The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)

The Capiru Group is a Neoproterozoic metasedimentary unit that crops out in the Curitiba terrane, Southern Ribeira Belt, Brazil. A detailed geological mapping of this unit was performed during 2016 to 2020. Original interpretations and the new geological map were compiled and integrated with the pas...

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Autores principales:	Larissa da Rocha Santos, André Luis Spisila, Daniel Patias Guimarães, Luizemara Szameitat, Alessandra de Barros e Silva Bongiolo, Leonardo Fadel Cury
Formato:	article
Lenguaje:	EN
Publicado:	Taylor & Francis Group 2021
Materias:	neoproterozoic curitiba microplate southern ribeira belt brasiliano – pan african orogeny south atlantic opening cenozoic rift of southern brazil Maps G3180-9980
Acceso en línea:	https://doaj.org/article/1cb384d54ed242c08020345ebc1ea997
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spelling	oai:doaj.org-article:1cb384d54ed242c08020345ebc1ea9972021-12-01T14:40:59ZThe geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)1744-564710.1080/17445647.2021.1982036https://doaj.org/article/1cb384d54ed242c08020345ebc1ea9972021-12-01T00:00:00Zhttp://dx.doi.org/10.1080/17445647.2021.1982036https://doaj.org/toc/1744-5647The Capiru Group is a Neoproterozoic metasedimentary unit that crops out in the Curitiba terrane, Southern Ribeira Belt, Brazil. A detailed geological mapping of this unit was performed during 2016 to 2020. Original interpretations and the new geological map were compiled and integrated with the past field data of the state (MINEROPAR) and national (CPRM) geological surveys, and to unpublished and recent published studies. This compilation represents the most updated synthesis of the Capiru Group, and provides the basis for recognition and individualization of lithostratigraphic units. The lithostratigraphic units reflect depositional/tectonic events, which involved: a) passive continental margin deposition on the Curitiba microplate, b) compressional episodes during the Brasiliano - Pan African Orogeny (Late Neoproterozoic), c) extensional processes that followed the collision stage (Cambrian), and finally, the d) extensional tectonics related to the Gondwana break-up during the Lower Cretaceous, that culminated to the Proto-Atlantic Ocean opening.Larissa da Rocha SantosAndré Luis SpisilaDaniel Patias GuimarãesLuizemara SzameitatAlessandra de Barros e Silva BongioloLeonardo Fadel CuryTaylor & Francis Grouparticleneoproterozoiccuritiba microplatesouthern ribeira beltbrasiliano – pan african orogenysouth atlantic openingcenozoic rift of southern brazilMapsG3180-9980ENJournal of Maps, Vol 17, Iss 2, Pp 779-787 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	neoproterozoic curitiba microplate southern ribeira belt brasiliano – pan african orogeny south atlantic opening cenozoic rift of southern brazil Maps G3180-9980
spellingShingle	neoproterozoic curitiba microplate southern ribeira belt brasiliano – pan african orogeny south atlantic opening cenozoic rift of southern brazil Maps G3180-9980 Larissa da Rocha Santos André Luis Spisila Daniel Patias Guimarães Luizemara Szameitat Alessandra de Barros e Silva Bongiolo Leonardo Fadel Cury The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
description	The Capiru Group is a Neoproterozoic metasedimentary unit that crops out in the Curitiba terrane, Southern Ribeira Belt, Brazil. A detailed geological mapping of this unit was performed during 2016 to 2020. Original interpretations and the new geological map were compiled and integrated with the past field data of the state (MINEROPAR) and national (CPRM) geological surveys, and to unpublished and recent published studies. This compilation represents the most updated synthesis of the Capiru Group, and provides the basis for recognition and individualization of lithostratigraphic units. The lithostratigraphic units reflect depositional/tectonic events, which involved: a) passive continental margin deposition on the Curitiba microplate, b) compressional episodes during the Brasiliano - Pan African Orogeny (Late Neoproterozoic), c) extensional processes that followed the collision stage (Cambrian), and finally, the d) extensional tectonics related to the Gondwana break-up during the Lower Cretaceous, that culminated to the Proto-Atlantic Ocean opening.
format	article
author	Larissa da Rocha Santos André Luis Spisila Daniel Patias Guimarães Luizemara Szameitat Alessandra de Barros e Silva Bongiolo Leonardo Fadel Cury
author_facet	Larissa da Rocha Santos André Luis Spisila Daniel Patias Guimarães Luizemara Szameitat Alessandra de Barros e Silva Bongiolo Leonardo Fadel Cury
author_sort	Larissa da Rocha Santos
title	The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
title_short	The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
title_full	The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
title_fullStr	The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
title_full_unstemmed	The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)
title_sort	geology of the capiru group, curitiba terrane, southern ribeira belt (brazil)
publisher	Taylor & Francis Group
publishDate	2021
url	https://doaj.org/article/1cb384d54ed242c08020345ebc1ea997
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The geology of the Capiru Group, Curitiba Terrane, Southern Ribeira Belt (Brazil)

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