Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil

Detalhes bibliográficos
Autor(a) principal: Rossetti, Dilce F.
Data de Publicação: 2013
Outros Autores: Bezerra, Francisco Hilário Rego, Dominguez, José Maria Landim
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFBA
Texto Completo: http://repositorio.ufba.br/ri/handle/ri/13327
Resumo: Texto completo. Acesso restrito. p. 87–112
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spelling Rossetti, Dilce F.Bezerra, Francisco Hilário RegoDominguez, José Maria Landim2013-10-30T16:41:21Z20130012-8252http://repositorio.ufba.br/ri/handle/ri/13327v. 123Texto completo. Acesso restrito. p. 87–112The seaboard of Brazil is a highly favorable setting for studying episodes of worldwide sea-level rise because of its passive nature. Previous studies of the equatorial coast of Brazil have led to the recognition of extensive Oligo-Miocene and Miocene marine-influenced deposits, but these deposits have been overlooked in other coastal areas of Brazil. The aim of the present study is to show the origin and evolution of late Oligocene and Miocene marine-influenced strata exposed in more than 5000 km of coastal areas along the WNW-trending equatorial and NNE-trending eastern Brazilian continental margins. We review the most relevant data concerning the strata of these ages exposed along the equatorial and eastern margins of Brazil, and combine them with new data. Based on these occurrences, we analyze the history of sea-level fluctuations and show that marine-influenced strata are more widespread in these margins than originally thought. Our main results indicate that a marine influence is not only imprinted in the deposits exposed along the equatorial margin, but it is also widespread in several areas of the eastern margin. For a long geological time interval ranging from the end of the Cretaceous or Paleogene up to the late Oligocene, most of the Brazilian coast remained a non-depositional site exposed to subaerial erosion and lateritic soil development. The combination of sea-level rise and tectonic subsidence promoted sediment accumulation in the onshore portion of several basins. Two transgressive episodes occurred: one in the Oligo-Miocene and another in the early/middle Miocene. The latter gave rise to deposition of the Barreiras Formation. However, during the supposedly middle Miocene eustatic sea-level highstand in coastal Brazil, there was a renewed and extensive phase of non-deposition and subaerial erosion with lateritic soil formation, a process that lasted up to the Late Quaternary. This mismatching of the sedimentary record with other South American and continental areas is discussed herein. As in many other areas of South America and of the world, the regressive–transgressive events recorded along the Brazilian coast most likely responded to a combination of eustatic sea-level fluctuations and local factors such as tectonic activity, intraplate stresses and changes in dynamic topography during the post-rift history of the eastern South American Plate.Submitted by Santiago Fabio (fabio.ssantiago@hotmail.com) on 2013-10-15T17:11:40Z No. of bitstreams: 1 aaaazs.pdf: 41210 bytes, checksum: ee00930f59f7591f66c75569d8cb3e4d (MD5)Approved for entry into archive by Rodrigo Meirelles (rodrigomei@ufba.br) on 2013-10-30T16:41:21Z (GMT) No. of bitstreams: 1 aaaazs.pdf: 41210 bytes, checksum: ee00930f59f7591f66c75569d8cb3e4d (MD5)Made available in DSpace on 2013-10-30T16:41:21Z (GMT). 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dc.title.pt_BR.fl_str_mv Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
dc.title.alternative.pt_BR.fl_str_mv Earth-Science Reviews
title Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
spellingShingle Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
Rossetti, Dilce F.
Miocene
Continental Brazilian margin
Tidal processes
Transgressions
Sea level
Tectonics
title_short Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
title_full Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
title_fullStr Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
title_full_unstemmed Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
title_sort Late Oligocene–Miocene transgressions along the equatorial and eastern margins of Brazil
author Rossetti, Dilce F.
author_facet Rossetti, Dilce F.
Bezerra, Francisco Hilário Rego
Dominguez, José Maria Landim
author_role author
author2 Bezerra, Francisco Hilário Rego
Dominguez, José Maria Landim
author2_role author
author
dc.contributor.author.fl_str_mv Rossetti, Dilce F.
Bezerra, Francisco Hilário Rego
Dominguez, José Maria Landim
dc.subject.por.fl_str_mv Miocene
Continental Brazilian margin
Tidal processes
Transgressions
Sea level
Tectonics
topic Miocene
Continental Brazilian margin
Tidal processes
Transgressions
Sea level
Tectonics
description Texto completo. Acesso restrito. p. 87–112
publishDate 2013
dc.date.accessioned.fl_str_mv 2013-10-30T16:41:21Z
dc.date.issued.fl_str_mv 2013
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://repositorio.ufba.br/ri/handle/ri/13327
dc.identifier.issn.none.fl_str_mv 0012-8252
dc.identifier.number.pt_BR.fl_str_mv v. 123
identifier_str_mv 0012-8252
v. 123
url http://repositorio.ufba.br/ri/handle/ri/13327
dc.language.iso.fl_str_mv eng
language eng
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Earth-Science Reviews
dc.publisher.country.fl_str_mv Brasil
publisher.none.fl_str_mv Earth-Science Reviews
dc.source.pt_BR.fl_str_mv http://www.sciencedirect.com/science/article/pii/S0012825213000792
dc.source.none.fl_str_mv reponame:Repositório Institucional da UFBA
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