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...

Full description

Bibliographic Details
Published in:Journal of the Geological Society
Main Authors: Hueck, Mathias, Oriolo, Sebastián, Dunkl, István, Wemmer, Klaus, Oyhantçabal, Pedro, Schanofski, Max, Stipp Basei, Miguel Angelo, Siegesmund, Siegfried
Format: Article in Journal/Newspaper
Language:English
Published: Geological Soc Publ House
Subjects:
-
Online Access:http://hdl.handle.net/11336/66401
id ftconicet:oai:ri.conicet.gov.ar:11336/66401
record_format openpolar
spelling 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
_version_ 1779320192508100608