Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina

Autores
Cisterna, Clara Eugenia; Coira, Beatriz Lidia Luisa
Año de publicación
2022
Idioma
español castellano
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The study of volcanic deposits along active margins provides an excellent tool to understand geodynamic processes linked to tectonic evolution. Such processes can be understood from compositional, lithofacial and textural studies of the volcanic deposits (Allen et al. 2007). The Suri- Las Planchadas Volcanic- Sedimentary Complex (SPVSC), that build up the Las Planchadas and Narváez hills (northwestern portion of the Sierras Pampeanas, Argentina) forming part of the proto-Andean margin, represents a well exposed example of the Famatinian arc with a complete record of the volcanic activity during the Early to Middle Ordovician. Lithofacies analysis based on features as composition, textures and structures of these ancient successions give insights on the emplacement mechanisms and eruption styles of volcanism during the evolution of the Famatinian arc. Likewise, this work attempts to contribute elements of analysis for the understanding of other ancient volcanic successions. Previous descriptions and interpretations of the SPVSC published by the authors, have focused on stratigraphic aspects and local petrographic and geochemical studies as tools to explain specifi c source processes (Cisterna and Coira 2014, 2017 and Cisterna et al. 2017, among others). This work analyses the characteristics and distribution of volcanic facies, focusing on styles of volcanic activity and sedimentation. Detailed facies analysis is based on mapping and profi les across the Las Planchadas and Narváez hills, and takes into account new data, previous works and the regional structures aff ecting the area.
Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Coira, Beatriz Lidia Luisa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones y Transferencia de Jujuy. Universidad Nacional de Jujuy. Centro de Investigaciones y Transferencia de Jujuy; Argentina
XXI Congreso Geológico Argentino
Puerto Madryn
Argentina
Asociación Geológica Argentina
Materia
ORÓGENO FAMATINIANO
VOLCANISMO
SISTEMA DE FAMATINA
ARCO DE ISLAS
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:11336/266830
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, ArgentinaCisterna, Clara EugeniaCoira, Beatriz Lidia LuisaORÓGENO FAMATINIANOVOLCANISMOSISTEMA DE FAMATINAARCO DE ISLAShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The study of volcanic deposits along active margins provides an excellent tool to understand geodynamic processes linked to tectonic evolution. Such processes can be understood from compositional, lithofacial and textural studies of the volcanic deposits (Allen et al. 2007). The Suri- Las Planchadas Volcanic- Sedimentary Complex (SPVSC), that build up the Las Planchadas and Narváez hills (northwestern portion of the Sierras Pampeanas, Argentina) forming part of the proto-Andean margin, represents a well exposed example of the Famatinian arc with a complete record of the volcanic activity during the Early to Middle Ordovician. Lithofacies analysis based on features as composition, textures and structures of these ancient successions give insights on the emplacement mechanisms and eruption styles of volcanism during the evolution of the Famatinian arc. Likewise, this work attempts to contribute elements of analysis for the understanding of other ancient volcanic successions. Previous descriptions and interpretations of the SPVSC published by the authors, have focused on stratigraphic aspects and local petrographic and geochemical studies as tools to explain specifi c source processes (Cisterna and Coira 2014, 2017 and Cisterna et al. 2017, among others). This work analyses the characteristics and distribution of volcanic facies, focusing on styles of volcanic activity and sedimentation. Detailed facies analysis is based on mapping and profi les across the Las Planchadas and Narváez hills, and takes into account new data, previous works and the regional structures aff ecting the area.Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaFil: Coira, Beatriz Lidia Luisa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones y Transferencia de Jujuy. Universidad Nacional de Jujuy. Centro de Investigaciones y Transferencia de Jujuy; ArgentinaXXI Congreso Geológico ArgentinoPuerto MadrynArgentinaAsociación Geológica ArgentinaAsociación Geológica Argentina2022info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/vnd.openxmlformats-officedocument.wordprocessingml.documentapplication/pdfhttp://hdl.handle.net/11336/266830Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina; XXI Congreso Geológico Argentino; Puerto Madryn; Argentina; 2022; 387-388978-987-48319-9-6CONICET DigitalCONICETspainfo:eu-repo/semantics/altIdentifier/url/https://geologica.org.ar/xxi-cga-2022-chubut/Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:46:01Zoai:ri.conicet.gov.ar:11336/266830instacron: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:34982025-10-15 15:46:01.461CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
title Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
spellingShingle Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
Cisterna, Clara Eugenia
ORÓGENO FAMATINIANO
VOLCANISMO
SISTEMA DE FAMATINA
ARCO DE ISLAS
title_short Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
