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dc.date.accessioned 2021-06-16T13:26:54Z
dc.date.available 2021-06-16T13:26:54Z
dc.date.issued 2015
dc.identifier.uri http://sedici.unlp.edu.ar/handle/10915/120341
dc.description.abstract The morphology, texture, grain size and other physicochemical characteristics of pyroclastic material from the first phases of the Puyehue-Cordon Caulle volcanic complex (PCCVC) eruption, (Southern Andes, Chile), can be associated to the model recently reported for the magma storage and its ascent conditions. The eruption started June 4th 2011, and the studied volcanic material corresponds to that collected in Argentine territory at different distances from the source, between 4 and 12 June 2011. The explosive-effusive volcanic process of the first days occurred with the simultaneous emplacement of lava flows and the venting of pyroclastic material, ejecting two well differentiated types of particles. The more abundant was constituted by rhyolitic and light color pumice fragments, characterized by a typical vesicular texture, easy fragmentation and absence of occluded crystalline phases. Particles found in minor proportion were dark color, different in shape and texture and rich in Fe and Ti. They seemed to be more effective for the interaction with emitted gases in the upper part of the column, for this reason, they appeared partially covered by condensation products. The ascent conditions of the magma affected its rheological behavior through variations in the degassing, viscosity and fragmentation. On the other hand, distance to the source, depositional time, volcanic evolution and environmental conditions are factors that affect the chemical composition of collected ash. So, the SiO2/FeO ratio not only increases with the distance but also with the deposition time and volcanic activity. The work was done with the aid of several techniques such as a laser-sediment analyzer, X-ray diffraction (XRD), chemical analysis (bulk and surface), SEM microscopy and Raman “microprobe” spectroscopy. On the other hand, the physicochemical behavior of the pyroclastic material allows us to suggest eventual applications. en
dc.format.extent 302-315 es
dc.language en es
dc.subject Pyroclastic materials es
dc.subject Chemical composition es
dc.subject Mineralogy es
dc.subject Sem microscopy es
dc.subject Raman spectroscopy es
dc.title Pyroclasts of the first phases of the explosive-effusive PCCVC volcanic eruption: physicochemical analysis en
dc.type Articulo es
sedici.identifier.other https://doi.org/10.4236/ampc.2015.58030 es
sedici.identifier.issn 2162-5328 es
sedici.creator.person Botto, Irma Lía es
sedici.creator.person Barone, Vicente es
sedici.creator.person Canafoglia, María Elena es
sedici.creator.person Rovere, Elizabeth es
sedici.creator.person Violante, Roberto es
sedici.creator.person González, María José es
sedici.creator.person Gazzoli, Delia es
sedici.creator.person Schalamuk, Isidoro Bernardo es
sedici.subject.materias Química es
sedici.description.fulltext true es
mods.originInfo.place Centro de Química Inorgánica es
mods.originInfo.place Instituto de Recursos Minerales es
sedici.subtype Articulo es
sedici.rights.license Creative Commons Attribution 4.0 International (CC BY 4.0)
sedici.rights.uri http://creativecommons.org/licenses/by/4.0/
sedici.description.peerReview peer-review es
sedici.relation.journalTitle Advances in Materials Physics and Chemistry es
sedici.relation.journalVolumeAndIssue vol. 5, no. 8 es


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Creative Commons Attribution 4.0 International (CC BY 4.0) Excepto donde se diga explícitamente, este item se publica bajo la siguiente licencia Creative Commons Attribution 4.0 International (CC BY 4.0)