The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina
- Autores
- Alasino, Pablo Horacio; Casquet, C.; Larrovere, Mariano Alexis; Pankhurst, R. J.; Galindo, C.; Dahlquist, J. A.; Baldo, Edgardo Gaspar Agustin; Rapela, Carlos Washington
- Año de publicación
- 2014
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- A more than 12 km wide sheeted tonalite complex in western Sierra de Famatina, NW Argentina, was emplaced at middle crust levels (ca 5 kbar), coeval with regional metamorphism during an early phase of the Ordovician Famatinian orogeny (ca. 480 Ma). Advective heat from the tonalite complex caused a rise in the host regional temperatures (≤ 700ºC) by a maximum of ca. 100ºC, developing an aureole (~3 km wide) parallel to the igneous contact. This was accompanied by significant melting (ca 40 %) of the host rocks that hybridized to a variable extent with the tonalitic magmas. Three metamorphic zones were distinguished in a cross-section through the aureole: (1) an external zone consisting of metatexitic gneisses, amphibolites and minor tonalites, (2) an intermediate zone formed by screens of highly melted gneisses, amphibolites and metagabbros lying between tonalite and newly formed leucogranitoid and hybrid rock sheets, (3) an internal zone formed almost exclusively of massive tonalite and minor hybrid rocks. Incongruent melting of biotite in gneisses of the intermediate zone produced peritectic cordierite and garnet. Hybrids resulting from variable mixing of anatectic granitoids and tonalite magma developed in the innermost part of the aureole at 750-800ºC. Increased water activity within this zone eventually promoted increased melting of plagioclase + quartz in the gneisses. Leucogranitoid magmas formed in part by extraction from the hybrid magmas led to heterogeneity of the Sr-isotope composition. The Cerro Toro contact aureole shows that assimilation of metasedimentary rocks through partial melting can play an important role during emplacement of tonalitic magmas at mid-crustal levels.
Fil: Alasino, Pablo Horacio. Universidad Nacional de la Rioja; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; Argentina
Fil: Casquet, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; España
Fil: Larrovere, Mariano Alexis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; Argentina. Universidad Nacional de la Rioja; Argentina
Fil: Pankhurst, R. J.. British Geological Survey; Reino Unido
Fil: Galindo, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; España
Fil: Dahlquist, J. A.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; Argentina
Fil: Baldo, Edgardo Gaspar Agustin. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; Argentina
Fil: Rapela, Carlos Washington. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico La Plata. Centro de Investigaciones Geológicas (i); Argentina. Universidad Nacional de La Plata; Argentina - Materia
-
I-Type Magmatism
Middle Crust Emplacement
Anatexis
Hybridization
Sierra de Famatina - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/12099
Ver los metadatos del registro completo
id |
CONICETDig_f5d5f63e673bb05d2f0e0e1a0053646f |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/12099 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
spelling |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW ArgentinaAlasino, Pablo HoracioCasquet, C.Larrovere, Mariano AlexisPankhurst, R. J.Galindo, C.Dahlquist, J. A.Baldo, Edgardo Gaspar AgustinRapela, Carlos WashingtonI-Type MagmatismMiddle Crust EmplacementAnatexisHybridizationSierra de Famatinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1A more than 12 km wide sheeted tonalite complex in western Sierra de Famatina, NW Argentina, was emplaced at middle crust levels (ca 5 kbar), coeval with regional metamorphism during an early phase of the Ordovician Famatinian orogeny (ca. 480 Ma). Advective heat from the tonalite complex caused a rise in the host regional temperatures (≤ 700ºC) by a maximum of ca. 100ºC, developing an aureole (~3 km wide) parallel to the igneous contact. This was accompanied by significant melting (ca 40 %) of the host rocks that hybridized to a variable extent with the tonalitic magmas. Three metamorphic zones were distinguished in a cross-section through the aureole: (1) an external zone consisting of metatexitic gneisses, amphibolites and minor tonalites, (2) an intermediate zone formed by screens of highly melted gneisses, amphibolites and metagabbros lying between tonalite and newly formed leucogranitoid and hybrid rock sheets, (3) an internal zone formed almost exclusively of massive tonalite and minor