Anomalous back-arc volcanism due to subducting linear topographic features

Autores
Ichihara, Mie; Adam, Claudia; Grosse, Pablo; Vidal, Valerie
Año de publicación
2019
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Back-arc volcanism along the Pacific Ring of Fire exhibits different types of volcanoes. Among them, anomalous volcanoes can be spotted either as uncommonly large volcanoes, or as isolated volcanoes in an region with few or no volcanism. These anomalous arc volcanoes are often correlated with the existence of a linear topographic feature (fracture zone, seamounts alignment, ridge) on the subducting seafloor. Based on an accurate volcano volume estimation, as well as a quantification of topographic anomalies on the oceanic side, we challenge this correlation and assess the relevance of a quantitative link between subducting topographic anomalies and uncommon back-arc volcanism.
Fil: Ichihara, Mie. University of Tokyo; Japón
Fil: Adam, Claudia. Kansas State University; Estados Unidos
Fil: Grosse, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Fundación Miguel Lillo. Dirección de Geología. Instituto de Minerología y Petrografia; Argentina
Fil: Vidal, Valerie. Centre National de la Recherche Scientifique; Francia
Joint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section Meeting
Manhattan
Estados Unidos
Geological Society of America
Materia
VOLCANISM
TOPOGRAPHIC FEATURES
VOLCAN
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:11336/280958
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Anomalous back-arc volcanism due to subducting linear topographic featuresIchihara, MieAdam, ClaudiaGrosse, PabloVidal, ValerieVOLCANISMTOPOGRAPHIC FEATURESVOLCANhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Back-arc volcanism along the Pacific Ring of Fire exhibits different types of volcanoes. Among them, anomalous volcanoes can be spotted either as uncommonly large volcanoes, or as isolated volcanoes in an region with few or no volcanism. These anomalous arc volcanoes are often correlated with the existence of a linear topographic feature (fracture zone, seamounts alignment, ridge) on the subducting seafloor. Based on an accurate volcano volume estimation, as well as a quantification of topographic anomalies on the oceanic side, we challenge this correlation and assess the relevance of a quantitative link between subducting topographic anomalies and uncommon back-arc volcanism.Fil: Ichihara, Mie. University of Tokyo; JapónFil: Adam, Claudia. Kansas State University; Estados UnidosFil: Grosse, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Fundación Miguel Lillo. Dirección de Geología. Instituto de Minerología y Petrografia; ArgentinaFil: Vidal, Valerie. Centre National de la Recherche Scientifique; FranciaJoint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section MeetingManhattanEstados UnidosGeological Society of AmericaGeological Society of America2019info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectReuniónJournalhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/280958Anomalous back-arc volcanism due to subducting linear topographic features; Joint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section Meeting; Manhattan; Estados Unidos; 2019; 1-10016-7592CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://gsa.confex.com/gsa/2019SC/webprogram/Paper326933.htmlinfo:eu-repo/semantics/altIdentifier/doi/10.1130/abs/2019SC-326933Nacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-06T12:22:29Zoai:ri.conicet.gov.ar:11336/280958instacron: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:34982026-02-06 12:22:29.859CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Anomalous back-arc volcanism due to subducting linear topographic features
title Anomalous back-arc volcanism due to subducting linear topographic features
spellingShingle Anomalous back-arc volcanism due to subducting linear topographic features
Ichihara, Mie
VOLCANISM
TOPOGRAPHIC FEATURES
VOLCAN
title_short Anomalous back-arc volcanism due to subducting linear topographic features
title_full Anomalous back-arc volcanism due to subducting linear topographic features
title_fullStr Anomalous back-arc volcanism due to subducting linear topographic features
title_full_unstemmed Anomalous back-arc volcanism due to subducting linear topographic features
title_sort Anomalous back-arc volcanism due to subducting linear topographic features
dc.creator.none.fl_str_mv Ichihara, Mie
Adam, Claudia
Grosse, Pablo
Vidal, Valerie
author Ichihara, Mie
author_facet Ichihara, Mie
Adam, Claudia
Grosse, Pablo
Vidal, Valerie
author_role author
author2 Adam, Claudia
Grosse, Pablo
Vidal, Valerie
author2_role author
author
author
dc.subject.none.fl_str_mv VOLCANISM
TOPOGRAPHIC FEATURES
VOLCAN
topic VOLCANISM
TOPOGRAPHIC FEATURES
VOLCAN
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Back-arc volcanism along the Pacific Ring of Fire exhibits different types of volcanoes. Among them, anomalous volcanoes can be spotted either as uncommonly large volcanoes, or as isolated volcanoes in an region with few or no volcanism. These anomalous arc volcanoes are often correlated with the existence of a linear topographic feature (fracture zone, seamounts alignment, ridge) on the subducting seafloor. Based on an accurate volcano volume estimation, as well as a quantification of topographic anomalies on the oceanic side, we challenge this correlation and assess the relevance of a quantitative link between subducting topographic anomalies and uncommon back-arc volcanism.
Fil: Ichihara, Mie. University of Tokyo; Japón
Fil: Adam, Claudia. Kansas State University; Estados Unidos
Fil: Grosse, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Fundación Miguel Lillo. Dirección de Geología. Instituto de Minerología y Petrografia; Argentina
Fil: Vidal, Valerie. Centre National de la Recherche Scientifique; Francia
Joint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section Meeting
Manhattan
Estados Unidos
Geological Society of America
description Back-arc volcanism along the Pacific Ring of Fire exhibits different types of volcanoes. Among them, anomalous volcanoes can be spotted either as uncommonly large volcanoes, or as isolated volcanoes in an region with few or no volcanism. These anomalous arc volcanoes are often correlated with the existence of a linear topographic feature (fracture zone, seamounts alignment, ridge) on the subducting seafloor. Based on an accurate volcano volume estimation, as well as a quantification of topographic anomalies on the oceanic side, we challenge this correlation and assess the relevance of a quantitative link between subducting topographic anomalies and uncommon back-arc volcanism.
publishDate 2019
dc.date.none.fl_str_mv 2019
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Reunión
Journal
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/280958
Anomalous back-arc volcanism due to subducting linear topographic features; Joint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section Meeting; Manhattan; Estados Unidos; 2019; 1-1
0016-7592
CONICET Digital
CONICET
url http://hdl.handle.net/11336/280958
identifier_str_mv Anomalous back-arc volcanism due to subducting linear topographic features; Joint 53rd South-Central, 53rd North-Central y 71st Rocky Mountain Section Meeting; Manhattan; Estados Unidos; 2019; 1-1
0016-7592
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://gsa.confex.com/gsa/2019SC/webprogram/Paper326933.html
info:eu-repo/semantics/altIdentifier/doi/10.1130/abs/2019SC-326933
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.coverage.none.fl_str_mv Nacional
dc.publisher.none.fl_str_mv Geological Society of America
publisher.none.fl_str_mv Geological Society of America
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 13.11174

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