Artigo

Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton

The Furna Azul Migmatite is a ~10 km2 complex located in Pontes e Lacerda city, Mato Grosso, Brazil. It belongs to Paraguá Terrane, limit with Rio Alegre Terrane, southeast of San Ignacio Province, in Amazon Craton. It consists of transitional metatexites with amphibolite enclaves and dioritic injec...

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Autor principal: NASCIMENTO, Newton Diego Couto do
Outros Autores: RUIZ, Amarildo Salina, PIEROSAN, Ronaldo, LIMA, Gabrielle Aparecida de, MATOS, João Batista, LAFON, Jean Michel, MOURA, Candido Augusto Veloso
Grau: Artigo
Idioma: por
Publicado em: Universidade Federal do Pará 2017
Assuntos:
Acesso em linha: http://repositorio.ufpa.br/jspui/handle/2011/8319
id ir-2011-8319
recordtype dspace
spelling ir-2011-83192017-10-16T11:59:37Z Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton Petrogênese, geocronologia U-Pb e Sm-Nd do Migmatito Furna Azul: evidência de fusão parcial durante a Orogenia San Ignácio, Terreno Paraguá, SW do Cráton Amazônico NASCIMENTO, Newton Diego Couto do RUIZ, Amarildo Salina PIEROSAN, Ronaldo LIMA, Gabrielle Aparecida de MATOS, João Batista LAFON, Jean Michel MOURA, Candido Augusto Veloso Petrogênese Geocronologia Geologia regional Petrografia Metatexito The Furna Azul Migmatite is a ~10 km2 complex located in Pontes e Lacerda city, Mato Grosso, Brazil. It belongs to Paraguá Terrane, limit with Rio Alegre Terrane, southeast of San Ignacio Province, in Amazon Craton. It consists of transitional metatexites with amphibolite enclaves and dioritic injections. The rocks were divided in residuum rich and leucosome rich; both have three deformation phases marked by folded stromatic layers affected by spaced foliation and metamorphosed in amphibolite facies, represented by garnet, biotite, sillimanite, and by the clinopyroxene in the enclaves. The metamorphic retrograde to greenschist is marked by formation of chlorite, muscovite and prehnite. Residuum-rich metatexites show higher CaO and Na2O contents, separating them from K2O, Ba and Rb enriched transitional metatexites. U-Pb on zircon and Sm-Nd whole-rocks dating indicates that the residuum-rich metatexite crystallized at 1436 ± 11 Ma, with a TDM age of 1.90 Ga and εNd(1.43) of -0.54, whereas the dioritic injection crystallized at 1341,7 ± 17 Ma with a TDM age of 1.47 Ga and εNd(1.34) of 3.39. These results indicate that the Furna Azul Migmatite protolith was formed during the San Ignácio Orogeny and was reworked during the same orogeny, as basement for collisional to post-magmatic granites from Pensamiento Intrusive Suite. O Migmatito Furna Azul é um complexo de ~10 km2 localizado em Pontes e Lacerda, Mato Grosso, Brasil. Pertence ao Terreno Paraguá, próximo ao limite com o Terreno Rio Alegre, sudeste da Província Rondoniana - San Ignácio - Cráton Amazônico. O migmatito consiste de metatexitos transicionais com enclaves anfibolíticos e injeções dioríticas. Os metatexitos são distinguidos em ricos em resíduo e ricos em leucossoma e exibem três fases deformacionais marcadas pelo bandamento estromático dobrado afetado por uma xistosidade espaçada e metamorfisados na fácies anfibolito alto, representada por granada, biotita e sillimanita, bem como pela formação de clinopiroxênio nos enclaves. O retrometamorfismo para a fácies xisto verde é marcado pela formação de clorita, muscovita/sericita e prehnita. O metatexito rico em resíduo apresenta maiores teores de CaO, Na 2O, separando-os do metatexito transicional enriquecidos em K2O, Ba e Rb. Comparando com produtos de anatexia, nota-se uma afinidade com produtos de protólitos tonalíticos e/ou anfibolíticos. Os dados geocronológicos (U-Pb SHRIMP em zircão e Sm-Nd em rocha total) mostraram que o metatexito rico em resíduo teve sua cristalização em 1436 ± 11 Ma, com idade modelo TDM de 1,90 Ga e ε Nd(1,43) de -0,54, enquanto a injeção diorítica cristalizou em 1341.7 ± 17 Ma com idade modelo TDM de 1,47 Ga e ε Nd(1,34) de 3,39. Esses resultados evidenciam que o protólito do Migmatito Furna Azul teria sido formado durante a Orogenia San Ignácio (1.43 Ga) posteriormente retrabalhado, servindo de embasamento para o magmatismo tardi a pós-colisional representado pela Suíte Intrusiva Pensamiento. 