Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético

Autores
Nieves, Alexis Iván Angel; Suzaño, Nestor Omar; Becchio, Raul Alberto; Ortiz Yañez, Agustín
Año de publicación
2019
Idioma
español castellano
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The granites of the Lower Paleozoic from the sierra de Inca Viejo, Puna Austral. Textural aspects of the mixture of magmas and petrogenetic model The Diablillos intrusive Complex which outcrops in the Inca Viejo Range, Eastern Puna Austral, record magma mixing process, during the Famatinian Arc evolution. This complex is formed by diorites, quartz-diorites, tonalites, granodiorites and granites (syeno and monzogranites) intruding low- to medium grade metamorphic rocks. The tonalites and granodiorites facies are hybrids that resulted from mixing between diorites and granites. In some cases, mechanic hybridization (mingling) was distinguished. Field relationships and petrography show successive dioritic magma pulses into a magmatic chamber of granitic composition, developing products with different degrees of crystallization and hybridization.In the context of a magmatic chamber, the different magmatic textures reflect a complex evolution from the generation of magmas until their emplacement and final consolidation. In this scenario, both slow cooling magmatic textures (such as, ocelli quartz, mantled plagioclase, corroded K-feldspars) as well as rapid cooling textures (e.g. acicular apatite) developed at lower crustal levels and intermediate-upper crustal levels respectively were identified. Magma mixing is probably the dominant magmatic differentiation process in the Inca Viejo range. The integrated results, allowed us to draw a conceptual mixing model, showing the interaction between mafic and felsic magmas at different rheological stages.Therefore the compositional variations observed in the Diablillos Intrusive Complex could be explained by mixing different proportions of felsic and mafic magmas.
Fil: Nieves, Alexis Iván Angel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Fil: Suzaño, Nestor Omar. Universidad Nacional de Jujuy. Facultad de Ingeniería; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta; Argentina
Fil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Fil: Ortiz Yañez, Agustín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Materia
Magmatism
Granitoids
Hibridization
Textural desequilibrium
Nivel de accesibilidad
acceso abierto
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https://creativecommons.org/licenses/by-nc/2.5/ar/
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CONICET Digital (CONICET)
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Consejo Nacional de Investigaciones Científicas y Técnicas
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oai:ri.conicet.gov.ar:11336/120687
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenéticoNieves, Alexis Iván AngelSuzaño, Nestor OmarBecchio, Raul AlbertoOrtiz Yañez, AgustínMagmatismGranitoidsHibridizationTextural desequilibriumhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The granites of the Lower Paleozoic from the sierra de Inca Viejo, Puna Austral. Textural aspects of the mixture of magmas and petrogenetic model The Diablillos intrusive Complex which outcrops in the Inca Viejo Range, Eastern Puna Austral, record magma mixing process, during the Famatinian Arc evolution. This complex is formed by diorites, quartz-diorites, tonalites, granodiorites and granites (syeno and monzogranites) intruding low- to medium grade metamorphic rocks. The tonalites and granodiorites facies are hybrids that resulted from mixing between diorites and granites. In some cases, mechanic hybridization (mingling) was distinguished. Field relationships and petrography show successive dioritic magma pulses into a magmatic chamber of granitic composition, developing products with different degrees of crystallization and hybridization.In the context of a magmatic chamber, the different magmatic textures reflect a complex evolution from the generation of magmas until their emplacement and final consolidation. In this scenario, both slow cooling magmatic textures (such as, ocelli quartz, mantled plagioclase, corroded K-feldspars) as well as rapid cooling textures (e.g. acicular apatite) developed at lower crustal levels and intermediate-upper crustal levels respectively were identified. Magma mixing is probably the dominant magmatic differentiation process in the Inca Viejo range. The integrated results, allowed us to draw a conceptual mixing model, showing the interaction between mafic and felsic magmas at different rheological stages.Therefore the compositional variations observed in the Diablillos Intrusive Complex could be explained by mixing different proportions of felsic and mafic magmas.Fil: Nieves, Alexis Iván Angel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; ArgentinaFil: Suzaño, Nestor Omar. Universidad Nacional de Jujuy. Facultad de Ingeniería; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta; ArgentinaFil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; ArgentinaFil: Ortiz Yañez, Agustín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; ArgentinaAsociación Geológica Argentina2019-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/120687Nieves, Alexis Iván Angel; Suzaño, Nestor Omar; Becchio, Raul Alberto; Ortiz Yañez, Agustín; Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético; Asociación Geológica Argentina; Revista de la Asociación Geológica Argentina; 76; 3; 12-2019; 279-2951851-82491669-7316CONICET DigitalCONICETspainfo:eu-repo/semantics/altIdentifier/url/http://ppct.caicyt.gov.ar/index.php/raga/article/view/12486info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:47:15Zoai:ri.conicet.gov.ar:11336/120687instacron: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 10:47:15.643CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
title Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
spellingShingle Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
Nieves, Alexis Iván Angel
