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Influencia do soerguimento do alto Paranaiba na sedimentacao pos- basaltica na area do Triangulo Mineiro (MG), borda NNE da Bacia do Parana

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dc.contributor.authorBarcelos, J. H.
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T07:11:52Z
dc.date.available2014-05-27T07:11:52Z
dc.date.issued1989-12-01
dc.description.abstractFaciologic analysis method was applied to after-basaltic sedimentary deposits in Triangulo Mineiro (MG) area. Faciologic association 1 (Adamantina formation) and unities 1 to 5 (Uberaba formation) are related to the fluvial and lake deposits: faciologic association 3 (Ponte Alta Member) and 2 (Sierra da Galga Member) represent the sedimentary deposits associated to the alluvial fans conditions. With faciologic association and unities it could be to recognize the paleogeografic and tectonic conditions in sedimentation time of that depositional tract. -English summaryen
dc.format.extent37-54
dc.identifier.citationGeociencias, v. 8, p. 37-54.
dc.identifier.issn0101-9082
dc.identifier.scopus2-s2.0-0024894704
dc.identifier.urihttp://hdl.handle.net/11449/63940
dc.language.isopor
dc.relation.ispartofGeociências
dc.relation.ispartofsjr0,230
dc.rights.accessRightsAcesso restrito
dc.sourceScopus
dc.subjectAdamantina Formation
dc.subjectCretaceous
dc.subjectlake deposit
dc.subjectsedimentation
dc.subjecttectonics
dc.subjectUberaba formation
dc.subjectuplift
dc.subjectBrazil, Parana Basin, Triangulo Mineiro area
dc.titleInfluencia do soerguimento do alto Paranaiba na sedimentacao pos- basaltica na area do Triangulo Mineiro (MG), borda NNE da Bacia do Paranapt
dc.title.alternativeInfluence of the Alto Paranaiba uplift in post-basaltic sedimentation of the Triangulo Mineiro (MG) area, NNE border of the Parana Basinen
dc.typeArtigo
dcterms.licensehttp://www.revistageociencias.com.br/
dspace.entity.typePublication

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