title_full Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
title_fullStr Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
title_full_unstemmed Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
title_sort Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina
dc.creator.none.fl_str_mv Cisterna, Clara Eugenia
Coira, Beatriz Lidia Luisa
author Cisterna, Clara Eugenia
author_facet Cisterna, Clara Eugenia
Coira, Beatriz Lidia Luisa
author_role author
author2 Coira, Beatriz Lidia Luisa
author2_role author
dc.subject.none.fl_str_mv ORÓGENO FAMATINIANO
VOLCANISMO
SISTEMA DE FAMATINA
ARCO DE ISLAS
topic ORÓGENO FAMATINIANO
VOLCANISMO
SISTEMA DE FAMATINA
ARCO DE ISLAS
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 study of volcanic deposits along active margins provides an excellent tool to understand geodynamic processes linked to tectonic evolution. Such processes can be understood from compositional, lithofacial and textural studies of the volcanic deposits (Allen et al. 2007). The Suri- Las Planchadas Volcanic- Sedimentary Complex (SPVSC), that build up the Las Planchadas and Narváez hills (northwestern portion of the Sierras Pampeanas, Argentina) forming part of the proto-Andean margin, represents a well exposed example of the Famatinian arc with a complete record of the volcanic activity during the Early to Middle Ordovician. Lithofacies analysis based on features as composition, textures and structures of these ancient successions give insights on the emplacement mechanisms and eruption styles of volcanism during the evolution of the Famatinian arc. Likewise, this work attempts to contribute elements of analysis for the understanding of other ancient volcanic successions. Previous descriptions and interpretations of the SPVSC published by the authors, have focused on stratigraphic aspects and local petrographic and geochemical studies as tools to explain specifi c source processes (Cisterna and Coira 2014, 2017 and Cisterna et al. 2017, among others). This work analyses the characteristics and distribution of volcanic facies, focusing on styles of volcanic activity and sedimentation. Detailed facies analysis is based on mapping and profi les across the Las Planchadas and Narváez hills, and takes into account new data, previous works and the regional structures aff ecting the area.
Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Coira, Beatriz Lidia Luisa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones y Transferencia de Jujuy. Universidad Nacional de Jujuy. Centro de Investigaciones y Transferencia de Jujuy; Argentina
XXI Congreso Geológico Argentino
Puerto Madryn
Argentina
Asociación Geológica Argentina
description The study of volcanic deposits along active margins provides an excellent tool to understand geodynamic processes linked to tectonic evolution. Such processes can be understood from compositional, lithofacial and textural studies of the volcanic deposits (Allen et al. 2007). The Suri- Las Planchadas Volcanic- Sedimentary Complex (SPVSC), that build up the Las Planchadas and Narváez hills (northwestern portion of the Sierras Pampeanas, Argentina) forming part of the proto-Andean margin, represents a well exposed example of the Famatinian arc with a complete record of the volcanic activity during the Early to Middle Ordovician. Lithofacies analysis based on features as composition, textures and structures of these ancient successions give insights on the emplacement mechanisms and eruption styles of volcanism during the evolution of the Famatinian arc. Likewise, this work attempts to contribute elements of analysis for the understanding of other ancient volcanic successions. Previous descriptions and interpretations of the SPVSC published by the authors, have focused on stratigraphic aspects and local petrographic and geochemical studies as tools to explain specifi c source processes (Cisterna and Coira 2014, 2017 and Cisterna et al. 2017, among others). This work analyses the characteristics and distribution of volcanic facies, focusing on styles of volcanic activity and sedimentation. Detailed facies analysis is based on mapping and profi les across the Las Planchadas and Narváez hills, and takes into account new data, previous works and the regional structures aff ecting the area.
publishDate 2022
dc.date.none.fl_str_mv 2022
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
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info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
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dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/266830
Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina; XXI Congreso Geológico Argentino; Puerto Madryn; Argentina; 2022; 387-388
978-987-48319-9-6
CONICET Digital
CONICET
url http://hdl.handle.net/11336/266830
identifier_str_mv Ordovician submarine to subaerial volcanism along the western Gondwana margin: records of the Famatinian belt evolution, sierras pampeanas, Argentina; XXI Congreso Geológico Argentino; Puerto Madryn; Argentina; 2022; 387-388
978-987-48319-9-6
CONICET Digital
CONICET
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://geologica.org.ar/xxi-cga-2022-chubut/
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dc.coverage.none.fl_str_mv Internacional
dc.publisher.none.fl_str_mv Asociación Geológica Argentina
publisher.none.fl_str_mv Asociación Geológica Argentina
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