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
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/120687
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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 Técnicas2025-09-03T10:11:55Zoai: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:34982025-09-03 10:11:56.044CONICET 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 |
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CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
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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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1842270177265188864 |
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13.13397 |