hybrid rocks. Incongruent melting of biotite in gneisses of the intermediate zone produced peritectic cordierite and garnet. Hybrids resulting from variable mixing of anatectic granitoids and tonalite magma developed in the innermost part of the aureole at 750-800ºC. Increased water activity within this zone eventually promoted increased melting of plagioclase + quartz in the gneisses. Leucogranitoid magmas formed in part by extraction from the hybrid magmas led to heterogeneity of the Sr-isotope composition. The Cerro Toro contact aureole shows that assimilation of metasedimentary rocks through partial melting can play an important role during emplacement of tonalitic magmas at mid-crustal levels.Fil: Alasino, Pablo Horacio. Universidad Nacional de la Rioja; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; ArgentinaFil: Casquet, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; EspañaFil: Larrovere, Mariano Alexis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; Argentina. Universidad Nacional de la Rioja; ArgentinaFil: Pankhurst, R. J.. British Geological Survey; Reino UnidoFil: Galindo, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; EspañaFil: Dahlquist, J. A.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; ArgentinaFil: Baldo, Edgardo Gaspar Agustin. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; ArgentinaFil: Rapela, Carlos Washington. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico La Plata. Centro de Investigaciones Geológicas (i); Argentina. Universidad Nacional de La Plata; ArgentinaElsevier Science2014-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/12099Alasino, Pablo Horacio; Casquet, C.; Larrovere, Mariano Alexis; Pankhurst, R. J.; Galindo, C.; et al.; The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina; Elsevier Science; Lithos; 190-191; 3-2014; 154-1720024-4937enginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0024493713004088info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2013.12.006info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:53:08Zoai:ri.conicet.gov.ar:11336/12099instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:53:08.659CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
title |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
spellingShingle |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina Alasino, Pablo Horacio I-Type Magmatism Middle Crust Emplacement Anatexis Hybridization Sierra de Famatina |
title_short |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
title_full |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
title_fullStr |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
title_full_unstemmed |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
title_sort |
The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina |
dc.creator.none.fl_str_mv |
Alasino, Pablo Horacio Casquet, C. Larrovere, Mariano Alexis Pankhurst, R. J. Galindo, C. Dahlquist, J. A. Baldo, Edgardo Gaspar Agustin Rapela, Carlos Washington |
author |
Alasino, Pablo Horacio |
author_facet |
Alasino, Pablo Horacio Casquet, C. Larrovere, Mariano Alexis Pankhurst, R. J. Galindo, C. Dahlquist, J. A. Baldo, Edgardo Gaspar Agustin Rapela, Carlos Washington |
author_role |
author |
author2 |
Casquet, C. Larrovere, Mariano Alexis Pankhurst, R. J. Galindo, C. Dahlquist, J. A. Baldo, Edgardo Gaspar Agustin Rapela, Carlos Washington |
author2_role |
author author author author author author author |
dc.subject.none.fl_str_mv |
I-Type Magmatism Middle Crust Emplacement Anatexis Hybridization Sierra de Famatina |
topic |
I-Type Magmatism Middle Crust Emplacement Anatexis Hybridization Sierra de Famatina |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
A more than 12 km wide sheeted tonalite complex in western Sierra de Famatina, NW Argentina, was emplaced at middle crust levels (ca 5 kbar), coeval with regional metamorphism during an early phase of the Ordovician Famatinian orogeny (ca. 480 Ma). Advective heat from the tonalite complex caused a rise in the host regional temperatures (≤ 700ºC) by a maximum of ca. 100ºC, developing an aureole (~3 km wide) parallel to the igneous contact. This was accompanied by significant melting (ca 40 %) of the host rocks that hybridized to a variable extent with the tonalitic magmas. Three metamorphic zones were distinguished in a cross-section through the aureole: (1) an external zone consisting of metatexitic gneisses, amphibolites and minor tonalites, (2) an intermediate zone formed by screens of highly melted gneisses, amphibolites and metagabbros lying between tonalite and newly formed leucogranitoid