The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup
International audience The rifted continental margins of Mozambique provide excellent examples of continental passive margins with a significant structural variability associated with magmatism and inheritance. Despite accumulated knowledge, the tectonic structure and nature of the crust beneath the...
Published in: | Tectonics |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2021
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Subjects: | |
Online Access: | https://hal-insu.archives-ouvertes.fr/insu-03445510 https://doi.org/10.1029/2021TC006914 |
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ftccsdartic:oai:HAL:insu-03445510v1 |
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openpolar |
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Open Polar |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
Transform margin magmatism strike-slip system pull-apart Mozambique Seismic reflection [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
spellingShingle |
Transform margin magmatism strike-slip system pull-apart Mozambique Seismic reflection [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics Roche, V. Leroy, S. Guillocheau, François Revillon, Sidonie Ruffet, Gilles Watremez, L. d’Acremont, E. Nonn, C. Vetel, W. Despinois, F. The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
topic_facet |
Transform margin magmatism strike-slip system pull-apart Mozambique Seismic reflection [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
description |
International audience The rifted continental margins of Mozambique provide excellent examples of continental passive margins with a significant structural variability associated with magmatism and inheritance. Despite accumulated knowledge, the tectonic structure and nature of the crust beneath the South Mozambique Coastal Plain (SMCP) are still poorly known. This study interprets high-resolution seismic reflection data paired with data from industry-drilled wells and proposes a structural model of the Limpopo transform margin in a magma-rich context. Results indicate that the Limpopo transform margin is characterized by an ocean-continent transition that links the Beira-High and Natal valley margin segments and represents the western limit of the continental crust, separating continental volcano-sedimentary infilled grabens from the oceanic crust domain. These basins result from the emplacement of the Karoo Supergroup during a Permo-Triassic tectonic event, followed by an Early Jurassic tectonic and magmatic event. This latter led to the establishment of steady-state seafloor spreading at ca.156 Ma along the SMCP. A Late Jurassic to Early Cretaceous event corresponds to formation of the Limpopo transform fault zone. Which accommodated the SSE-ward displacement of Antarctica with respect to Africa. We define a new type of margin: the magma-rich transform margin, characterized by the presence of voluminous magmatic extrusion and intrusion coincident with the formation and evolution of the transform margin. The Limpopo transform fault zone consists of several syn-transfer and -transform faults rather than a single transform fault. The intense magmatic activity was associated primarily with mantle dynamics, which controlled the large-scale differential subsidence along the transform margin. |
author2 |
Institut des Sciences de la Terre de Paris (iSTeP) Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS) 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) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG) Centre National de la Recherche Scientifique (CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Institut national des sciences de l'Univers (INSU - CNRS) TotalEnergies E&P, CSTJF, Pau, France PAMELA project (PAssive Margin Exploration Laboratories) (IFREMER, TotalEnergies) |
format |
Article in Journal/Newspaper |
author |
Roche, V. Leroy, S. Guillocheau, François Revillon, Sidonie Ruffet, Gilles Watremez, L. d’Acremont, E. Nonn, C. Vetel, W. Despinois, F. |
author_facet |
Roche, V. Leroy, S. Guillocheau, François Revillon, Sidonie Ruffet, Gilles Watremez, L. d’Acremont, E. Nonn, C. Vetel, W. Despinois, F. |
author_sort |
Roche, V. |
title |
The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
title_short |
The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
title_full |
The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
title_fullStr |
The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
title_full_unstemmed |
The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup |
title_sort |
limpopo magma‐rich transform margin, south mozambique – part 2: implications for the gondwana breakup |
publisher |
HAL CCSD |
publishDate |
2021 |
url |
https://hal-insu.archives-ouvertes.fr/insu-03445510 https://doi.org/10.1029/2021TC006914 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
ISSN: 0278-7407 EISSN: 1944-9194 Tectonics https://hal-insu.archives-ouvertes.fr/insu-03445510 Tectonics, American Geophysical Union (AGU), In press, ⟨10.1029/2021TC006914⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2021TC006914 insu-03445510 https://hal-insu.archives-ouvertes.fr/insu-03445510 doi:10.1029/2021TC006914 |
op_doi |
https://doi.org/10.1029/2021TC006914 |
container_title |
Tectonics |
container_volume |
40 |
container_issue |
12 |
_version_ |
1766261001299165184 |
spelling |
ftccsdartic:oai:HAL:insu-03445510v1 2023-05-15T13:54:52+02:00 The Limpopo magma‐rich transform margin, South Mozambique – part 2: Implications for the Gondwana breakup Roche, V. Leroy, S. Guillocheau, François Revillon, Sidonie Ruffet, Gilles Watremez, L. d’Acremont, E. Nonn, C. Vetel, W. Despinois, F. Institut des Sciences de la Terre de Paris (iSTeP) Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS) 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) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG) Centre National de la Recherche Scientifique (CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Institut national des sciences de l'Univers (INSU - CNRS) TotalEnergies E&P, CSTJF, Pau, France PAMELA project (PAssive Margin Exploration Laboratories) (IFREMER, TotalEnergies) 2021 https://hal-insu.archives-ouvertes.fr/insu-03445510 https://doi.org/10.1029/2021TC006914 en eng HAL CCSD American Geophysical Union (AGU) info:eu-repo/semantics/altIdentifier/doi/10.1029/2021TC006914 insu-03445510 https://hal-insu.archives-ouvertes.fr/insu-03445510 doi:10.1029/2021TC006914 ISSN: 0278-7407 EISSN: 1944-9194 Tectonics https://hal-insu.archives-ouvertes.fr/insu-03445510 Tectonics, American Geophysical Union (AGU), In press, ⟨10.1029/2021TC006914⟩ Transform margin magmatism strike-slip system pull-apart Mozambique Seismic reflection [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics info:eu-repo/semantics/article Journal articles 2021 ftccsdartic https://doi.org/10.1029/2021TC006914 2022-01-08T23:51:22Z International audience The rifted continental margins of Mozambique provide excellent examples of continental passive margins with a significant structural variability associated with magmatism and inheritance. Despite accumulated knowledge, the tectonic structure and nature of the crust beneath the South Mozambique Coastal Plain (SMCP) are still poorly known. This study interprets high-resolution seismic reflection data paired with data from industry-drilled wells and proposes a structural model of the Limpopo transform margin in a magma-rich context. Results indicate that the Limpopo transform margin is characterized by an ocean-continent transition that links the Beira-High and Natal valley margin segments and represents the western limit of the continental crust, separating continental volcano-sedimentary infilled grabens from the oceanic crust domain. These basins result from the emplacement of the Karoo Supergroup during a Permo-Triassic tectonic event, followed by an Early Jurassic tectonic and magmatic event. This latter led to the establishment of steady-state seafloor spreading at ca.156 Ma along the SMCP. A Late Jurassic to Early Cretaceous event corresponds to formation of the Limpopo transform fault zone. Which accommodated the SSE-ward displacement of Antarctica with respect to Africa. We define a new type of margin: the magma-rich transform margin, characterized by the presence of voluminous magmatic extrusion and intrusion coincident with the formation and evolution of the transform margin. The Limpopo transform fault zone consists of several syn-transfer and -transform faults rather than a single transform fault. The intense magmatic activity was associated primarily with mantle dynamics, which controlled the large-scale differential subsidence along the transform margin. Article in Journal/Newspaper Antarc* Antarctica Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Tectonics 40 12 |