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Authordc.contributor.authorRobidoux, Philippe
Authordc.contributor.authorPastén, Daniela
Authordc.contributor.authorLevresse, Gilles
Authordc.contributor.authorDíaz, Gloria
Authordc.contributor.authorParedes, Dante
Admission datedc.date.accessioned2022-12-21T20:15:06Z
Available datedc.date.available2022-12-21T20:15:06Z
Publication datedc.date.issued2021
Cita de ítemdc.identifier.citationGeosciences 2021, 11, 309es_ES
Identifierdc.identifier.other10.3390/geosciences11080309
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/189939
Abstractdc.description.abstractPotential flank eruptions at the presently active Villarrica, Southern Andes Volcanic Zone (33.3–46 S) require the drawing of a comprehensive scenario of eruptive style dynamics, which partially depends on the degassing process. The case we consider in this study is from the Los Nevados Subgroup 2 (LNG2) and constitutes post-glacial minor eruptive centers (MECs) of basaltic– andesitic and basaltic composition, associated with the northeastern Villarrica flank. Petrological studies of the melt inclusions volatile content in olivine determined the pre-eruptive conditions of the shallow magma feeding system (<249 Mpa saturation pressure, 927–1201 C). The volatile saturation model on “pressure-dependent” volatile species, measured by Fourier Transform Infrared Microspectrometry (FTIR) (H2O of 0.4–3.0 wt.% and CO2 of 114–1586 ppm) and electron microprobe (EMP), revealed that fast cooling pyroclasts like vesicular scoria preserve a ~1.5 times larger amount of CO2, S, Cl, and volatile species contained in melt inclusions from primitive olivine (Fo76–86). Evidence from geological mapping and drone surveys demonstrated the eruption chronology and spatial changes in eruption style from all the local vents along a N45 corridor. The mechanism by which LNG2 is degassed plays a critical role in increasing the explosivity uphill on the Villarrica flank from volcanic vents in the NE sector (<9 km minimum saturation depth) to the SW sector (<8.1 km), where many crystalline ballistic bombs were expulsed, rather than vesicular and spatter scoria.es_ES
Patrocinadordc.description.sponsorship(ANID) Fondecyt Iniciacion a la Investigacion de Philippe Robidoux, Etapa N11190816es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherMDPIes_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
Sourcedc.sourceGeoscienceses_ES
Keywordsdc.subjectEruptive stylees_ES
Keywordsdc.subjectVolatileses_ES
Keywordsdc.subjectVillarricaes_ES
Keywordsdc.subjectMelt inclusiones_ES
Keywordsdc.subjectLos Nevados groupes_ES
Títulodc.titleVolatile content implications of increasing explosivity of the strombolian eruptive style along the fracture opening on the NE Villarrica Flank: minor eruptive centers in the Los Nevados Group 2es_ES
Document typedc.typeArtículo de revistaes_ES
dc.description.versiondc.description.versionVersión publicada - versión final del editores_ES
dcterms.accessRightsdcterms.accessRightsAcceso abiertoes_ES
Catalogueruchile.catalogadorcfres_ES
Indexationuchile.indexArtículo de publícación WoSes_ES


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Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States