/img alt="Imagem da capa" class="recordcover" src="""/>
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...
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 |