The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana
In recent years, multiple Mesozoic episodes of crustal shortening and extension have been documented throughout Patagonia. These findings unveil a complex history of regional intraplate tectonic deformation. Nevertheless, there are numerous sectors in this vast region that have yet to undergo in-dep...
Published in: | Tectonophysics |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier Science
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Online Access: | http://hdl.handle.net/11336/230811 |
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author | Perez Frasette, Maximiliano Jose Navarrete Granzotto, César Rodrigo Bastías Silva, Joaquín Valle, Mauro Nicolás Chew, David Iglesias, Maximiliano Lujan Suárez, Manuel Márquez, Marcelo Drakou, Foteini Folguera, Andrés |
author_facet | Perez Frasette, Maximiliano Jose Navarrete Granzotto, César Rodrigo Bastías Silva, Joaquín Valle, Mauro Nicolás Chew, David Iglesias, Maximiliano Lujan Suárez, Manuel Márquez, Marcelo Drakou, Foteini Folguera, Andrés |
author_sort | Perez Frasette, Maximiliano Jose |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_start_page | 230241 |
container_title | Tectonophysics |
container_volume | 874 |
description | In recent years, multiple Mesozoic episodes of crustal shortening and extension have been documented throughout Patagonia. These findings unveil a complex history of regional intraplate tectonic deformation. Nevertheless, there are numerous sectors in this vast region that have yet to undergo in-depth tectonic investigations, and hence aspects of its evolutionary history remain elusive. We present herein a comprehensive dataset comprising geophysical data (2D seismic lines), field data (detailed geological mapping and lithofacies analysis), and Usingle bondPb geochronological data (LA-ICP-MS and SHRIMP zircon ages) from a key region in southern Patagonia, known as the Bajo Grande area, located in the center of the Deseado Massif. The datasets support the hypothesis of a Late Jurassic(?) to Early Cretaceous shortening event that led to the tectonic inversion of former Jurassic (or may be older) extensional depocenters. This episode promoted the syn-inversion (syn-orogenic) deposition of Late Jurassic(?)-Early Cretaceous (140 ± 3 Ma) epiclastic and pyroclastic rocks within NNE-striking depocenters. These rocks are part of the Bajo Grande Formation, representing one of the oldest documented syn-orogenic sequences in southern Patagonia. This shortening event may have been triggered by a far-field response to the opening of the Rocas Verdes basin and to the rift-drift transition of the South-Atlantic Ocean. Fil: Perez Frasette, Maximiliano Jose. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Bastías Silva, Joaquín. Universidad Nacional de la Patagonia "san Juan Bosco". Facultad de Cs.naturales - Sede Comodoro. Cátedra de Geología Historica; Argentina. Eidgenossische Technische Hochschule zurich (eth Zurich); . Trinity College Dublin; Irlanda ... |
format | Article in Journal/Newspaper |
genre | South Atlantic Ocean |
genre_facet | South Atlantic Ocean |
geographic | Patagonia San Juan Argentina Perez Rocas Navarrete |
geographic_facet | Patagonia San Juan Argentina Perez Rocas Navarrete |
id | ftconicet:oai:ri.conicet.gov.ar:11336/230811 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-69.117,-69.117,-68.517,-68.517) ENVELOPE(-56.948,-56.948,-63.398,-63.398) ENVELOPE(-62.533,-62.533,-64.833,-64.833) |
op_collection_id | ftconicet |
op_doi | https://doi.org/10.1016/j.tecto.2024.230241 |
op_relation | info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S004019512400043X info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2024.230241 http://hdl.handle.net/11336/230811 CONICET Digital CONICET |
op_rights | info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
publisher | Elsevier Science |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/230811 2025-01-17T00:50:12+00:00 The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana Perez Frasette, Maximiliano Jose Navarrete Granzotto, César Rodrigo Bastías Silva, Joaquín Valle, Mauro Nicolás Chew, David Iglesias, Maximiliano Lujan Suárez, Manuel Márquez, Marcelo Drakou, Foteini Folguera, Andrés application/pdf http://hdl.handle.net/11336/230811 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S004019512400043X info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2024.230241 http://hdl.handle.net/11336/230811 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ Patagonia Intraplate Contraction Tectonic inversion 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/10.1016/j.tecto.2024.230241 2024-10-04T09:34:18Z In recent years, multiple Mesozoic episodes of crustal shortening and extension have been documented throughout Patagonia. These findings unveil a complex history of regional intraplate tectonic deformation. Nevertheless, there are numerous sectors in this vast region that have yet to undergo in-depth tectonic investigations, and hence aspects of its evolutionary history remain elusive. We present herein a comprehensive dataset comprising geophysical data (2D seismic lines), field data (detailed geological mapping and lithofacies analysis), and Usingle bondPb geochronological data (LA-ICP-MS and SHRIMP zircon ages) from a key region in southern Patagonia, known as the Bajo Grande area, located in the center of the Deseado Massif. The datasets support the hypothesis of a Late Jurassic(?) to Early Cretaceous shortening event that led to the tectonic inversion of former Jurassic (or may be older) extensional depocenters. This episode promoted the syn-inversion (syn-orogenic) deposition of Late Jurassic(?)-Early Cretaceous (140 ± 3 Ma) epiclastic and pyroclastic rocks within NNE-striking depocenters. These rocks are part of the Bajo Grande Formation, representing one of the oldest documented syn-orogenic sequences in southern Patagonia. This shortening event may have been triggered by a far-field response to the opening of the Rocas Verdes basin and to the rift-drift transition of the South-Atlantic Ocean. Fil: Perez Frasette, Maximiliano Jose. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Bastías Silva, Joaquín. Universidad Nacional de la Patagonia "san Juan Bosco". Facultad de Cs.naturales - Sede Comodoro. Cátedra de Geología Historica; Argentina. Eidgenossische Technische Hochschule zurich (eth Zurich); . Trinity College Dublin; Irlanda ... Article in Journal/Newspaper South Atlantic Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Patagonia San Juan Argentina Perez ENVELOPE(-69.117,-69.117,-68.517,-68.517) Rocas ENVELOPE(-56.948,-56.948,-63.398,-63.398) Navarrete ENVELOPE(-62.533,-62.533,-64.833,-64.833) Tectonophysics 874 230241 |
spellingShingle | Patagonia Intraplate Contraction Tectonic inversion https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Perez Frasette, Maximiliano Jose Navarrete Granzotto, César Rodrigo Bastías Silva, Joaquín Valle, Mauro Nicolás Chew, David Iglesias, Maximiliano Lujan Suárez, Manuel Márquez, Marcelo Drakou, Foteini Folguera, Andrés The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title | The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title_full | The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title_fullStr | The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title_full_unstemmed | The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title_short | The Bajo Grande Basin: Late Jurassic(?)-Early Cretaceous syn-orogenic depocenters in southwestern Gondwana |
title_sort | bajo grande basin: late jurassic(?)-early cretaceous syn-orogenic depocenters in southwestern gondwana |
topic | Patagonia Intraplate Contraction Tectonic inversion https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | Patagonia Intraplate Contraction Tectonic inversion https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/230811 |