The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast

Detalhes bibliográficos
Autor(a) principal: Mio,Giuliano de
Data de Publicação: 2007
Outros Autores: Giacheti,Heraldo L.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652007000100017
Resumo: Correlations between mapping units of costal sedimentary basin and interpretation of piezocone test results are presented and discussed based on examples from Caravelas strandplain, (State of Bahia), Paranaguá (State of Paraná) and Guarujá bays (State of São Paulo), Brazil. Recognizing that the sedimentary environment was mainly controlled by sea level fluctuations led to the interpretation of transgressive and regressive sedimentary sequences, which is in a good agreement with the sea level fluctuation curves currently accepted for these regions. The interpretation of piezocone test results shows that the sedimentary sequences of Caravelas and Guarujá sites are similar and they have a good correlation to the sea level fluctuation curve accepted for Salvador region, State of Bahia. On the other hand, the piezocone test results from Paranaguá site indicate a different sedimentary sequence from the previous ones, relating to the sea level fluctuation curve accepted for Paranaguá region. The results show the high applicability of piezocone testing for stratigraphical logging and suggest that it is possible to integrate it with other current techniques used for paleo-environmental studies in Brazil, in accordance with recent approaches used in international research on the subject.
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spelling The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coaststratigraphic loggingpiezocone testpaleoenvironmentgeological mappingCorrelations between mapping units of costal sedimentary basin and interpretation of piezocone test results are presented and discussed based on examples from Caravelas strandplain, (State of Bahia), Paranaguá (State of Paraná) and Guarujá bays (State of São Paulo), Brazil. Recognizing that the sedimentary environment was mainly controlled by sea level fluctuations led to the interpretation of transgressive and regressive sedimentary sequences, which is in a good agreement with the sea level fluctuation curves currently accepted for these regions. The interpretation of piezocone test results shows that the sedimentary sequences of Caravelas and Guarujá sites are similar and they have a good correlation to the sea level fluctuation curve accepted for Salvador region, State of Bahia. On the other hand, the piezocone test results from Paranaguá site indicate a different sedimentary sequence from the previous ones, relating to the sea level fluctuation curve accepted for Paranaguá region. The results show the high applicability of piezocone testing for stratigraphical logging and suggest that it is possible to integrate it with other current techniques used for paleo-environmental studies in Brazil, in accordance with recent approaches used in international research on the subject.Academia Brasileira de Ciências2007-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652007000100017Anais da Academia Brasileira de Ciências v.79 n.1 2007reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/S0001-37652007000100017info:eu-repo/semantics/openAccessMio,Giuliano deGiacheti,Heraldo L.eng2007-03-23T00:00:00Zoai:scielo:S0001-37652007000100017Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2007-03-23T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
title The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
spellingShingle The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
Mio,Giuliano de
stratigraphic logging
piezocone test
paleoenvironment
geological mapping
title_short The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
title_full The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
title_fullStr The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
title_full_unstemmed The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
title_sort The use of piezocone tests for high-resolution stratigraphy of Quaternary sediment sequences in the Brazilian coast
author Mio,Giuliano de
author_facet Mio,Giuliano de
Giacheti,Heraldo L.
author_role author
author2 Giacheti,Heraldo L.
author2_role author
dc.contributor.author.fl_str_mv Mio,Giuliano de
Giacheti,Heraldo L.
dc.subject.por.fl_str_mv stratigraphic logging
piezocone test
paleoenvironment
geological mapping
topic stratigraphic logging
piezocone test
paleoenvironment
geological mapping
description Correlations between mapping units of costal sedimentary basin and interpretation of piezocone test results are presented and discussed based on examples from Caravelas strandplain, (State of Bahia), Paranaguá (State of Paraná) and Guarujá bays (State of São Paulo), Brazil. Recognizing that the sedimentary environment was mainly controlled by sea level fluctuations led to the interpretation of transgressive and regressive sedimentary sequences, which is in a good agreement with the sea level fluctuation curves currently accepted for these regions. The interpretation of piezocone test results shows that the sedimentary sequences of Caravelas and Guarujá sites are similar and they have a good correlation to the sea level fluctuation curve accepted for Salvador region, State of Bahia. On the other hand, the piezocone test results from Paranaguá site indicate a different sedimentary sequence from the previous ones, relating to the sea level fluctuation curve accepted for Paranaguá region. The results show the high applicability of piezocone testing for stratigraphical logging and suggest that it is possible to integrate it with other current techniques used for paleo-environmental studies in Brazil, in accordance with recent approaches used in international research on the subject.
publishDate 2007
dc.date.none.fl_str_mv 2007-03-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652007000100017
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652007000100017
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/S0001-37652007000100017
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.79 n.1 2007
reponame:Anais da Academia Brasileira de Ciências (Online)
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instname_str Academia Brasileira de Ciências (ABC)
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reponame_str Anais da Academia Brasileira de Ciências (Online)
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