Magmatism
Granitoids
Hibridization
Textural desequilibrium
title_short Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
title_full Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
title_fullStr Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
title_full_unstemmed Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
title_sort Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético
dc.creator.none.fl_str_mv Nieves, Alexis Iván Angel
Suzaño, Nestor Omar
Becchio, Raul Alberto
Ortiz Yañez, Agustín
author Nieves, Alexis Iván Angel
author_facet Nieves, Alexis Iván Angel
Suzaño, Nestor Omar
Becchio, Raul Alberto
Ortiz Yañez, Agustín
author_role author
author2 Suzaño, Nestor Omar
Becchio, Raul Alberto
Ortiz Yañez, Agustín
author2_role author
author
author
dc.subject.none.fl_str_mv Magmatism
Granitoids
Hibridization
Textural desequilibrium
topic Magmatism
Granitoids
Hibridization
Textural desequilibrium
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The granites of the Lower Paleozoic from the sierra de Inca Viejo, Puna Austral. Textural aspects of the mixture of magmas and petrogenetic model The Diablillos intrusive Complex which outcrops in the Inca Viejo Range, Eastern Puna Austral, record magma mixing process, during the Famatinian Arc evolution. This complex is formed by diorites, quartz-diorites, tonalites, granodiorites and granites (syeno and monzogranites) intruding low- to medium grade metamorphic rocks. The tonalites and granodiorites facies are hybrids that resulted from mixing between diorites and granites. In some cases, mechanic hybridization (mingling) was distinguished. Field relationships and petrography show successive dioritic magma pulses into a magmatic chamber of granitic composition, developing products with different degrees of crystallization and hybridization.In the context of a magmatic chamber, the different magmatic textures reflect a complex evolution from the generation of magmas until their emplacement and final consolidation. In this scenario, both slow cooling magmatic textures (such as, ocelli quartz, mantled plagioclase, corroded K-feldspars) as well as rapid cooling textures (e.g. acicular apatite) developed at lower crustal levels and intermediate-upper crustal levels respectively were identified. Magma mixing is probably the dominant magmatic differentiation process in the Inca Viejo range. The integrated results, allowed us to draw a conceptual mixing model, showing the interaction between mafic and felsic magmas at different rheological stages.Therefore the compositional variations observed in the Diablillos Intrusive Complex could be explained by mixing different proportions of felsic and mafic magmas.
Fil: Nieves, Alexis Iván Angel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Fil: Suzaño, Nestor Omar. Universidad Nacional de Jujuy. Facultad de Ingeniería; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta; Argentina
Fil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Fil: Ortiz Yañez, Agustín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
description The granites of the Lower Paleozoic from the sierra de Inca Viejo, Puna Austral. Textural aspects of the mixture of magmas and petrogenetic model The Diablillos intrusive Complex which outcrops in the Inca Viejo Range, Eastern Puna Austral, record magma mixing process, during the Famatinian Arc evolution. This complex is formed by diorites, quartz-diorites, tonalites, granodiorites and granites (syeno and monzogranites) intruding low- to medium grade metamorphic rocks. The tonalites and granodiorites facies are hybrids that resulted from mixing between diorites and granites. In some cases, mechanic hybridization (mingling) was distinguished. Field relationships and petrography show successive dioritic magma pulses into a magmatic chamber of granitic composition, developing products with different degrees of crystallization and hybridization.In the context of a magmatic chamber, the different magmatic textures reflect a complex evolution from the generation of magmas until their emplacement and final consolidation. In this scenario, both slow cooling magmatic textures (such as, ocelli quartz, mantled plagioclase, corroded K-feldspars) as well as rapid cooling textures (e.g. acicular apatite) developed at lower crustal levels and intermediate-upper crustal levels respectively were identified. Magma mixing is probably the dominant magmatic differentiation process in the Inca Viejo range. The integrated results, allowed us to draw a conceptual mixing model, showing the interaction between mafic and felsic magmas at different rheological stages.Therefore the compositional variations observed in the Diablillos Intrusive Complex could be explained by mixing different proportions of felsic and mafic magmas.
publishDate 2019
dc.date.none.fl_str_mv 2019-12
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/11336/120687
Nieves, Alexis Iván Angel; Suzaño, Nestor Omar; Becchio, Raul Alberto; Ortiz Yañez, Agustín; Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético; Asociación Geológica Argentina; Revista de la Asociación Geológica Argentina; 76; 3; 12-2019; 279-295
1851-8249
1669-7316
CONICET Digital
CONICET
url http://hdl.handle.net/11336/120687
identifier_str_mv Nieves, Alexis Iván Angel; Suzaño, Nestor Omar; Becchio, Raul Alberto; Ortiz Yañez, Agustín; Los granitos del Paleozoico inferior de la sierra de Inca Viejo, Puna Austral: aspectos texturales de la mezcla de magmas y modelo petrogenético; Asociación Geológica Argentina; Revista de la Asociación Geológica Argentina; 76; 3; 12-2019; 279-295
1851-8249
1669-7316
CONICET Digital
CONICET
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://ppct.caicyt.gov.ar/index.php/raga/article/view/12486
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Asociación Geológica Argentina
publisher.none.fl_str_mv Asociación Geológica Argentina
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
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score 13.070432

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