U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana
Zircon U-Pb geochronology was applied to investigate the provenance, depositional ages, and paleogeography of the southwestern Gondwana in detrital and ash fall sediments from Carboniferous to Jurassic succession of the southern Paraná Basin. Four detrital age populations suggest provenance from loc...
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| Aineistotyyppi: | Artikkeli |
| Kieli: | English |
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MDPI AG
2023-07-01
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| Sarja: | Geosciences |
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| Linkit: | https://www.mdpi.com/2076-3263/13/8/225 |
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| author | Ruy Paulo Philipp Ubiratan Ferrucio Faccini Cesar Leandro Schultz Gustavo Zvirtes Matheus Philippe Bruckmann Ernesto Lavina Joice Cagliari Andrea Ritter Jelinek Renata Guimarães Netto Adriano Roessler Viana Miguel Angelo Stipp Basei |
| author_facet | Ruy Paulo Philipp Ubiratan Ferrucio Faccini Cesar Leandro Schultz Gustavo Zvirtes Matheus Philippe Bruckmann Ernesto Lavina Joice Cagliari Andrea Ritter Jelinek Renata Guimarães Netto Adriano Roessler Viana Miguel Angelo Stipp Basei |
| author_sort | Ruy Paulo Philipp |
| collection | DOAJ |
| description | Zircon U-Pb geochronology was applied to investigate the provenance, depositional ages, and paleogeography of the southwestern Gondwana in detrital and ash fall sediments from Carboniferous to Jurassic succession of the southern Paraná Basin. Four detrital age populations suggest provenance from local and distal sources located to the south, southeast, and southwest: (i) Archean to Paleoproterozoic zircons from the Rio de La Plata Craton, Nico Peres and Taquarembó terranes; (ii) Grenvillian zircons from the basement of the Gondwanides and Namaqua–Natal belts; (iii) Neoproterozoic grains from the Don Feliciano Belt; and (iv) Phanerozoic populations from Paleozoic orogenic belts and related foreland systems in Argentina, as well as eroded units of the Paraná Basin. The paleogeographic reconstruction indicates an evolution in three distinct stages: (1) a gulf open to the Panthalassa Ocean during the Carboniferous; (2) an epicontinental sea with the rise of the Gondwanides Orogeny during the Permian; and (3) continental deposits controlled by an intra-plate graben system during the Triassic. Permian–Triassic volcanogenic zircons provide constrained maximum depositional ages and attested persistent volcanism, related to the Choiyoi magmatism and effects of the climate change episodes. During the Triassic, the extensional graben system recorded the uplift of the basement through regional northwest and northeast fault systems, and the recycling of Permian zircons, modifying source-to-sink relationships. |
| first_indexed | 2024-03-10T23:54:04Z |
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| id | doaj.art-22fba03f55b341269fcc0465e2f2d930 |
| institution | Directory Open Access Journal |
| issn | 2076-3263 |
| language | English |
| last_indexed | 2024-03-10T23:54:04Z |
| publishDate | 2023-07-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Geosciences |
| spelling | doaj.art-22fba03f55b341269fcc0465e2f2d9302023-11-19T01:16:50ZengMDPI AGGeosciences2076-32632023-07-0113822510.3390/geosciences13080225U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW GondwanaRuy Paulo Philipp0Ubiratan Ferrucio Faccini1Cesar Leandro Schultz2Gustavo Zvirtes3Matheus Philippe Bruckmann4Ernesto Lavina5Joice Cagliari6Andrea Ritter Jelinek7Renata Guimarães Netto8Adriano Roessler Viana9Miguel Angelo Stipp Basei10Centro de Estudos em Petrologia e Geoquímica (CPGq), Instituto de Geociências, Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre 90010-150, RS, BrazilPrograma de Pós-Graduação em Geologia, Departamento de Geologia, Universidade do Vale do Rio dos Sinos (UNISINOS), São Leopoldo 93022-750, RS, BrazilCentro de Estudos em Petrologia e Geoquímica (CPGq), Instituto de