Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina

Autores
Baez, Walter Ariel; Carrasco Nuñez, Gerardo; Giordano, Guido; Viramonte, Jose German; Chiodi, Agostina Laura
Año de publicación
2017
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Despite a number of published papers focusing on the geodynamic implications of the recent Southern Puna mafic magmatism, there have been fewer studies of the volcanology and stratigraphy of this outstanding volcanism. This paper presents a detailed map of two well-preserved Quaternary scoria cones showing their complex stratigraphy. Complementary morphometric, morpho-structural, petrographic and geochemical data were used to reconstruct the evolution of both volcanoes. The occurrence of more than one eruption at each volcano was inferred by the recognition of temporal hiatuses using morpho-stratigraphic criteria. The polycyclic nature of both scoria cones could be related to a combination of a high input magma in response to lithospheric delamination, a favourable regional stress field and the interaction of rising magma with pre-existing faults. The youngest eruptions in both volcanoes were complex, with shifts in the eruptive style from violent strombolian to hawaiian/strombolian phases, and probably lasted for a few years. The explosive activity was accompanied by the emission of lava flows from lateral vents. Phreatomagmatic activity was triggered during the waning stages of the eruptions. The occurrence of more than one eruption in a single scoria cone and the changes in the eruptive style during long-lasting eruptions are important topics for volcanic hazard assessment in the Southern Puna.
Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
Fil: Carrasco Nuñez, Gerardo. Universidad Nacional Autónoma de México; México
Fil: Giordano, Guido. Università di Roma; Italia
Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
Fil: Chiodi, Agostina Laura. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
Materia
Mafic Volcanism
Volcanotectonic Interplay
Morpho-stratigraphy
Litho-stratigraphy
Complex volcanic evolution
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/66691
Acceder
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network_acronym_str CONICETDig
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network_name_str CONICET Digital (CONICET)
spelling Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, ArgentinaBaez, Walter ArielCarrasco Nuñez, GerardoGiordano, GuidoViramonte, Jose GermanChiodi, Agostina LauraMafic VolcanismVolcanotectonic InterplayMorpho-stratigraphyLitho-stratigraphyComplex volcanic evolutionhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Despite a number of published papers focusing on the geodynamic implications of the recent Southern Puna mafic magmatism, there have been fewer studies of the volcanology and stratigraphy of this outstanding volcanism. This paper presents a detailed map of two well-preserved Quaternary scoria cones showing their complex stratigraphy. Complementary morphometric, morpho-structural, petrographic and geochemical data were used to reconstruct the evolution of both volcanoes. The occurrence of more than one eruption at each volcano was inferred by the recognition of temporal hiatuses using morpho-stratigraphic criteria. The polycyclic nature of both scoria cones could be related to a combination of a high input magma in response to lithospheric delamination, a favourable regional stress field and the interaction of rising magma with pre-existing faults. The youngest eruptions in both volcanoes were complex, with shifts in the eruptive style from violent strombolian to hawaiian/strombolian phases, and probably lasted for a few years. The explosive activity was accompanied by the emission of lava flows from lateral vents. Phreatomagmatic activity was triggered during the waning stages of the eruptions. The occurrence of more than one eruption in a single scoria cone and the changes in the eruptive style during long-lasting eruptions are important topics for volcanic hazard assessment in the Southern Puna.Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; ArgentinaFil: Carrasco Nuñez, Gerardo. Universidad Nacional Autónoma de México; MéxicoFil: Giordano, Guido. Università di Roma; ItaliaFil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; ArgentinaFil: Chiodi, Agostina Laura. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; ArgentinaEdinburgh Scottish Academy2017-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/66691Baez, Walter Ariel; Carrasco Nuñez, Gerardo; Giordano, Guido; Viramonte, Jose German; Chiodi, Agostina Laura; Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina; Edinburgh Scottish Academy; Geological Society of London Special Publication; 446; 1; 6-2017; 311-3360305-8719CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1144/SP446.3info:eu-repo/semantics/altIdentifier/url/http://sp.lyellcollection.org/content/446/1/311info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T12:14:46Zoai:ri.conicet.gov.ar:11336/66691instacron: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:34982025-10-22 12:14:46.412CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
title Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
spellingShingle Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
Baez, Walter Ariel
Mafic Volcanism
Volcanotectonic Interplay
Morpho-stratigraphy
