Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust

Detalhes bibliográficos
Autor(a) principal: Hernandez Tasco, Lizeth
Data de Publicação: 2020
Tipo de documento: Dissertação
Idioma: eng
Título da fonte: Biblioteca Digital de Teses e Dissertações da USP
Texto Completo: https://www.teses.usp.br/teses/disponiveis/44/44143/tde-01032021-110432/
Resumo: The main objective of this study is to contribute to the understanding of deformation of leucosome and its residue, in diatexites and granulites, using as examples two units of the Nappe Socorro-Guaxupé, the metatexite unit and the basal granulite unit, from the southernmost portion of the Brasília Orogen. The first is dominated by metasedimentary rocks, although has a name of metatexite unit, it is dominated by diatexite at its base, and the second, is composed primarily by felsic granulite. In oriented samples, after textural characterization, the quartz caxis fabric thermomether and cathodoluminescence (CL) images, where Ti in quartz evidences temperature domains, were used to determine the deformation temperature, which was compared with thermobarometry data in the respective residues. In this way, it was established that the crystallization in the basal granulite and metatexite units occurred along the cooling portion of the P-T path, but in some portions, it was deformed and might be related to medium and high temperatures. During the metamorphism of the amphibolite and granulite facies, synanatectic deformation with melt crystallization and late deformation in solid-state occurred. Therefore, when the granulite is in the solid state, the diatexite is still in the dominantly liquid state, causing the granulite to register those higher deformation temperatures that the diatexite cannot register due to its still mostly liquid state.
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spelling Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crustnão disponívelEixo-c de quartzoFusão parcialLeucosomeLeucossomaNappe Socorro-GuaxupéNappe Socorro-GuaxupéPartial meltingQuartz c-axis fabricTi em quartzoTi in quartzThe main objective of this study is to contribute to the understanding of deformation of leucosome and its residue, in diatexites and granulites, using as examples two units of the Nappe Socorro-Guaxupé, the metatexite unit and the basal granulite unit, from the southernmost portion of the Brasília Orogen. The first is dominated by metasedimentary rocks, although has a name of metatexite unit, it is dominated by diatexite at its base, and the second, is composed primarily by felsic granulite. In oriented samples, after textural characterization, the quartz caxis fabric thermomether and cathodoluminescence (CL) images, where Ti in quartz evidences temperature domains, were used to determine the deformation temperature, which was compared with thermobarometry data in the respective residues. In this way, it was established that the crystallization in the basal granulite and metatexite units occurred along the cooling portion of the P-T path, but in some portions, it was deformed and might be related to medium and high temperatures. During the metamorphism of the amphibolite and granulite facies, synanatectic deformation with melt crystallization and late deformation in solid-state occurred. Therefore, when the granulite is in the solid state, the diatexite is still in the dominantly liquid state, causing the granulite to register those higher deformation temperatures that the diatexite cannot register due to its still mostly liquid state.O objetivo principal deste estudo é contribuir para o entendimento da deformação do leucossoma e seus resíduos, em diatexitos e granulitos, utilizando como exemplos duas unidades da Nappe Socorro-Guaxupé, a unidade metatexito e a unidade granulíto basal, da porção mais meridional do Orógeno Brasília. A primeira é dominada por rochas metassedimentares, embora tenha o nome de unidade metatexíto, é dominada por diatexito em sua base, e a segunda, é composta principalmente por granulito félsico. Nas amostras orientadas, após a caracterização textural, o termômetro do eixo c de quartzo e imagens de catodoluminescência (CL), em que o Ti no quartzo indica temperatura, foram utilizados para determinar a temperatura de deformação, a qual foi comparada com os dados de termobarometria nos respectivos resíduos. Desta forma, foi estabelecido que a cristalização nas unidades basais de granulito e metatexito ocorreu ao longo da porção de resfriamento da trajetória P-T, mas em algumas porções foi deformada e pode estar relacionada a médias e altas temperaturas. Durante o metamorfismo das fácies anfibolito e granulito, ocorreu deformação sin-anatética com cristalização por fusão e deformação tardia no estado sólido. Portanto, quando o granulito está no estado sólido, o diatexito ainda está no estado dominantemente líquido, fazendo com que o granulito registre aquelas temperaturas de deformação mais altas