Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil

Detalhes bibliográficos
Autor(a) principal: Bezerra, Francisco Hilário Rego
Data de Publicação: 2001
Outros Autores: Amaro, Venerando Eustáquio, Vita-Finzi, Claudio, Saadi, Allaoua
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFRN
Texto Completo: https://repositorio.ufrn.br/handle/123456789/31231
Resumo: Although the last major tectonic event in the Brazilian passive margin was the South America–Africa breakup during the Mesozoic, there is pervasive evidence in northeastern Brazil for pronounced faulting since the late Tertiary. The faulting was partitioned between strike-slip and normal-slip and it reactivated Precambrian shear zones as well as generating new structures. A 040–060° -trending fault set and a 300–320° -trending set have strongly influenced both the deposition of alluvial and aeolian sediments and coastal evolution. Vertical throws have attained 260 m since the Pliocene, and topographic breaks resulting from cumulative late Tertiary to Quaternary slip have attained 30–40 m. Fault control of sediment deposition and coastal morphology may have affected the entire South American passive margin
id UFRN_c8903b3d58a4b70222e5483a7ce5c4d5
oai_identifier_str oai:https://repositorio.ufrn.br:123456789/31231
network_acronym_str UFRN
network_name_str Repositório Institucional da UFRN
repository_id_str
spelling Bezerra, Francisco Hilário RegoAmaro, Venerando EustáquioVita-Finzi, ClaudioSaadi, Allaoua2021-01-07T18:29:21Z2021-01-07T18:29:21Z2001-04BEZERRA, F. H. R.; AMARO, V. E.; VITA-FINZI, C.; SAADI, A.. Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil. Journal of South American Earth Sciences, v. 14, p. 61-75, 2001. Disponível em: https://www.sciencedirect.com/science/article/abs/pii/S0895981101000098?via%3Dihub. Acesso em: 29 dez. 2020. https://doi.org/10.1016/S0895-9811(01)00009-80895-9811https://repositorio.ufrn.br/handle/123456789/3123110.1016/S0895-9811(01)00009-8ElsevierAttribution 3.0 Brazilhttp://creativecommons.org/licenses/by/3.0/br/info:eu-repo/semantics/openAccessCenozoicSedimentationCoastal plain morphologyFault controlNE BrazilPliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleAlthough the last major tectonic event in the Brazilian passive margin was the South America–Africa breakup during the Mesozoic, there is pervasive evidence in northeastern Brazil for pronounced faulting since the late Tertiary. The faulting was partitioned between strike-slip and normal-slip and it reactivated Precambrian shear zones as well as generating new structures. A 040–060° -trending fault set and a 300–320° -trending set have strongly influenced both the deposition of alluvial and aeolian sediments and coastal evolution. Vertical throws have attained 260 m since the Pliocene, and topographic breaks resulting from cumulative late Tertiary to Quaternary slip have attained 30–40 m. Fault control of sediment deposition and coastal morphology may have affected the entire South American passive marginengreponame:Repositório Institucional da UFRNinstname:Universidade Federal do Rio Grande do Norte (UFRN)instacron:UFRNCC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8914https://repositorio.ufrn.br/bitstream/123456789/31231/2/license_rdf4d2950bda3d176f570a9f8b328dfbbefMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-81484https://repositorio.ufrn.br/bitstream/123456789/31231/3/license.txte9597aa2854d128fd968be5edc8a28d9MD53ORIGINALPliocene-QuaternaryFault_AMARO_2001.pdfPliocene-QuaternaryFault_AMARO_2001.pdfapplication/pdf1617569https://repositorio.ufrn.br/bitstream/123456789/31231/1/Pliocene-QuaternaryFault_AMARO_2001.pdf449a1931717cd933f874f5380147b40cMD51TEXTPliocene-QuaternaryFault_AMARO_2001.pdf.txtPliocene-QuaternaryFault_AMARO_2001.pdf.txtExtracted texttext/plain46702https://repositorio.ufrn.br/bitstream/123456789/31231/4/Pliocene-QuaternaryFault_AMARO_2001.pdf.txta3b5fce61b447507914716c4881400b9MD54THUMBNAILPliocene-QuaternaryFault_AMARO_2001.pdf.jpgPliocene-QuaternaryFault_AMARO_2001.pdf.jpgGenerated Thumbnailimage/jpeg1769https://repositorio.ufrn.br/bitstream/123456789/31231/5/Pliocene-QuaternaryFault_AMARO_2001.pdf.jpg118f338e0e6f8f90ce8df795d0f7765fMD55123456789/312312021-01-10 04:54:17.925oai:https://repositorio.ufrn.br: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Repositório de PublicaçõesPUBhttp://repositorio.ufrn.br/oai/opendoar:2021-01-10T07:54:17Repositório Institucional da UFRN - Universidade Federal do Rio Grande do Norte (UFRN)false
dc.title.pt_BR.fl_str_mv Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
title Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
