The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil

Detalhes bibliográficos
Autor(a) principal: NOWATZKI,CARLOS H.
Data de Publicação: 2000
Outros Autores: KERN,HENRIQUE P.
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=S0001-37652000000200010
Resumo: This paper discusses the facies distribution of Mesozoic eolian sandstones between the Sanga do Cabral and Botucatu formations and also their contact relationships, in São Leopoldo area, State of Rio Grande do Sul (RS), southern Brazil. The main distinctive characteristics regarding these sandstones and formations are the mineralogical composition, paleocurrents and the occurrence of wet interdune deposits. These interdune deposits are characterized by frequent thin mudstone layers with mudcracks, ichnofossils and salt impressions. There are also some features that resemble plant fossils. The distinctive characteristics of these sequences to Sanga do Cabral and Botucatu formations allow us to suggest the informal name of Pedreira Sandstone, considering its type section, the Pedreira Cliff, at Sapucaia do Sul, RS.
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spelling The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, BrazilstratigraphyParaná BasinMesozoicfaciologypaleoenvironmentsThis paper discusses the facies distribution of Mesozoic eolian sandstones between the Sanga do Cabral and Botucatu formations and also their contact relationships, in São Leopoldo area, State of Rio Grande do Sul (RS), southern Brazil. The main distinctive characteristics regarding these sandstones and formations are the mineralogical composition, paleocurrents and the occurrence of wet interdune deposits. These interdune deposits are characterized by frequent thin mudstone layers with mudcracks, ichnofossils and salt impressions. There are also some features that resemble plant fossils. The distinctive characteristics of these sequences to Sanga do Cabral and Botucatu formations allow us to suggest the informal name of Pedreira Sandstone, considering its type section, the Pedreira Cliff, at Sapucaia do Sul, RS.Academia Brasileira de Ciências2000-06-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652000000200010Anais da Academia Brasileira de Ciências v.72 n.2 2000reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/S0001-37652000000200010info:eu-repo/semantics/openAccessNOWATZKI,CARLOS H.KERN,HENRIQUE P.eng2000-08-07T00:00:00Zoai:scielo:S0001-37652000000200010Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2000-08-07T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
title The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
spellingShingle The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
NOWATZKI,CARLOS H.
stratigraphy
Paraná Basin
Mesozoic
faciology
paleoenvironments
title_short The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
title_full The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
title_fullStr The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
title_full_unstemmed The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
title_sort The eolianites between Sanga do Cabral and Botucatu formations in Rio Grande do Sul State, Brazil
author NOWATZKI,CARLOS H.
author_facet NOWATZKI,CARLOS H.
KERN,HENRIQUE P.
author_role author
author2 KERN,HENRIQUE P.
author2_role author
dc.contributor.author.fl_str_mv NOWATZKI,CARLOS H.
KERN,HENRIQUE P.
dc.subject.por.fl_str_mv stratigraphy
Paraná Basin
Mesozoic
faciology
paleoenvironments
topic stratigraphy
Paraná Basin
Mesozoic
faciology
paleoenvironments
description This paper discusses the facies distribution of Mesozoic eolian sandstones between the Sanga do Cabral and Botucatu formations and also their contact relationships, in São Leopoldo area, State of Rio Grande do Sul (RS), southern Brazil. The main distinctive characteristics regarding these sandstones and formations are the mineralogical composition, paleocurrents and the occurrence of wet interdune deposits. These interdune deposits are characterized by frequent thin mudstone layers with mudcracks, ichnofossils and salt impressions. There are also some features that resemble plant fossils. The distinctive characteristics of these sequences to Sanga do Cabral and Botucatu formations allow us to suggest the informal name of Pedreira Sandstone, considering its type section, the Pedreira Cliff, at Sapucaia do Sul, RS.
publishDate 2000
dc.date.none.fl_str_mv 2000-06-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652000000200010
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dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/S0001-37652000000200010
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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.72 n.2 2000
reponame:Anais da Academia Brasileira de Ciências (Online)
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reponame_str Anais da Academia Brasileira de Ciências (Online)
collection Anais da Academia Brasileira de Ciências (Online)
repository.name.fl_str_mv Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)
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