and hybrid rock sheets, (3) an internal zone formed almost exclusively of massive tonalite and minor hybrid rocks. Incongruent melting of biotite in gneisses of the intermediate zone produced peritectic cordierite and garnet. Hybrids resulting from variable mixing of anatectic granitoids and tonalite magma developed in the innermost part of the aureole at 750-800ºC. Increased water activity within this zone eventually promoted increased melting of plagioclase + quartz in the gneisses. Leucogranitoid magmas formed in part by extraction from the hybrid magmas led to heterogeneity of the Sr-isotope composition. The Cerro Toro contact aureole shows that assimilation of metasedimentary rocks through partial melting can play an important role during emplacement of tonalitic magmas at mid-crustal levels. Fil: Alasino, Pablo Horacio. Universidad Nacional de la Rioja; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; Argentina Fil: Casquet, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; España Fil: Larrovere, Mariano Alexis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Regional de Investigaciones Cientificas y Transferencia Tecnológica de Anillaco; Argentina. Universidad Nacional de la Rioja; Argentina Fil: Pankhurst, R. J.. British Geological Survey; Reino Unido Fil: Galindo, C.. Consejo Superior de Investigaciones Cientificas; España. Universidad Complutense de Madrid; España Fil: Dahlquist, J. A.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; Argentina Fil: Baldo, Edgardo Gaspar Agustin. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Córdoba. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Universidad Nacional de Córdoba; Argentina Fil: Rapela, Carlos Washington. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico La Plata. Centro de Investigaciones Geológicas (i); Argentina. Universidad Nacional de La Plata; Argentina |
description |
A more than 12 km wide sheeted tonalite complex in western Sierra de Famatina, NW Argentina, was emplaced at middle crust levels (ca 5 kbar), coeval with regional metamorphism during an early phase of the Ordovician Famatinian orogeny (ca. 480 Ma). Advective heat from the tonalite complex caused a rise in the host regional temperatures (≤ 700ºC) by a maximum of ca. 100ºC, developing an aureole (~3 km wide) parallel to the igneous contact. This was accompanied by significant melting (ca 40 %) of the host rocks that hybridized to a variable extent with the tonalitic magmas. Three metamorphic zones were distinguished in a cross-section through the aureole: (1) an external zone consisting of metatexitic gneisses, amphibolites and minor tonalites, (2) an intermediate zone formed by screens of highly melted gneisses, amphibolites and metagabbros lying between tonalite and newly formed leucogranitoid and hybrid rock sheets, (3) an internal zone formed almost exclusively of massive tonalite and minor hybrid rocks. Incongruent melting of biotite in gneisses of the intermediate zone produced peritectic cordierite and garnet. Hybrids resulting from variable mixing of anatectic granitoids and tonalite magma developed in the innermost part of the aureole at 750-800ºC. Increased water activity within this zone eventually promoted increased melting of plagioclase + quartz in the gneisses. Leucogranitoid magmas formed in part by extraction from the hybrid magmas led to heterogeneity of the Sr-isotope composition. The Cerro Toro contact aureole shows that assimilation of metasedimentary rocks through partial melting can play an important role during emplacement of tonalitic magmas at mid-crustal levels. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-03 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/12099 Alasino, Pablo Horacio; Casquet, C.; Larrovere, Mariano Alexis; Pankhurst, R. J.; Galindo, C.; et al.; The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina; Elsevier Science; Lithos; 190-191; 3-2014; 154-172 0024-4937 |
url |
http://hdl.handle.net/11336/12099 |
identifier_str_mv |
Alasino, Pablo Horacio; Casquet, C.; Larrovere, Mariano Alexis; Pankhurst, R. J.; Galindo, C.; et al.; The evolution of a mid-crustal thermal aureole at Cerro Toro, Sierra de Famatina, NW Argentina; Elsevier Science; Lithos; 190-191; 3-2014; 154-172 0024-4937 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0024493713004088 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2013.12.006 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier Science |
publisher.none.fl_str_mv |
Elsevier Science |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
_version_ |
1844613626165460992 |
score |
13.070432 |