The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction

The Amirante Ridge and Trench System forms a 600-km-long arcuate structure in the Mascarene Basin (Indian Ocean), whose origin remains enigmatic. Here, I provide a paleogeographic reconstruction of the NW India margin for the Late Cretaceous–Paleocene interval, compiling information from ophiolites...

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Main Author: Rodriguez, Mathieu
Format: Article
Language:English
Published: Académie des sciences 2020-12-01
Series:Comptes Rendus. Géoscience
Subjects:
Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.40/
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author Rodriguez, Mathieu
author_facet Rodriguez, Mathieu
author_sort Rodriguez, Mathieu
collection DOAJ
description The Amirante Ridge and Trench System forms a 600-km-long arcuate structure in the Mascarene Basin (Indian Ocean), whose origin remains enigmatic. Here, I provide a paleogeographic reconstruction of the NW India margin for the Late Cretaceous–Paleocene interval, compiling information from ophiolites surrounding the Arabian Sea and data collected at sea. This reconstruction shows that the Amirante Ridge and Trench System constitutes the southern termination of a ${\sim }$1500-km-long subduction, which used to run along the NW Indian margin during the Late Cretaceous–Paleocene. The dislocation of the NW Indian subduction, recorded at the Amirante Ridge and Trench System and the Bela ophiolites, may have played a role in the plate reorganization event recorded at 73–63 Ma.
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spelling doaj.art-2798acf6bc994a29a217a25b38a0aaf82023-10-24T14:24:07ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252020-12-01352323524510.5802/crgeos.4010.5802/crgeos.40The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subductionRodriguez, Mathieu0Laboratoire de Géologie, Ecole normale supérieure, PSL research university, CNRS UMR 8538, 24 rue Lhomond, 75005 Paris, FranceThe Amirante Ridge and Trench System forms a 600-km-long arcuate structure in the Mascarene Basin (Indian Ocean), whose origin remains enigmatic. Here, I provide a paleogeographic reconstruction of the NW India margin for the Late Cretaceous–Paleocene interval, compiling information from ophiolites surrounding the Arabian Sea and data collected at sea. This reconstruction shows that the Amirante Ridge and Trench System constitutes the southern termination of a ${\sim }$1500-km-long subduction, which used to run along the NW Indian margin during the Late Cretaceous–Paleocene. The dislocation of the NW Indian subduction, recorded at the Amirante Ridge and Trench System and the Bela ophiolites, may have played a role in the plate reorganization event recorded at 73–63 Ma.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.40/AmiranteIndian OceanDeccanSubductionOphiolites
spellingShingle Rodriguez, Mathieu
The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
Comptes Rendus. Géoscience
Amirante
Indian Ocean
Deccan
Subduction
Ophiolites
title The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
title_full The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
title_fullStr The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
title_full_unstemmed The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
title_short The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction
title_sort amirante ridge and trench system in the indian ocean the southern termination of the nw indian subduction
topic Amirante
Indian Ocean
Deccan
Subduction
Ophiolites
url https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.40/
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