Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin
The crystalline basement of Uruguay was assembled during the Brasiliano Orogeny in the Neoproterozoic Era and was later affected by discrete tectonic activity. A new multi-method low-temperature dataset including (U-Th)/He ages from both zircon and apatite, T-t modelling and K-Ar dating of fine seri...
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ftconicet:oai:ri.conicet.gov.ar:11336/66401 2023-10-09T21:55:56+02:00 Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin Hueck, Mathias Oriolo, Sebastián Dunkl, István Wemmer, Klaus Oyhantçabal, Pedro Schanofski, Max Stipp Basei, Miguel Angelo Siegesmund, Siegfried application/pdf http://hdl.handle.net/11336/66401 eng eng Geological Soc Publ House info:eu-repo/semantics/altIdentifier/url/http://jgs.lyellcollection.org/lookup/doi/10.1144/jgs2016-101 info:eu-repo/semantics/altIdentifier/doi/10.1144/jgs2016-101 info:eu-repo/semantics/altIdentifier/url/http://mr.crossref.org/iPage?doi=10.1144%2Fjgs2016-101 http://hdl.handle.net/11336/66401 Hueck, Mathias; Oriolo, Sebastián; Dunkl, István; Wemmer, Klaus; Oyhantçabal, Pedro; et al.; Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin; Geological Soc Publ House; Journal of the Geological Society; 174; 4; 7-2017; 609-626 0016-7649 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ - 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/10.1144/jgs2016-101 2023-09-24T18:33:27Z The crystalline basement of Uruguay was assembled during the Brasiliano Orogeny in the Neoproterozoic Era and was later affected by discrete tectonic activity. A new multi-method low-temperature dataset including (U-Th)/He ages from both zircon and apatite, T-t modelling and K-Ar dating of fine sericite fractions and fault gouge reveal a detailed post-orogenic geological history spanning the Phanerozoic Eon. The juxtaposition of the terranes that compose the area was achieved in the Ediacaran Period, and post-collision was marked by intense exhumation, in which the crystalline basement reached near-surface conditions by the early to mid-Palaeozoic. Regional subsidence promoted sedimentation in the Paraná Basin until the Permian, covering and reheating much of the basement that is at present exposed. Afterwards, deposition and volcanism were mostly confined to its current limits. Regional exhumation of the shield during the Permo-Triassic exposed much of the northern portion of the basement, and the south was further affected by the opening of the South Atlantic Ocean during the Mesozoic. Little exhumation affected the Uruguayan Shield during the Cenozoic, as reflected in its modest topography. The reactivation of inherited Neoproterozoic structures influenced the development of Mesozoic basins and the present-day landscape. Fil: Hueck, Mathias. Universität Göttingen; Alemania Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universität Göttingen; Alemania Fil: Dunkl, István. Universität Göttingen; Alemania Fil: Wemmer, Klaus. Universität Göttingen; Alemania Fil: Oyhantçabal, Pedro. Universidad de la Republica. Instituto de Ciencias Geológicas; Uruguay Fil: Schanofski, Max. Universität Göttingen; Alemania Fil: Stipp Basei, Miguel Angelo. Universidade de Sao Paulo; Brasil Fil: Siegesmund, Siegfried. Universität Göttingen; Alemania Article in Journal/Newspaper South Atlantic Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Uruguay Klaus ENVELOPE(24.117,24.117,65.717,65.717) Journal of the Geological Society 174 4 609 626 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
- https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
- https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Hueck, Mathias Oriolo, Sebastián Dunkl, István Wemmer, Klaus Oyhantçabal, Pedro Schanofski, Max Stipp Basei, Miguel Angelo Siegesmund, Siegfried Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
topic_facet |
- https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
The crystalline basement of Uruguay was assembled during the Brasiliano Orogeny in the Neoproterozoic Era and was later affected by discrete tectonic activity. A new multi-method low-temperature dataset including (U-Th)/He ages from both zircon and apatite, T-t modelling and K-Ar dating of fine sericite fractions and fault gouge reveal a detailed post-orogenic geological history spanning the Phanerozoic Eon. The juxtaposition of the terranes that compose the area was achieved in the Ediacaran Period, and post-collision was marked by intense exhumation, in which the crystalline basement reached near-surface conditions by the early to mid-Palaeozoic. Regional subsidence promoted sedimentation in the Paraná Basin until the Permian, covering and reheating much of the basement that is at present exposed. Afterwards, deposition and volcanism were mostly confined to its current limits. Regional exhumation of the shield during the Permo-Triassic exposed much of the northern portion of the basement, and the south was further affected by the opening of the South Atlantic Ocean during the Mesozoic. Little exhumation affected the Uruguayan Shield during the Cenozoic, as reflected in its modest topography. The reactivation of inherited Neoproterozoic structures influenced the development of Mesozoic basins and the present-day landscape. Fil: Hueck, Mathias. Universität Göttingen; Alemania Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universität Göttingen; Alemania Fil: Dunkl, István. Universität Göttingen; Alemania Fil: Wemmer, Klaus. Universität Göttingen; Alemania Fil: Oyhantçabal, Pedro. Universidad de la Republica. Instituto de Ciencias Geológicas; Uruguay Fil: Schanofski, Max. Universität Göttingen; Alemania Fil: Stipp Basei, Miguel Angelo. Universidade de Sao Paulo; Brasil Fil: Siegesmund, Siegfried. Universität Göttingen; Alemania |
format |
Article in Journal/Newspaper |
author |
Hueck, Mathias Oriolo, Sebastián Dunkl, István Wemmer, Klaus Oyhantçabal, Pedro Schanofski, Max Stipp Basei, Miguel Angelo Siegesmund, Siegfried |
author_facet |
Hueck, Mathias Oriolo, Sebastián Dunkl, István Wemmer, Klaus Oyhantçabal, Pedro Schanofski, Max Stipp Basei, Miguel Angelo Siegesmund, Siegfried |
author_sort |
Hueck, Mathias |
title |
Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
title_short |
Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
title_full |
Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
title_fullStr |
Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
title_full_unstemmed |
Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin |
title_sort |
phanerozoic low-temperature evolution of the uruguayan shield along the south american passive margin |
publisher |
Geological Soc Publ House |
url |
http://hdl.handle.net/11336/66401 |
long_lat |
ENVELOPE(24.117,24.117,65.717,65.717) |
geographic |
Argentina Uruguay Klaus |
geographic_facet |
Argentina Uruguay Klaus |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
info:eu-repo/semantics/altIdentifier/url/http://jgs.lyellcollection.org/lookup/doi/10.1144/jgs2016-101 info:eu-repo/semantics/altIdentifier/doi/10.1144/jgs2016-101 info:eu-repo/semantics/altIdentifier/url/http://mr.crossref.org/iPage?doi=10.1144%2Fjgs2016-101 http://hdl.handle.net/11336/66401 Hueck, Mathias; Oriolo, Sebastián; Dunkl, István; Wemmer, Klaus; Oyhantçabal, Pedro; et al.; Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin; Geological Soc Publ House; Journal of the Geological Society; 174; 4; 7-2017; 609-626 0016-7649 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1144/jgs2016-101 |
container_title |
Journal of the Geological Society |
container_volume |
174 |
container_issue |
4 |
container_start_page |
609 |
op_container_end_page |
626 |
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1779320192508100608 |