Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands

International audience The syenitic rocks of South Rallier du Baty Intrusive Complex (SRBIC) represent in- trusions into the oceanic plateau basalts of the south-western Kerguelen Islands. The SRBIC was previously interpreted as a typical ring complex due to magma emplace- ment with cauldron subside...

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Published in:Terra Nova
Main Authors: Ponthus, Léandre, de Saint Blanquat, Michel, Guillaume, Damien, Le Romancer, Marc, Pearson, Norman, O'Reilly, Suzanne, Grégoire, Michel
Other Authors: Géosciences Environnement Toulouse (GET), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Laboratoire Magmas et Volcans (LMV), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS), Géoarchitecture : Territoires, Urbanisation, Biodiversité, Environnement, Université de Rennes (UR)-Université de Brest (UBO), Macquarie University Sydney, Institut Polaire Français Paul Emile Victor, Centre National de la Recherche Scientifique
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.science/hal-03024359
https://hal.science/hal-03024359/document
https://hal.science/hal-03024359/file/2020-Ponthusetal-SRBIC%20%281%29.pdf
https://doi.org/10.1111/ter.12471
id ftunivlyon:oai:HAL:hal-03024359v1
record_format openpolar
institution Open Polar
collection Université de Lyon: HAL
op_collection_id ftunivlyon
language English
topic alkaline magmatism
Kerguelen
oceanic plateau
pluton emplacement
syenite intrusion
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics
[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography
spellingShingle alkaline magmatism
Kerguelen
oceanic plateau
pluton emplacement
syenite intrusion
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics
[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography
Ponthus, Léandre
de Saint Blanquat, Michel
Guillaume, Damien
Le Romancer, Marc
Pearson, Norman
O'Reilly, Suzanne
Grégoire, Michel
Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
topic_facet alkaline magmatism
Kerguelen
oceanic plateau
pluton emplacement
syenite intrusion
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics
[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography
description International audience The syenitic rocks of South Rallier du Baty Intrusive Complex (SRBIC) represent in- trusions into the oceanic plateau basalts of the south-western Kerguelen Islands. The SRBIC was previously interpreted as a typical ring complex due to magma emplace- ment with cauldron subsidence. Our new structural and geochronological data reveal that it is a laccolith built between 11.6 and 7.9 Ma by successive injections of magma sheets around the crust–mantle boundary, with an average injection rate between 0.8 and 1.4 × 10−4 km3/year. These results establish strong similarities between the SRBIC, the only recorded example of a felsic laccolith in an oceanic intraplate setting, and many continental plutons emplaced in various geodynamic setting. The SRBIC thus has the characteristics of a continental plutonic complex emplaced in an oceanic plateau crust. We postulate the critical parameter relevant to causing such similari- ties and plutonic magmatism is crustal thickness.
author2 Géosciences Environnement Toulouse (GET)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Laboratoire Magmas et Volcans (LMV)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)
Géoarchitecture : Territoires, Urbanisation, Biodiversité, Environnement
Université de Rennes (UR)-Université de Brest (UBO)
Macquarie University Sydney
Institut Polaire Français Paul Emile Victor
Centre National de la Recherche Scientifique
format Article in Journal/Newspaper
author Ponthus, Léandre
de Saint Blanquat, Michel
Guillaume, Damien
Le Romancer, Marc
Pearson, Norman
O'Reilly, Suzanne
Grégoire, Michel
author_facet Ponthus, Léandre
de Saint Blanquat, Michel
Guillaume, Damien
Le Romancer, Marc
Pearson, Norman
O'Reilly, Suzanne
Grégoire, Michel
author_sort Ponthus, Léandre
title Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
title_short Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
title_full Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
title_fullStr Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
title_full_unstemmed Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands
title_sort plutonic processes in transitional oceanic plateau crust: structure, age and emplacement of the south rallier du baty laccolith, kerguelen islands
publisher HAL CCSD
publishDate 2020
url https://hal.science/hal-03024359
https://hal.science/hal-03024359/document
https://hal.science/hal-03024359/file/2020-Ponthusetal-SRBIC%20%281%29.pdf
https://doi.org/10.1111/ter.12471
genre Kerguelen Islands
genre_facet Kerguelen Islands
op_source ISSN: 0954-4879
EISSN: 1365-3121
Terra Nova
https://hal.science/hal-03024359
Terra Nova, 2020, 32 (6), pp.408-414. ⟨10.1111/ter.12471⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12471
hal-03024359
https://hal.science/hal-03024359
https://hal.science/hal-03024359/document
https://hal.science/hal-03024359/file/2020-Ponthusetal-SRBIC%20%281%29.pdf
doi:10.1111/ter.12471
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1111/ter.12471
container_title Terra Nova
container_volume 32
container_issue 6
container_start_page 408
op_container_end_page 414
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spelling ftunivlyon:oai:HAL:hal-03024359v1 2024-09-15T18:16:26+00:00 Plutonic processes in transitional oceanic plateau crust: Structure, age and emplacement of the South Rallier du Baty laccolith, Kerguelen Islands Construction des plutons dans une croûte océanique transitionnelle : structure, âge et mise en place du laccolithe de Rallier du Baty Sud, Iles Kerguelen Ponthus, Léandre de Saint Blanquat, Michel Guillaume, Damien Le Romancer, Marc Pearson, Norman O'Reilly, Suzanne Grégoire, Michel Géosciences Environnement Toulouse (GET) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Laboratoire Magmas et Volcans (LMV) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS) Géoarchitecture : Territoires, Urbanisation, Biodiversité, Environnement Université de Rennes (UR)-Université de Brest (UBO) Macquarie University Sydney Institut Polaire Français Paul Emile Victor Centre National de la Recherche Scientifique 2020-12 https://hal.science/hal-03024359 https://hal.science/hal-03024359/document https://hal.science/hal-03024359/file/2020-Ponthusetal-SRBIC%20%281%29.pdf https://doi.org/10.1111/ter.12471 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12471 hal-03024359 https://hal.science/hal-03024359 https://hal.science/hal-03024359/document https://hal.science/hal-03024359/file/2020-Ponthusetal-SRBIC%20%281%29.pdf doi:10.1111/ter.12471 info:eu-repo/semantics/OpenAccess ISSN: 0954-4879 EISSN: 1365-3121 Terra Nova https://hal.science/hal-03024359 Terra Nova, 2020, 32 (6), pp.408-414. ⟨10.1111/ter.12471⟩ alkaline magmatism Kerguelen oceanic plateau pluton emplacement syenite intrusion [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography info:eu-repo/semantics/article Journal articles 2020 ftunivlyon https://doi.org/10.1111/ter.12471 2024-07-08T23:59:53Z International audience The syenitic rocks of South Rallier du Baty Intrusive Complex (SRBIC) represent in- trusions into the oceanic plateau basalts of the south-western Kerguelen Islands. The SRBIC was previously interpreted as a typical ring complex due to magma emplace- ment with cauldron subsidence. Our new structural and geochronological data reveal that it is a laccolith built between 11.6 and 7.9 Ma by successive injections of magma sheets around the crust–mantle boundary, with an average injection rate between 0.8 and 1.4 × 10−4 km3/year. These results establish strong similarities between the SRBIC, the only recorded example of a felsic laccolith in an oceanic intraplate setting, and many continental plutons emplaced in various geodynamic setting. The SRBIC thus has the characteristics of a continental plutonic complex emplaced in an oceanic plateau crust. We postulate the critical parameter relevant to causing such similari- ties and plutonic magmatism is crustal thickness. Article in Journal/Newspaper Kerguelen Islands Université de Lyon: HAL Terra Nova 32 6 408 414