
url https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.250/
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