Petrografia, química mineral e geotermobarometria de metapelito do grupo carrancas na Nappe de Luminárias (MG)

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dc.contributor.authorFumes, Regiane Andrade [UNESP]
dc.contributor.authorLuvizotto, George Luiz [UNESP]
dc.contributor.authorMoraes, Renato
dc.contributor.authorFerraz, Edson Ricardo Maia [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.date.accessioned2018-12-11T16:51:50Z
dc.date.available2018-12-11T16:51:50Z
dc.date.issued2017-01-01
dc.description.abstractThe Luminárias Nappe is a NNE-SSW elongated structure, located in the southern portion of the Neoproterozoic Brasília Orogen, which borders the São Francisco Craton, MG, Brazil. It is composed of metapelite and quartzite from the Carrancas Group. The present work focuses on the metamorphic characterization of the Luminárias Nappe by means of petrography, mineral chemistry and average PT method of THERMOCALC. In the northern portion, the paragenesis is Chl+St+Ky+Rt+Qtz+Ms; in the center-north it is St+Grt+Bt+Rt+Qtz+Ms and in the southern it is Grt+Ky+St+Rt+Qtz+Ms. Retrometamorphic chlorite is observed in the center-north and southern portions, while retrometamorphic biotite is observed in the southern portion. Mineral chemistry data on the rock forming minerals show differences in the composition of minerals from the northern, center-north and southern portion of the Luminárias Nappe. Metamorphic peak conditions (average PT) in the center-northern portion are 570 ±67 ˚C and 9.4 ±1.9 kbar, in the southern portion are 609 ±63 ˚C and 11.4 ±3.9 kbar. Results indicate the presence of a metamorphic gradient with conditions increasing from lower amphibolite facies in the northern and center-north to medium amphibolite in the southern portion, both at high-pressures.en
dc.description.affiliationUniversidade Estadual Paulista (Unesp) Instituto de Geociências e Ciências Exatas
dc.description.affiliationUniversidade de São Paulo Instituto de Geociências
dc.description.affiliationUnespUniversidade Estadual Paulista (Unesp) Instituto de Geociências e Ciências Exatas
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.description.sponsorshipIdCAPES: 2013/04007-0
dc.description.sponsorshipIdFAPESP: 2013/04007-0
dc.description.sponsorshipIdCAPES: 2015/05230-0
dc.description.sponsorshipIdFAPESP: 2015/05230-0
dc.description.sponsorshipIdCAPES: 2015/07750-5
dc.description.sponsorshipIdFAPESP: 2015/07750-5
dc.format.extent639-654
dc.identifier.citationGeociencias, v. 36, n. 4, p. 639-654, 2017.
dc.identifier.issn1980-900X
dc.identifier.issn0101-9082
dc.identifier.scopus2-s2.0-85041797870
dc.identifier.urihttp://hdl.handle.net/11449/170649
dc.language.isopor
dc.relation.ispartofGeociencias
dc.relation.ispartofsjr0,230
dc.rights.accessRightsAcesso restrito
dc.sourceScopus
dc.subjectAverage PT
dc.subjectCarrancas group
dc.subjectHigh-pressure amphibolite facies
dc.subjectMineral chemistry
dc.subjectTHERMOCALC
dc.titlePetrografia, química mineral e geotermobarometria de metapelito do grupo carrancas na Nappe de Luminárias (MG)pt
dc.title.alternativePetrography, mineral chemistry and thermobarometry of metapelite of the carrancas group in the LuminÁrias Nappe – Minas Gerais – Brazilen
dc.typeArtigo
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