Magmatic gas percolation through the old lava dome of El Misti volcano

Descripción del Articulo

The proximity of the major city of Arequipa to El Misti has focused attention on the hazards posed by the active volcano. Since its last major eruption in the fifteenth century, El Misti has experienced a series of modest phreatic eruptions and fluctuating fumarolic activity. Here, we present the fi...

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Detalles Bibliográficos
Autores: Moussallam, Yves, Peters, Nial, Masías Alvarez, Pablo Jorge, Apaza Choquehuayta, Fredy Erlingtton, Barnie, Talfan, Schipper, C. Ian, Curtis, Aaron, Tamburello, Giancarlo, Aiuppa, Alessandro, Bani, Philipson, Giudice, Gaetano, Pieri, David, Davies, Ashley Gerard, Oppenheimer, Clive
Formato: artículo
Fecha de Publicación:2017
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/1171
Enlace del recurso:https://hdl.handle.net/20.500.12544/1171
https://doi.org/10.1007/s00445-017-1129-5
Nivel de acceso:acceso abierto
Materia:Gases volcánicos
Desgasificación
Imágenes ASTER
Volcanes
Volcán Misti
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dc.title.es_PE.fl_str_mv Magmatic gas percolation through the old lava dome of El Misti volcano
title Magmatic gas percolation through the old lava dome of El Misti volcano
spellingShingle Magmatic gas percolation through the old lava dome of El Misti volcano
Moussallam, Yves
Gases volcánicos
Desgasificación
Imágenes ASTER
Volcanes
Volcán Misti
title_short Magmatic gas percolation through the old lava dome of El Misti volcano
title_full Magmatic gas percolation through the old lava dome of El Misti volcano
title_fullStr Magmatic gas percolation through the old lava dome of El Misti volcano
title_full_unstemmed Magmatic gas percolation through the old lava dome of El Misti volcano
title_sort Magmatic gas percolation through the old lava dome of El Misti volcano
author Moussallam, Yves
author_facet Moussallam, Yves
Peters, Nial
Masías Alvarez, Pablo Jorge
Apaza Choquehuayta, Fredy Erlingtton
Barnie, Talfan
Schipper, C. Ian
Curtis, Aaron
Tamburello, Giancarlo
Aiuppa, Alessandro
Bani, Philipson
Giudice, Gaetano
Pieri, David
Davies, Ashley Gerard
Oppenheimer, Clive
author_role author
author2 Peters, Nial
Masías Alvarez, Pablo Jorge
Apaza Choquehuayta, Fredy Erlingtton
Barnie, Talfan
Schipper, C. Ian
Curtis, Aaron
Tamburello, Giancarlo
Aiuppa, Alessandro
Bani, Philipson
Giudice, Gaetano
Pieri, David
Davies, Ashley Gerard
Oppenheimer, Clive
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Moussallam, Yves
Peters, Nial
Masías Alvarez, Pablo Jorge
Apaza Choquehuayta, Fredy Erlingtton
Barnie, Talfan
Schipper, C. Ian
Curtis, Aaron
Tamburello, Giancarlo
Aiuppa, Alessandro
Bani, Philipson
Giudice, Gaetano
Pieri, David
Davies, Ashley Gerard
Oppenheimer, Clive
dc.subject.es_PE.fl_str_mv Gases volcánicos
Desgasificación
Imágenes ASTER
Volcanes
Volcán Misti
topic Gases volcánicos
Desgasificación
Imágenes ASTER
Volcanes
Volcán Misti
description The proximity of the major city of Arequipa to El Misti has focused attention on the hazards posed by the active volcano. Since its last major eruption in the fifteenth century, El Misti has experienced a series of modest phreatic eruptions and fluctuating fumarolic activity. Here, we present the first measurements of the compositions of gas emitted from the lava dome in the summit crater. The gas composition is found to be fairly dry with a H2O/SO2 molar ratio of 32 ± 3, a CO2/SO2 molar ratio of 2.7 ± 0.2, a H2S/SO2 molar ratio of 0.23 ± 0.02 and a H2/SO2 molar ratio of 0.012 ± 0.002. This magmatic gas signature with minimal evidence of hydrothermal or wall rock interaction points to a shallow magma source that is efficiently outgassing through a permeable conduit and lava dome. Field and satellite observations show no evolution of the lava dome over the last decade, indicating sustained outgassing through an established fracture network. This stability could be disrupted if dome permeability were to be reduced by annealing or occlusion of outgassing pathways. Continued monitoring of gas composition and flux at El Misti will be essential to determine the evolution of hazard potential at this dangerous volcano.
