Výsledky vyhledávání - "José Renato Nogueira"

Akademický článek

Geology and Lithogeochemistry of the Supracrustal Sequence and Interlayered Metabasites of NE Santos Dumont Region (MG)

Autor: Renata Hiraga, José Renato Nogueira, Beatriz Paschoal Duarte, Claudia Sayão Valladares, Vinicius de Oliveira Monteiro Guimarães, Rodrigo Peternel

Publikováno v: Anuário do Instituto de Geociências, Vol 40, Iss 3, Pp 359-376 (2017)

The region near Santos Dumont town consists of a sequence of interlayered metabasic rocks and supracrustal gneisses. Two lithological units were individualized based on geological-structural mapping (1:50,000), petrography and lithogeochemistry: a

Externí odkaz: https://doaj.org/article/95fea5d6eb88497db6f876953a2316e7

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Unraveling CO2-rich fluids and daughter minerals recorded in fluid and mineral inclusions from the Martin Vaz archipelago, Vitória-Trindade Ridge (VTR), South Atlantic

Autor: André Leite de Oliveira, Anderson Costa dos Santos, José Renato Nogueira, Lucília A.R. de Oliveira, Dailto Silva, Gabriela Rodrigues Caitano, Lucas Guimarães Pereira Monteiro

Publikováno v: Journal of South American Earth Sciences. 127:104365

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6cbbacbcfdc296c7abf1f7651678e4b7
https://doi.org/10.1016/j.jsames.2023.104365

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Geologia e Litogeoquímica da Sequência Supracrustal e Metabasitos Intercalados da Região NE de Santos Dumont (MG)

Autor: Beatriz Paschoal Duarte, Rodrigo Peternel, Renata Hiraga, José Renato Nogueira, Vinicius de Oliveira Monteiro Guimarães, Claudia Sayão Valladares

Publikováno v: Anuário do Instituto de Geociências - UFRJ. 40:359-376

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a65d2a47be8dbde226a31ad8a01f5697
https://doi.org/10.11137/2017_3_359_376

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Geology and Lithogeochemistry of the Supracrustal Sequence and Interlayered Metabasites of NE Santos Dumont Region (MG)

Autor: Renata Hiraga, José Renato Nogueira, Beatriz Paschoal Duarte, Claudia Sayão Valladares, Vinicius de Oliveira Monteiro Guimarães, Rodrigo Peternel

Publikováno v: Anuário do Instituto de Geociências; Vol 40, No 3 (2017); 359-376
Anuário do Instituto de Geociências
Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
Anuário do Instituto de Geociências, Vol 40, Iss 3, Pp 359-376 (2017)

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::df47fde7fabd4e97620caa06860403bb
https://revistas.ufrj.br/index.php/aigeo/article/view/27240

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Evolution of reworked Paleoproterozoic basement rocks within the Ribeira belt (Neoproterozoic), SE-Brazil, based on U–Pb geochronology: Implications for paleogeographic reconstructions of the São Francisco-Congo paleocontinent

Autor: Nuno Machado, Claudio de Morisson Valeriano, Beatriz Paschoal Duarte, Monica Heilbron, José Renato Nogueira, Antonio Simonetti

Publikováno v: Precambrian Research. 178:136-148

Geological, geochemical and geochronological data suggest that the basement exposed in the Occidental terrane of the Neoproterozoic-Ordovician Ribeira belt represents the continuation of the Sao Francisco paleocontinent, which was amalgamated at the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5b649b3a4d61a1755a6c3ef426ab85f7
https://doi.org/10.1016/j.precamres.2010.02.002

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GEOTECTONIC MODELS AND GEOLOGIC EVOLUTION OF THE HIGH-GRADE GNEISS TERRANES OF JUIZ DE FORA (MG), BRAZIL

Autor: JOSÉ RENATO NOGUEIRA, ASIT CHOUDHURI

Publikováno v: Revista Brasileira de Geociências. 30:169-173

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f73ad5da60968480dfb87b6f11818878
https://doi.org/10.25249/0375-7536.2000301169173

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The Juiz De Fora Granulite Complex of the Central Ribeira Belt, SE Brazil: A Paleoproterozoic Crustal Segment Thrust During the Pan-African Orogeny

Autor: José Renato Nogueira, Beatriz Paschoal Duarte, Monica Heilbron

Publikováno v: Gondwana Research. 1:373-381

The granulites of the Juiz de Fora complex occur within thick basement thrust slices associated with the Pan-African shortening process in the central segment of the Ribeira belt. Five lithological units of the Intermediate tectonic domain of the bel

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::dc181eac5bbe48abc28a4ba10a8f747d
https://doi.org/10.1016/s1342-937x(05)70853-4

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PYROXENES AND THE P-T PATH IN GRANULITE FACIES OF SW MINAS GERAIS, BRAZIL

Autor: Asit Choudhuri, S. S. Iyer, José Renato Nogueira

Publikováno v: Revista Brasileira de Geociências. 27:49-52

RESUMO PIROXENOS E O PERCURSO P-T EM FACIES GRANULITO DO SW DE MINAS GERAIS, BRASIL Piroxenios de facies granulito do Macico de Guaxupe apresentam exsolucoes caracteristicas na forma de lamelas paralelas a (001) em clinopiroxenios calcicos e, por vez

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ead7852c0ce690f740802f8940c0c5a8
https://doi.org/10.25249/0375-7536.19974952

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GEOLOGIA DA FAIXA RIBEIRA SETENTRIONAL: ESTADO DA ARTE E CONEXÕES COM A FAIXA ARAÇUAÍ

Autor: Monica Heilbron, Célia Diana Ragatky, Isabel Pereira Ludka, Julio Cesar Horta de Almeida, José Renato Nogueira, Miguel Tupinambá, Claudia Sayão Valladares, Julio Cezar Mendes, Alan Wanderley Albuquerque Miranda, Silvia Regina Batistuzzo de Medeiros, Luiz Guilherme do Eirado Silva, Clayton Guia de Almeida, Beatriz Paschoal Duarte

Publikováno v: Revista Geonomos; Geonomos-v.15 n. 1 (2007)
BASE-Bielefeld Academic Search Engine

As unidades litológicas da região noroeste do Estado do Rio de Janeiro e sul do Espírito Santo estão situadasno segmento setentrional da Faixa Ribeira. O conhecimento da estruturação tectônica deste segmento dafaixa possibilita sua correlaçã

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bcc3b779a376c7120f1edf6463780cec
https://seer.ufmg.br/index.php/revistageonomos/article/view/12544

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GRANULITE FACIES ROCKS FROM GUAXUPÉ, MG: GNEISS-FLUID SEQUENCES AND P-T CONDITIONS

Autor: Gergely Sabó, José Renato Nogueira, Dailto Silva, Asit Choudhuri

Publikováno v: Revista Geonomos; Geonomos-v.3 n. 2 (1995)
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP

Gnaisses de fácies granulito nos arredores de Guaxupé formaram-se em condições de P-T estimadas em 8-9 Kb/800-900°C, e depois sofreram descompressão P-T-t em virtude dosoerguimento. O limite inferior deste caminho é estimado em 5-6 Kb/600-700�

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c2b3e5daa4fd283d65eae4d98916fc1c
https://seer.ufmg.br/index.php/revistageonomos/article/view/12425

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