Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up
Petrobras Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) Center for Geosciences Applied to Petroleum Geology - UNESPetro, IGCE/Unesp/Rio Claro Training of Human Resources in Petroleum Geology Program - UNESP Petrobra...
Published in: | Cretaceous Research |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2016
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Online Access: | http://hdl.handle.net/11449/165289 https://doi.org/10.1016/j.cretres.2016.06.014 |
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ftunivespir:oai:repositorio.unesp.br:11449/165289 2023-07-02T03:33:44+02:00 Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up Varejao, Filipe Giovanini Warren, Lucas Verissimo Jesus Perinotto, Jose Alexandre de Neumann, Virginio Henrique Freitas, Bernardo Tavares Almeida, Renato Paes de Assine, Mario Luis Universidade Estadual Paulista (UNESP) 2016-12-01 44-58 http://hdl.handle.net/11449/165289 https://doi.org/10.1016/j.cretres.2016.06.014 eng eng Elsevier B.V. Cretaceous Research http://dx.doi.org/10.1016/j.cretres.2016.06.014 Cretaceous Research. London: Academic Press Ltd- Elsevier Science Ltd, v. 67, p. 44-58, 2016. 0195-6671 http://hdl.handle.net/11449/165289 doi:10.1016/j.cretres.2016.06.014 WOS:000382351000005 WOS000382351000005.pdf 1333845337012256 0471102133658128 openAccess Serra do Tona Marizal Formation Crato Formation Cretaceous paleogeography Microbialites info:eu-repo/semantics/article 2016 ftunivespir https://doi.org/10.1016/j.cretres.2016.06.014 2023-06-12T17:02:51Z Petrobras Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) Center for Geosciences Applied to Petroleum Geology - UNESPetro, IGCE/Unesp/Rio Claro Training of Human Resources in Petroleum Geology Program - UNESP Petrobras: 0050.0023165.06.4 Petrobras: 46.00321584 Processo FAPESP: 2004/15786-0 Processo FAPESP: 2014/16739-8 Processo FAPESP: 2010/51559-0 CNPq: 476727/2004-9 CNPq: 302905/2015-4 Training of Human Resources in Petroleum Geology Program - UNESP: PRH 05 The evolution of the Cretaceous basins of the Brazilian northeastern hinterland was associated with the Gondwana rifting and opening of the South Atlantic Ocean. The first marine ingression in northeastern Brazil occurred in the late Aptian and was recorded as the Santana Group of the Araripe Basin, which is currently an isolated basin, located hundreds of kilometers away from the Brazilian marginal basins. Bellow the first upper Aptian marine deposits, an important section of fossiliferous limestone (Lagerstatte) was deposited and preserved in the Crato Formation transitioning upward into evaporites of the Ipubi Formation. The direction of the marine ingression is controversial, with several possibilities being suggested, mainly due to the absence of other areas of upper Aptian marine sections within the hinterland. Serra do Tona is a sedimentary mesa with scarped edges where the upper part of the Marizal Formation crops out, displaying laminated limestones, litho-and chrono-correlated with those of the Crato Formation, is preserved. Therefore, this mixed upper Aptian section, at the North Tucano Basin (Serra do Tona), is a unique occurrence of utmost importance to the definition of sedimentary events and paleogeographical reconstruction of northeastern Brazil during the late Aptian. A detailed stratigraphic analysis allowed the definition and characterization of two upper Aptian depositional sequences bounded by regional disconformities. Both ... Article in Journal/Newspaper South Atlantic Ocean Universidade Estadual Paulista São Paulo: Repositório Institucional UNESP Claro ENVELOPE(-63.383,-63.383,-64.250,-64.250) Cretaceous Research 67 44 58 |
institution |
Open Polar |
collection |
Universidade Estadual Paulista São Paulo: Repositório Institucional UNESP |
op_collection_id |
ftunivespir |
language |
English |
topic |
Serra do Tona Marizal Formation Crato Formation Cretaceous paleogeography Microbialites |
spellingShingle |
Serra do Tona Marizal Formation Crato Formation Cretaceous paleogeography Microbialites Varejao, Filipe Giovanini Warren, Lucas Verissimo Jesus Perinotto, Jose Alexandre de Neumann, Virginio Henrique Freitas, Bernardo Tavares Almeida, Renato Paes de Assine, Mario Luis Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