que os diatexitos não puderam registrar devido ao seu estado ainda dominantemente líquido.Biblioteca Digitais de Teses e Dissertações da USPMoraes, Renato deHernandez Tasco, Lizeth 2020-12-18info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisapplication/pdfhttps://www.teses.usp.br/teses/disponiveis/44/44143/tde-01032021-110432/reponame:Biblioteca Digital de Teses e Dissertações da USPinstname:Universidade de São Paulo (USP)instacron:USPLiberar o conteúdo para acesso público.info:eu-repo/semantics/openAccesseng2021-03-03T14:13:02Zoai:teses.usp.br:tde-01032021-110432Biblioteca Digital de Teses e Dissertaçõeshttp://www.teses.usp.br/PUBhttp://www.teses.usp.br/cgi-bin/mtd2br.plvirginia@if.usp.br|| atendimento@aguia.usp.br||virginia@if.usp.bropendoar:27212021-03-03T14:13:02Biblioteca Digital de Teses e Dissertações da USP - Universidade de São Paulo (USP)false
dc.title.none.fl_str_mv Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
não disponível
title Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
spellingShingle Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
Hernandez Tasco, Lizeth
Eixo-c de quartzo
Fusão parcial
Leucosome
Leucossoma
Nappe Socorro-Guaxupé
Nappe Socorro-Guaxupé
Partial melting
Quartz c-axis fabric
Ti em quartzo
Ti in quartz
title_short Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
title_full Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
title_fullStr Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
title_full_unstemmed Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
title_sort Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes in the rheology of the lower continental crust
author Hernandez Tasco, Lizeth
author_facet Hernandez Tasco, Lizeth
author_role author
dc.contributor.none.fl_str_mv Moraes, Renato de
dc.contributor.author.fl_str_mv Hernandez Tasco, Lizeth
dc.subject.por.fl_str_mv Eixo-c de quartzo
Fusão parcial
Leucosome
Leucossoma
Nappe Socorro-Guaxupé
Nappe Socorro-Guaxupé
Partial melting
Quartz c-axis fabric
Ti em quartzo
Ti in quartz
topic Eixo-c de quartzo
Fusão parcial
Leucosome
Leucossoma
Nappe Socorro-Guaxupé
Nappe Socorro-Guaxupé
Partial melting
Quartz c-axis fabric
Ti em quartzo
Ti in quartz
description The main objective of this study is to contribute to the understanding of deformation of leucosome and its residue, in diatexites and granulites, using as examples two units of the Nappe Socorro-Guaxupé, the metatexite unit and the basal granulite unit, from the southernmost portion of the Brasília Orogen. The first is dominated by metasedimentary rocks, although has a name of metatexite unit, it is dominated by diatexite at its base, and the second, is composed primarily by felsic granulite. In oriented samples, after textural characterization, the quartz caxis fabric thermomether and cathodoluminescence (CL) images, where Ti in quartz evidences temperature domains, were used to determine the deformation temperature, which was compared with thermobarometry data in the respective residues. In this way, it was established that the crystallization in the basal granulite and metatexite units occurred along the cooling portion of the P-T path, but in some portions, it was deformed and might be related to medium and high temperatures. During the metamorphism of the amphibolite and granulite facies, synanatectic deformation with melt crystallization and late deformation in solid-state occurred. Therefore, when the granulite is in the solid state, the diatexite is still in the dominantly liquid state, causing the granulite to register those higher deformation temperatures that the diatexite cannot register due to its still mostly liquid state.
publishDate 2020
dc.date.none.fl_str_mv 2020-12-18
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://www.teses.usp.br/teses/disponiveis/44/44143/tde-01032021-110432/
url https://www.teses.usp.br/teses/disponiveis/44/44143/tde-01032021-110432/
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv
dc.rights.driver.fl_str_mv Liberar o conteúdo para acesso público.
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Liberar o conteúdo para acesso público.
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.coverage.none.fl_str_mv
dc.publisher.none.fl_str_mv Biblioteca Digitais de Teses e Dissertações da USP
publisher.none.fl_str_mv Biblioteca Digitais de Teses e Dissertações da USP
dc.source.none.fl_str_mv
reponame:Biblioteca Digital de Teses e Dissertações da USP
instname:Universidade de São Paulo (USP)
instacron:USP
instname_str Universidade de São Paulo (USP)
instacron_str USP
institution USP
reponame_str Biblioteca Digital de Teses e Dissertações da USP
collection Biblioteca Digital de Teses e Dissertações da USP
repository.name.fl_str_mv Biblioteca Digital de Teses e Dissertações da USP - Universidade de São Paulo (USP)
repository.mail.fl_str_mv virginia@if.usp.br|| atendimento@aguia.usp.br||virginia@if.usp.br
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