publishDate 2017
dc.date.accessioned.none.fl_str_mv 2018-03-22T20:33:23Z
dc.date.available.none.fl_str_mv 2018-03-22T20:33:23Z
dc.date.issued.fl_str_mv 2017-05
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.es_PE.fl_str_mv Moussallam, Y.; Peters, N.; Masías, P.; Apaza, F.; Barnie, Talfan, et al. (2017) - Magmatic gas percolation through the old lava dome of El Misti volcano. Bulletin of Volcanology, 79 (6): 46. Doi: 10.1007/s00445-017-1129-5
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/1171
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1007/s00445-017-1129-5
dc.identifier.journal.es_PE.fl_str_mv Bulletin of Volcanology
dc.identifier.bibliographicCitation.es_PE.fl_str_mv Bulletin of Volcanology, v. 79, n. 6, 2017
identifier_str_mv Moussallam, Y.; Peters, N.; Masías, P.; Apaza, F.; Barnie, Talfan, et al. (2017) - Magmatic gas percolation through the old lava dome of El Misti volcano. Bulletin of Volcanology, 79 (6): 46. Doi: 10.1007/s00445-017-1129-5
Bulletin of Volcanology
Bulletin of Volcanology, v. 79, n. 6, 2017
url https://hdl.handle.net/20.500.12544/1171
https://doi.org/10.1007/s00445-017-1129-5
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:1432-0819
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
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dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Arequipa
Perú
dc.publisher.es_PE.fl_str_mv Springer Berlin Heidelberg
dc.publisher.country.es_PE.fl_str_mv DE
dc.source.es_PE.fl_str_mv Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
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spelling Moussallam, YvesPeters, NialMasías Alvarez, Pablo JorgeApaza Choquehuayta, Fredy ErlingttonBarnie, TalfanSchipper, C. IanCurtis, AaronTamburello, GiancarloAiuppa, AlessandroBani, PhilipsonGiudice, GaetanoPieri, DavidDavies, Ashley GerardOppenheimer, CliveArequipaPerú2018-03-22T20:33:23Z2018-03-22T20:33:23Z2017-05Moussallam, Y.; Peters, N.; Masías, P.; Apaza, F.; Barnie, Talfan, et al. (2017) - Magmatic gas percolation through the old lava dome of El Misti volcano. Bulletin of Volcanology, 79 (6): 46. Doi: 10.1007/s00445-017-1129-5https://hdl.handle.net/20.500.12544/1171https://doi.org/10.1007/s00445-017-1129-5Bulletin of VolcanologyBulletin of Volcanology, v. 79, n. 6, 2017The proximity of the major city of Arequipa to El Misti has focused attention on the hazards posed by the active volcano. Since its last major eruption in the fifteenth century, El Misti has experienced a series of modest phreatic eruptions and fluctuating fumarolic activity. Here, we present the first measurements of the compositions of gas emitted from the lava dome in the summit crater. The gas composition is found to be fairly dry with a H2O/SO2 molar ratio of 32 ± 3, a CO2/SO2 molar ratio of 2.7 ± 0.2, a H2S/SO2 molar ratio of 0.23 ± 0.02 and a H2/SO2 molar ratio of 0.012 ± 0.002. This magmatic gas signature with minimal evidence of hydrothermal or wall rock interaction points to a shallow magma source that is efficiently outgassing through a permeable conduit and lava dome. Field and satellite observations show no evolution of the lava dome over the last decade, indicating sustained outgassing through an established fracture network. This stability could be disrupted if dome permeability were to be reduced by annealing or occlusion of outgassing pathways. 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