Geociências, Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre 90010-150, RS, BrazilDepartment of Geology and Geophysics, University of Aberdeen (UoA), Aberdeen AB24 3FX, UKCentro de Estudos em Petrologia e Geoquímica (CPGq), Instituto de Geociências, Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre 90010-150, RS, BrazilPrograma de Pós-Graduação em Geologia, Departamento de Geologia, Universidade do Vale do Rio dos Sinos (UNISINOS), São Leopoldo 93022-750, RS, BrazilPrograma de Pós-Graduação em Geologia, Departamento de Geologia, Universidade do Vale do Rio dos Sinos (UNISINOS), São Leopoldo 93022-750, RS, BrazilCentro de Estudos em Petrologia e Geoquímica (CPGq), Instituto de Geociências, Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre 90010-150, RS, BrazilPrograma de Pós-Graduação em Geologia, Departamento de Geologia, Universidade do Vale do Rio dos Sinos (UNISINOS), São Leopoldo 93022-750, RS, BrazilPETROBRAS S.A., Rio de Janeiro 20031-912, RJ, BrazilCentro de Pesquisas Geocronológicas (CPGEO), Instituto de Geociências, USP, São Paulo 13083-896, SP, BrazilZircon U-Pb geochronology was applied to investigate the provenance, depositional ages, and paleogeography of the southwestern Gondwana in detrital and ash fall sediments from Carboniferous to Jurassic succession of the southern Paraná Basin. Four detrital age populations suggest provenance from local and distal sources located to the south, southeast, and southwest: (i) Archean to Paleoproterozoic zircons from the Rio de La Plata Craton, Nico Peres and Taquarembó terranes; (ii) Grenvillian zircons from the basement of the Gondwanides and Namaqua–Natal belts; (iii) Neoproterozoic grains from the Don Feliciano Belt; and (iv) Phanerozoic populations from Paleozoic orogenic belts and related foreland systems in Argentina, as well as eroded units of the Paraná Basin. The paleogeographic reconstruction indicates an evolution in three distinct stages: (1) a gulf open to the Panthalassa Ocean during the Carboniferous; (2) an epicontinental sea with the rise of the Gondwanides Orogeny during the Permian; and (3) continental deposits controlled by an intra-plate graben system during the Triassic. Permian–Triassic volcanogenic zircons provide constrained maximum depositional ages and attested persistent volcanism, related to the Choiyoi magmatism and effects of the climate change episodes. During the Triassic, the extensional graben system recorded the uplift of the basement through regional northwest and northeast fault systems, and the recycling of Permian zircons, modifying source-to-sink relationships.https://www.mdpi.com/2076-3263/13/8/225paraná basinzircon geochronologygondwanagondwanides beltprovenanceash fall layers |
| spellingShingle | Ruy Paulo Philipp Ubiratan Ferrucio Faccini Cesar Leandro Schultz Gustavo Zvirtes Matheus Philippe Bruckmann Ernesto Lavina Joice Cagliari Andrea Ritter Jelinek Renata Guimarães Netto Adriano Roessler Viana Miguel Angelo Stipp Basei U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana Geosciences paraná basin zircon geochronology gondwana gondwanides belt provenance ash fall layers |
| title | U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana |
| title_full | U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana |
| title_fullStr | U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana |
| title_full_unstemmed | U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana |
| title_short | U-Pb Zircon Geochronology of Detrital and Ash Fall Deposits of the Southern Paraná Basin: A Contribution for Provenance, Tectonic Evolution, and the Paleogeography of the SW Gondwana |
| title_sort | u pb zircon geochronology of detrital and ash fall deposits of the southern parana basin a contribution for provenance tectonic evolution and the paleogeography of the sw gondwana |
| topic | paraná basin zircon geochronology gondwana gondwanides belt provenance ash fall layers |
| url | https://www.mdpi.com/2076-3263/13/8/225 |
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