Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection

International audience This study presents the first geochronological results on basement rocks from the Penguin-Bage-Webb (PBW) domain located east of the Neoarchean-Paleoproterozoic Terre Adélie craton, Antarctica. Investigated samples are paragneiss xenoliths hosted within early Paleozoic granito...

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Published in:Lithos
Main Authors: Lamarque, Gaëlle, Bascou, Jerôme, Ménot, René-Pierre, Paquette, Jean-Louis, Couzinié, Simon, Rolland, Yann, Cottin, Jean-Yves
Other Authors: Laboratoire Magmas et Volcans (LMV), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement et la société-Institut national des sciences de l'Univers (INSU - 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)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Université Jean Monnet Saint-Étienne (UJM), Laboratoire de Physique de l'ENS Lyon (Phys-ENS), École normale supérieure - Lyon (ENS Lyon)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement Lyon (LGL-TPE), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Géoazur (GEOAZUR 7329), Université Côte d'Azur (UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD France-Sud )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2018
Subjects:
Online Access:https://hal.uca.fr/hal-01863781
https://doi.org/10.1016/j.lithos.2018.08.021
id ftccsdartic:oai:HAL:hal-01863781v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic Antarctica-Australia connection
Zircon and monazite UPb dating
Gondwana margin
Ross orogeny
George V Land
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
spellingShingle Antarctica-Australia connection
Zircon and monazite UPb dating
Gondwana margin
Ross orogeny
George V Land
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
Lamarque, Gaëlle
Bascou, Jerôme
Ménot, René-Pierre
Paquette, Jean-Louis
Couzinié, Simon
Rolland, Yann
Cottin, Jean-Yves
Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
topic_facet Antarctica-Australia connection
Zircon and monazite UPb dating
Gondwana margin
Ross orogeny
George V Land
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
description International audience This study presents the first geochronological results on basement rocks from the Penguin-Bage-Webb (PBW) domain located east of the Neoarchean-Paleoproterozoic Terre Adélie craton, Antarctica. Investigated samples are paragneiss xenoliths hosted within early Paleozoic granitoids, which were emplaced during the Ross orogeny. Zircon UPb dating yielded ages ranging from the Archean to the Cambrian, with a dominant Ediacaran (550–635 Ma) population and maximum depositional ages around 570–575 Ma. U–Th–Pb analyses of monazite suggest that the metamorphic event that formed the gneiss samples occured at ca. 515 Ma, shortly prior to incorporation within the granitic magmas. The studied samples likely represent relics of the pre-Gondawana Pacific margin, which was subsequently deformed and metamorphosed during the early Paleozoic Ross orogeny. The obtained zircon UPb date distributions present similarities with those of the Kanmantoo and Nargoon sediments in Southern Australia and provide new constrains for the correlations between East Antarctica and South Australia before the opening of the Southern Ocean.
author2 Laboratoire Magmas et Volcans (LMV)
Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement et la société-Institut national des sciences de l'Univers (INSU - 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)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Université Jean Monnet Saint-Étienne (UJM)
Laboratoire de Physique de l'ENS Lyon (Phys-ENS)
École normale supérieure - Lyon (ENS Lyon)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon-Université de Lyon
Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement Lyon (LGL-TPE)
École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Géoazur (GEOAZUR 7329)
Université Côte d'Azur (UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD France-Sud )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur
Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)
format Article in Journal/Newspaper
author Lamarque, Gaëlle
Bascou, Jerôme
Ménot, René-Pierre
Paquette, Jean-Louis
Couzinié, Simon
Rolland, Yann
Cottin, Jean-Yves
author_facet Lamarque, Gaëlle
Bascou, Jerôme
Ménot, René-Pierre
Paquette, Jean-Louis
Couzinié, Simon
Rolland, Yann
Cottin, Jean-Yves
author_sort Lamarque, Gaëlle
title Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
title_short Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
title_full Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
title_fullStr Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
