Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica

New isotopic studies on mantle xenoliths from Santa Cruz Province, southern Patagonia, Argentina, reveal that at least three discrete subcontinental lithospheric mantle (SCLM) domains—the Deseado Massif, Tres Lagos, and Pali Aike—form the southernmost part of South America. Re-Os systematics yield e...

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Published in:Geology
Main Authors: Mundl, Andrea, Ntaflos, Theodoros, Ackerman, Lukas, Bizimis, Michael, Bjerg, Ernesto Alfredo, Hauzenberger, Christoph A.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of America
Subjects:
Online Access:http://hdl.handle.net/11336/6492
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/6492 2023-10-09T21:47:16+02:00 Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica Mundl, Andrea Ntaflos, Theodoros Ackerman, Lukas Bizimis, Michael Bjerg, Ernesto Alfredo Hauzenberger, Christoph A. application/pdf http://hdl.handle.net/11336/6492 eng eng Geological Society of America info:eu-repo/semantics/altIdentifier/doi/ info:eu-repo/semantics/altIdentifier/doi/10.1130/G36344.1 info:eu-repo/semantics/altIdentifier/url/http://geology.gsapubs.org/content/43/1/39 info:eu-repo/semantics/altIdentifier/url/http://geology.geoscienceworld.org/content/43/1/39 http://hdl.handle.net/11336/6492 Mundl, Andrea; Ntaflos, Theodoros; Ackerman, Lukas; Bizimis, Michael; Bjerg, Ernesto Alfredo; et al.; Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica; Geological Society of America; Geology; 43; 1; 1-2015; 39-42 0091-7613 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ MESOPROTEROZOIC PALEOPROTEROZOIC MANTLE PATAGONIA https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1130/G36344.1 2023-09-24T19:11:06Z New isotopic studies on mantle xenoliths from Santa Cruz Province, southern Patagonia, Argentina, reveal that at least three discrete subcontinental lithospheric mantle (SCLM) domains—the Deseado Massif, Tres Lagos, and Pali Aike—form the southernmost part of South America. Re-Os systematics yield early Paleoproterozoic (up to 2.5 Ga) SCLM formation ages (rhenium depletion ages, TRD) for Pali Aike spinel peridotites, while samples from the Deseado Massif and Tres Lagos indicate a younger SCLM origin with Neoproterozoic to Mesoproterozoic (0.9–1.3 Ga) and Mesoproterozoic to late Paleoproterozoic (1.3–1.9 Ga) TRD ages, respectively. Hf-Sr-Nd isotopic compositions indicate metasomatic overprinting of the majority of the samples, which, however, has not affected the Os isotopic system. Based on similar formation ages, the geological evolution of the Deseado Massif is most likely connected to the evolution of the Namaqua-Natal belt of South Africa. TRD ages from SCLM domains underneath Tres Lagos and Pali Aike indicate a common origin with crustal sections from Shackleton Range, Antarctica, positioning the southern tip of South America closer to west Antarctica in the reconstructed Rodinia supercontinent than previously assumed. Fil: Mundl, Andrea. University of Vienna.Department of Lithospheric Research; Austria Fil: Ntaflos, Theodoros. University of Vienna. Department of Lithospheric Research; Austria Fil: Ackerman, Lukas. Academy of Sciences of the Czech Republic; República Checa. Czech Geological Survey; República Checa Fil: Bizimis, Michael. University of South Carolina; Estados Unidos Fil: Bjerg, Ernesto Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Geológico del Sur; Argentina. Universidad Nacional del Sur; Argentina Fil: Hauzenberger, Christoph A. University of Graz. Institute for Earth Sciences; Austria Article in Journal/Newspaper Antarc* Antarctica West Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Patagonia West Antarctica Shackleton Argentina Shackleton Range ENVELOPE(-26.000,-26.000,-80.833,-80.833) Geology 43 1 39 42
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic MESOPROTEROZOIC
PALEOPROTEROZOIC
MANTLE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle MESOPROTEROZOIC
PALEOPROTEROZOIC
MANTLE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Mundl, Andrea
Ntaflos, Theodoros
Ackerman, Lukas
Bizimis, Michael
Bjerg, Ernesto Alfredo
Hauzenberger, Christoph A.
Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
topic_facet MESOPROTEROZOIC
PALEOPROTEROZOIC
MANTLE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description New isotopic studies on mantle xenoliths from Santa Cruz Province, southern Patagonia, Argentina, reveal that at least three discrete subcontinental lithospheric mantle (SCLM) domains—the Deseado Massif, Tres Lagos, and Pali Aike—form the southernmost part of South America. Re-Os systematics yield early Paleoproterozoic (up to 2.5 Ga) SCLM formation ages (rhenium depletion ages, TRD) for Pali Aike spinel peridotites, while samples from the Deseado Massif and Tres Lagos indicate a younger SCLM origin with Neoproterozoic to Mesoproterozoic (0.9–1.3 Ga) and Mesoproterozoic to late Paleoproterozoic (1.3–1.9 Ga) TRD ages, respectively. Hf-Sr-Nd isotopic compositions indicate metasomatic overprinting of the majority of the samples, which, however, has not affected the Os isotopic system. Based on similar formation ages, the geological evolution of the Deseado Massif is most likely connected to the evolution of the Namaqua-Natal belt of South Africa. TRD ages from SCLM domains underneath Tres Lagos and Pali Aike indicate a common origin with crustal sections from Shackleton Range, Antarctica, positioning the southern tip of South America closer to west Antarctica in the reconstructed Rodinia supercontinent than previously assumed. Fil: Mundl, Andrea. University of Vienna.Department of Lithospheric Research; Austria Fil: Ntaflos, Theodoros. University of Vienna. Department of Lithospheric Research; Austria Fil: Ackerman, Lukas. Academy of Sciences of the Czech Republic; República Checa. Czech Geological Survey; República Checa Fil: Bizimis, Michael. University of South Carolina; Estados Unidos Fil: Bjerg, Ernesto Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Geológico del Sur; Argentina. Universidad Nacional del Sur; Argentina Fil: Hauzenberger, Christoph A. University of Graz. Institute for Earth Sciences; Austria
format Article in Journal/Newspaper
author Mundl, Andrea
Ntaflos, Theodoros
Ackerman, Lukas
Bizimis, Michael
Bjerg, Ernesto Alfredo
Hauzenberger, Christoph A.
author_facet Mundl, Andrea
Ntaflos, Theodoros
Ackerman, Lukas
Bizimis, Michael
Bjerg, Ernesto Alfredo
Hauzenberger, Christoph A.
author_sort Mundl, Andrea
title Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
title_short Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
title_full Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
title_fullStr Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
title_full_unstemmed Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica
title_sort mesoproterozoic and paleoproterozoic subcontinental lithospheric mantle domains beneath southern patagonia: isotopic evidence for its connection to africa and antarctica
publisher Geological Society of America
url http://hdl.handle.net/11336/6492
long_lat ENVELOPE(-26.000,-26.000,-80.833,-80.833)
geographic Patagonia
West Antarctica
Shackleton
Argentina
Shackleton Range
geographic_facet Patagonia
West Antarctica
Shackleton
Argentina
Shackleton Range
genre Antarc*
Antarctica
West Antarctica
genre_facet Antarc*
Antarctica
West Antarctica
op_relation info:eu-repo/semantics/altIdentifier/doi/
info:eu-repo/semantics/altIdentifier/doi/10.1130/G36344.1
info:eu-repo/semantics/altIdentifier/url/http://geology.gsapubs.org/content/43/1/39
info:eu-repo/semantics/altIdentifier/url/http://geology.geoscienceworld.org/content/43/1/39
http://hdl.handle.net/11336/6492
Mundl, Andrea; Ntaflos, Theodoros; Ackerman, Lukas; Bizimis, Michael; Bjerg, Ernesto Alfredo; et al.; Mesoproterozoic and Paleoproterozoic subcontinental lithospheric mantle domains beneath southern Patagonia: Isotopic evidence for its connection to Africa and Antarctica; Geological Society of America; Geology; 43; 1; 1-2015; 39-42
0091-7613
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
op_doi https://doi.org/10.1130/G36344.1
container_title Geology
container_volume 43
container_issue 1
container_start_page 39
op_container_end_page 42
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