spellingShingle Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
Bezerra, Francisco Hilário Rego
Cenozoic
Sedimentation
Coastal plain morphology
Fault control
NE Brazil
title_short Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
title_full Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
title_fullStr Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
title_full_unstemmed Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
title_sort Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil
author Bezerra, Francisco Hilário Rego
author_facet Bezerra, Francisco Hilário Rego
Amaro, Venerando Eustáquio
Vita-Finzi, Claudio
Saadi, Allaoua
author_role author
author2 Amaro, Venerando Eustáquio
Vita-Finzi, Claudio
Saadi, Allaoua
author2_role author
author
author
dc.contributor.author.fl_str_mv Bezerra, Francisco Hilário Rego
Amaro, Venerando Eustáquio
Vita-Finzi, Claudio
Saadi, Allaoua
dc.subject.por.fl_str_mv Cenozoic
Sedimentation
Coastal plain morphology
Fault control
NE Brazil
topic Cenozoic
Sedimentation
Coastal plain morphology
Fault control
NE Brazil
description Although the last major tectonic event in the Brazilian passive margin was the South America–Africa breakup during the Mesozoic, there is pervasive evidence in northeastern Brazil for pronounced faulting since the late Tertiary. The faulting was partitioned between strike-slip and normal-slip and it reactivated Precambrian shear zones as well as generating new structures. A 040–060° -trending fault set and a 300–320° -trending set have strongly influenced both the deposition of alluvial and aeolian sediments and coastal evolution. Vertical throws have attained 260 m since the Pliocene, and topographic breaks resulting from cumulative late Tertiary to Quaternary slip have attained 30–40 m. Fault control of sediment deposition and coastal morphology may have affected the entire South American passive margin
publishDate 2001
dc.date.issued.fl_str_mv 2001-04
dc.date.accessioned.fl_str_mv 2021-01-07T18:29:21Z
dc.date.available.fl_str_mv 2021-01-07T18:29:21Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.citation.fl_str_mv BEZERRA, F. H. R.; AMARO, V. E.; VITA-FINZI, C.; SAADI, A.. Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil. Journal of South American Earth Sciences, v. 14, p. 61-75, 2001. Disponível em: https://www.sciencedirect.com/science/article/abs/pii/S0895981101000098?via%3Dihub. Acesso em: 29 dez. 2020. https://doi.org/10.1016/S0895-9811(01)00009-8
dc.identifier.uri.fl_str_mv https://repositorio.ufrn.br/handle/123456789/31231
dc.identifier.issn.none.fl_str_mv 0895-9811
dc.identifier.doi.none.fl_str_mv 10.1016/S0895-9811(01)00009-8
identifier_str_mv BEZERRA, F. H. R.; AMARO, V. E.; VITA-FINZI, C.; SAADI, A.. Pliocene-Quaternary fault control of sedimentation and coastal plain morphology in NE Brazil. Journal of South American Earth Sciences, v. 14, p. 61-75, 2001. Disponível em: https://www.sciencedirect.com/science/article/abs/pii/S0895981101000098?via%3Dihub. Acesso em: 29 dez. 2020. https://doi.org/10.1016/S0895-9811(01)00009-8
0895-9811
10.1016/S0895-9811(01)00009-8
url https://repositorio.ufrn.br/handle/123456789/31231
dc.language.iso.fl_str_mv eng
language eng
dc.rights.driver.fl_str_mv Attribution 3.0 Brazil
http://creativecommons.org/licenses/by/3.0/br/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Attribution 3.0 Brazil
http://creativecommons.org/licenses/by/3.0/br/
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:Repositório Institucional da UFRN
instname:Universidade Federal do Rio Grande do Norte (UFRN)
instacron:UFRN
instname_str Universidade Federal do Rio Grande do Norte (UFRN)
instacron_str UFRN
institution UFRN
reponame_str Repositório Institucional da UFRN
collection Repositório Institucional da UFRN
bitstream.url.fl_str_mv https://repositorio.ufrn.br/bitstream/123456789/31231/2/license_rdf
https://repositorio.ufrn.br/bitstream/123456789/31231/3/license.txt
https://repositorio.ufrn.br/bitstream/123456789/31231/1/Pliocene-QuaternaryFault_AMARO_2001.pdf
https://repositorio.ufrn.br/bitstream/123456789/31231/4/Pliocene-QuaternaryFault_AMARO_2001.pdf.txt
https://repositorio.ufrn.br/bitstream/123456789/31231/5/Pliocene-QuaternaryFault_AMARO_2001.pdf.jpg
bitstream.checksum.fl_str_mv 4d2950bda3d176f570a9f8b328dfbbef
e9597aa2854d128fd968be5edc8a28d9
449a1931717cd933f874f5380147b40c
a3b5fce61b447507914716c4881400b9
118f338e0e6f8f90ce8df795d0f7765f
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
MD5
MD5
repository.name.fl_str_mv Repositório Institucional da UFRN - Universidade Federal do Rio Grande do Norte (UFRN)
repository.mail.fl_str_mv
_version_ 1814833062802882560

Registros relacionados