title_full_unstemmed Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection
title_sort ediacaran to lower cambrian basement in eastern george v land (antarctica): evidence from u pb dating of gneiss xenoliths and implications for the south australia- east antarctica connection
publisher HAL CCSD
publishDate 2018
url https://hal.uca.fr/hal-01863781
https://doi.org/10.1016/j.lithos.2018.08.021
long_lat ENVELOPE(146.583,146.583,-67.733,-67.733)
ENVELOPE(148.000,148.000,-68.500,-68.500)
ENVELOPE(139.000,139.000,-67.000,-67.000)
ENVELOPE(138.991,138.991,-59.999,-59.999)
ENVELOPE(146.867,146.867,-67.867,-67.867)
geographic Bage
East Antarctica
George V Land
Pacific
Southern Ocean
Terre Adélie
Terre-Adélie
Webb
geographic_facet Bage
East Antarctica
George V Land
Pacific
Southern Ocean
Terre Adélie
Terre-Adélie
Webb
genre Antarc*
Antarctica
East Antarctica
George V Land
Southern Ocean
genre_facet Antarc*
Antarctica
East Antarctica
George V Land
Southern Ocean
op_source ISSN: 0024-4937
Lithos
https://hal.uca.fr/hal-01863781
Lithos, Elsevier, 2018, 318-319, pp.219 - 229. ⟨10.1016/j.lithos.2018.08.021⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2018.08.021
hal-01863781
https://hal.uca.fr/hal-01863781
doi:10.1016/j.lithos.2018.08.021
op_doi https://doi.org/10.1016/j.lithos.2018.08.021
container_title Lithos
container_volume 318-319
container_start_page 219
op_container_end_page 229
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spelling ftccsdartic:oai:HAL:hal-01863781v1 2023-05-15T13:56:48+02:00 Ediacaran to lower Cambrian basement in eastern George V Land (Antarctica): Evidence from U Pb dating of gneiss xenoliths and implications for the South Australia- East Antarctica connection Lamarque, Gaëlle Bascou, Jerôme Ménot, René-Pierre Paquette, Jean-Louis Couzinié, Simon Rolland, Yann Cottin, Jean-Yves Laboratoire Magmas et Volcans (LMV) Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement et la société-Institut national des sciences de l'Univers (INSU - 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)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Université Jean Monnet Saint-Étienne (UJM) Laboratoire de Physique de l'ENS Lyon (Phys-ENS) École normale supérieure - Lyon (ENS Lyon)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement Lyon (LGL-TPE) École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Géoazur (GEOAZUR 7329) Université Côte d'Azur (UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD France-Sud )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA) 2018-10 https://hal.uca.fr/hal-01863781 https://doi.org/10.1016/j.lithos.2018.08.021 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2018.08.021 hal-01863781 https://hal.uca.fr/hal-01863781 doi:10.1016/j.lithos.2018.08.021 ISSN: 0024-4937 Lithos https://hal.uca.fr/hal-01863781 Lithos, Elsevier, 2018, 318-319, pp.219 - 229. ⟨10.1016/j.lithos.2018.08.021⟩ Antarctica-Australia connection Zircon and monazite UPb dating Gondwana margin Ross orogeny George V Land [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry info:eu-repo/semantics/article Journal articles 2018 ftccsdartic https://doi.org/10.1016/j.lithos.2018.08.021 2021-12-12T03:14:16Z International audience This study presents the first geochronological results on basement rocks from the Penguin-Bage-Webb (PBW) domain located east of the Neoarchean-Paleoproterozoic Terre Adélie craton, Antarctica. Investigated samples are paragneiss xenoliths hosted within early Paleozoic granitoids, which were emplaced during the Ross orogeny. Zircon UPb dating yielded ages ranging from the Archean to the Cambrian, with a dominant Ediacaran (550–635 Ma) population and maximum depositional ages around 570–575 Ma. U–Th–Pb analyses of monazite suggest that the metamorphic event that formed the gneiss samples occured at ca. 515 Ma, shortly prior to incorporation within the granitic magmas. The studied samples likely represent relics of the pre-Gondawana Pacific margin, which was subsequently deformed and metamorphosed during the early Paleozoic Ross orogeny. The obtained zircon UPb date distributions present similarities with those of the Kanmantoo and Nargoon sediments in Southern Australia and provide new constrains for the correlations between East Antarctica and South Australia before the opening of the Southern Ocean. Article in Journal/Newspaper Antarc* Antarctica East Antarctica George V Land Southern Ocean Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Bage ENVELOPE(146.583,146.583,-67.733,-67.733) East Antarctica George V Land ENVELOPE(148.000,148.000,-68.500,-68.500) Pacific Southern Ocean Terre Adélie ENVELOPE(139.000,139.000,-67.000,-67.000) Terre-Adélie ENVELOPE(138.991,138.991,-59.999,-59.999) Webb ENVELOPE(146.867,146.867,-67.867,-67.867) Lithos 318-319 219 229