topic_facet |
Serra do Tona Marizal Formation Crato Formation Cretaceous paleogeography Microbialites |
description |
Petrobras Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) Center for Geosciences Applied to Petroleum Geology - UNESPetro, IGCE/Unesp/Rio Claro Training of Human Resources in Petroleum Geology Program - UNESP Petrobras: 0050.0023165.06.4 Petrobras: 46.00321584 Processo FAPESP: 2004/15786-0 Processo FAPESP: 2014/16739-8 Processo FAPESP: 2010/51559-0 CNPq: 476727/2004-9 CNPq: 302905/2015-4 Training of Human Resources in Petroleum Geology Program - UNESP: PRH 05 The evolution of the Cretaceous basins of the Brazilian northeastern hinterland was associated with the Gondwana rifting and opening of the South Atlantic Ocean. The first marine ingression in northeastern Brazil occurred in the late Aptian and was recorded as the Santana Group of the Araripe Basin, which is currently an isolated basin, located hundreds of kilometers away from the Brazilian marginal basins. Bellow the first upper Aptian marine deposits, an important section of fossiliferous limestone (Lagerstatte) was deposited and preserved in the Crato Formation transitioning upward into evaporites of the Ipubi Formation. The direction of the marine ingression is controversial, with several possibilities being suggested, mainly due to the absence of other areas of upper Aptian marine sections within the hinterland. Serra do Tona is a sedimentary mesa with scarped edges where the upper part of the Marizal Formation crops out, displaying laminated limestones, litho-and chrono-correlated with those of the Crato Formation, is preserved. Therefore, this mixed upper Aptian section, at the North Tucano Basin (Serra do Tona), is a unique occurrence of utmost importance to the definition of sedimentary events and paleogeographical reconstruction of northeastern Brazil during the late Aptian. A detailed stratigraphic analysis allowed the definition and characterization of two upper Aptian depositional sequences bounded by regional disconformities. Both ... |
author2 |
Universidade Estadual Paulista (UNESP) |
format |
Article in Journal/Newspaper |
author |
Varejao, Filipe Giovanini Warren, Lucas Verissimo Jesus Perinotto, Jose Alexandre de Neumann, Virginio Henrique Freitas, Bernardo Tavares Almeida, Renato Paes de Assine, Mario Luis |
author_facet |
Varejao, Filipe Giovanini Warren, Lucas Verissimo Jesus Perinotto, Jose Alexandre de Neumann, Virginio Henrique Freitas, Bernardo Tavares Almeida, Renato Paes de Assine, Mario Luis |
author_sort |
Varejao, Filipe Giovanini |
title |
Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
title_short |
Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
title_full |
Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
title_fullStr |
Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
title_full_unstemmed |
Upper Aptian mixed carbonate-siliciclastic sequences from Tucano Basin, Northeastern Brazil: Implications for paleogeographic reconstructions following Gondwana break-up |
title_sort |
upper aptian mixed carbonate-siliciclastic sequences from tucano basin, northeastern brazil: implications for paleogeographic reconstructions following gondwana break-up |
publisher |
Elsevier B.V. |
publishDate |
2016 |
url |
http://hdl.handle.net/11449/165289 https://doi.org/10.1016/j.cretres.2016.06.014 |
long_lat |
ENVELOPE(-63.383,-63.383,-64.250,-64.250) |
geographic |
Claro |
geographic_facet |
Claro |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
Cretaceous Research http://dx.doi.org/10.1016/j.cretres.2016.06.014 Cretaceous Research. London: Academic Press Ltd- Elsevier Science Ltd, v. 67, p. 44-58, 2016. 0195-6671 http://hdl.handle.net/11449/165289 doi:10.1016/j.cretres.2016.06.014 WOS:000382351000005 WOS000382351000005.pdf 1333845337012256 0471102133658128 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.1016/j.cretres.2016.06.014 |
container_title |
Cretaceous Research |
container_volume |
67 |
container_start_page |
44 |
op_container_end_page |
58 |
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1770273792170393600 |