2017-05-09T11:41:36Z 2017-05-09T11:41:36Z 2016-06 Artigo de Periódico NASCIMENTO, Newton Diego Couto do et al. Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton. Brazilian Journal of Geology, São Paulo, v. 46, n. 2, p. 239-259, abr/jun. 2016. Disponível em: <http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892016000200239&lng=pt&nrm=iso>. Acesso em: 05 maio 2017. <http://dx.doi.org/10.1590/2317-4889201620160030>. 2317-4692 http://repositorio.ufpa.br/jspui/handle/2011/8319 por Brazilian Journal of Geology Acesso Aberto application/pdf Universidade Federal do Pará Brasil UFPA
institution Repositório Institucional - Universidade Federal do Pará
collection RI-UFPA
language por
topic Petrogênese
Geocronologia
Geologia regional
Petrografia
Metatexito
spellingShingle Petrogênese
Geocronologia
Geologia regional
Petrografia
Metatexito
NASCIMENTO, Newton Diego Couto do
Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
topic_facet Petrogênese
Geocronologia
Geologia regional
Petrografia
Metatexito
description The Furna Azul Migmatite is a ~10 km2 complex located in Pontes e Lacerda city, Mato Grosso, Brazil. It belongs to Paraguá Terrane, limit with Rio Alegre Terrane, southeast of San Ignacio Province, in Amazon Craton. It consists of transitional metatexites with amphibolite enclaves and dioritic injections. The rocks were divided in residuum rich and leucosome rich; both have three deformation phases marked by folded stromatic layers affected by spaced foliation and metamorphosed in amphibolite facies, represented by garnet, biotite, sillimanite, and by the clinopyroxene in the enclaves. The metamorphic retrograde to greenschist is marked by formation of chlorite, muscovite and prehnite. Residuum-rich metatexites show higher CaO and Na2O contents, separating them from K2O, Ba and Rb enriched transitional metatexites. U-Pb on zircon and Sm-Nd whole-rocks dating indicates that the residuum-rich metatexite crystallized at 1436 ± 11 Ma, with a TDM age of 1.90 Ga and εNd(1.43) of -0.54, whereas the dioritic injection crystallized at 1341,7 ± 17 Ma with a TDM age of 1.47 Ga and εNd(1.34) of 3.39. These results indicate that the Furna Azul Migmatite protolith was formed during the San Ignácio Orogeny and was reworked during the same orogeny, as basement for collisional to post-magmatic granites from Pensamiento Intrusive Suite.
format Artigo
author NASCIMENTO, Newton Diego Couto do
author2 RUIZ, Amarildo Salina
PIEROSAN, Ronaldo
LIMA, Gabrielle Aparecida de
MATOS, João Batista
LAFON, Jean Michel
MOURA, Candido Augusto Veloso
author2Str RUIZ, Amarildo Salina
PIEROSAN, Ronaldo
LIMA, Gabrielle Aparecida de
MATOS, João Batista
LAFON, Jean Michel
MOURA, Candido Augusto Veloso
title Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
title_short Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
title_full Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
title_fullStr Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
title_full_unstemmed Petrogenesis, U-Pb and Sm-Nd geochronology of the Furna Azul Migmatite: partial melting evidence during the San Ignácio Orogeny, Paraguá Terrane, SW Amazon Craton
title_sort petrogenesis, u-pb and sm-nd geochronology of the furna azul migmatite: partial melting evidence during the san ignácio orogeny, paraguá terrane, sw amazon craton
publisher Universidade Federal do Pará
publishDate 2017
url http://repositorio.ufpa.br/jspui/handle/2011/8319
_version_ 1832603383531307008
score 11.755432