Litho-stratigraphy
Complex volcanic evolution
title_short Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
title_full Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
title_fullStr Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
title_full_unstemmed Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
title_sort Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina
dc.creator.none.fl_str_mv Baez, Walter Ariel
Carrasco Nuñez, Gerardo
Giordano, Guido
Viramonte, Jose German
Chiodi, Agostina Laura
author Baez, Walter Ariel
author_facet Baez, Walter Ariel
Carrasco Nuñez, Gerardo
Giordano, Guido
Viramonte, Jose German
Chiodi, Agostina Laura
author_role author
author2 Carrasco Nuñez, Gerardo
Giordano, Guido
Viramonte, Jose German
Chiodi, Agostina Laura
author2_role author
author
author
author
dc.subject.none.fl_str_mv Mafic Volcanism
Volcanotectonic Interplay
Morpho-stratigraphy
Litho-stratigraphy
Complex volcanic evolution
topic Mafic Volcanism
Volcanotectonic Interplay
Morpho-stratigraphy
Litho-stratigraphy
Complex volcanic evolution
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Despite a number of published papers focusing on the geodynamic implications of the recent Southern Puna mafic magmatism, there have been fewer studies of the volcanology and stratigraphy of this outstanding volcanism. This paper presents a detailed map of two well-preserved Quaternary scoria cones showing their complex stratigraphy. Complementary morphometric, morpho-structural, petrographic and geochemical data were used to reconstruct the evolution of both volcanoes. The occurrence of more than one eruption at each volcano was inferred by the recognition of temporal hiatuses using morpho-stratigraphic criteria. The polycyclic nature of both scoria cones could be related to a combination of a high input magma in response to lithospheric delamination, a favourable regional stress field and the interaction of rising magma with pre-existing faults. The youngest eruptions in both volcanoes were complex, with shifts in the eruptive style from violent strombolian to hawaiian/strombolian phases, and probably lasted for a few years. The explosive activity was accompanied by the emission of lava flows from lateral vents. Phreatomagmatic activity was triggered during the waning stages of the eruptions. The occurrence of more than one eruption in a single scoria cone and the changes in the eruptive style during long-lasting eruptions are important topics for volcanic hazard assessment in the Southern Puna.
Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
Fil: Carrasco Nuñez, Gerardo. Universidad Nacional Autónoma de México; México
Fil: Giordano, Guido. Università di Roma; Italia
Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
Fil: Chiodi, Agostina Laura. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
description Despite a number of published papers focusing on the geodynamic implications of the recent Southern Puna mafic magmatism, there have been fewer studies of the volcanology and stratigraphy of this outstanding volcanism. This paper presents a detailed map of two well-preserved Quaternary scoria cones showing their complex stratigraphy. Complementary morphometric, morpho-structural, petrographic and geochemical data were used to reconstruct the evolution of both volcanoes. The occurrence of more than one eruption at each volcano was inferred by the recognition of temporal hiatuses using morpho-stratigraphic criteria. The polycyclic nature of both scoria cones could be related to a combination of a high input magma in response to lithospheric delamination, a favourable regional stress field and the interaction of rising magma with pre-existing faults. The youngest eruptions in both volcanoes were complex, with shifts in the eruptive style from violent strombolian to hawaiian/strombolian phases, and probably lasted for a few years. The explosive activity was accompanied by the emission of lava flows from lateral vents. Phreatomagmatic activity was triggered during the waning stages of the eruptions. The occurrence of more than one eruption in a single scoria cone and the changes in the eruptive style during long-lasting eruptions are important topics for volcanic hazard assessment in the Southern Puna.
publishDate 2017
dc.date.none.fl_str_mv 2017-06
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/11336/66691
Baez, Walter Ariel; Carrasco Nuñez, Gerardo; Giordano, Guido; Viramonte, Jose German; Chiodi, Agostina Laura; Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina; Edinburgh Scottish Academy; Geological Society of London Special Publication; 446; 1; 6-2017; 311-336
0305-8719
CONICET Digital
CONICET
url http://hdl.handle.net/11336/66691
identifier_str_mv Baez, Walter Ariel; Carrasco Nuñez, Gerardo; Giordano, Guido; Viramonte, Jose German; Chiodi, Agostina Laura; Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina; Edinburgh Scottish Academy; Geological Society of London Special Publication; 446; 1; 6-2017; 311-336
0305-8719
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1144/SP446.3
info:eu-repo/semantics/altIdentifier/url/http://sp.lyellcollection.org/content/446/1/311
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Edinburgh Scottish Academy
publisher.none.fl_str_mv Edinburgh Scottish Academy
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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