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http://hdl.handle.net/2122/8929
DC Field | Value | Language |
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dc.contributor.authorall | Kahl, M.; Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität Bochum, Bochum 44780, Germany | en |
dc.contributor.authorall | Chakraborty, S.; Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität Bochum, Bochum 44780, Germany | en |
dc.contributor.authorall | Costa, F.; Earth Observatory of Singapore, Nanyang Technological University, Singapore 639798, Singapore | en |
dc.contributor.authorall | Pompilio, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia | en |
dc.contributor.authorall | Liuzzo, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Viccaro, M.; Dipartimento di Scienze Biologiche, Geologiche e Ambientali— Sezione di Scienze della Terra, Università di Catania, Corso Italia 57, Catania 95129, Italy | en |
dc.date.accessioned | 2014-02-14T11:24:05Z | en |
dc.date.available | 2014-02-14T11:24:05Z | en |
dc.date.issued | 2013-01-30 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8929 | en |
dc.description.abstract | One of the major objectives of volcanology remains relating variations in surface monitoring signals to the magmatic processes at depth that cause these variations. We present a method that enables compositional and temporal information stored in zoning of minerals (olivine in this case) to be linked to observations of real-time degassing data. The integrated record may reveal details of the dynamics of gradual evolution of a plumbing system during eruption. We illustrate our approach using the 2006 summit eruptive episodes of Mt. Etna. We find that the history tracked by olivine crystals, and hence, most likely the magma pathways within the shallow plumbing system of Mt. Etna, differed considerably between the July and October eruptions. The compositional and temporal record preserved in the olivine zoning patterns reveal two mafic recharge events within months of each other (June and September 2006), and each of these magma supplies may have triggered the initiation of different eruptive cycles (July 14–24 and August 31–December 14). Correlation of these observations with gas monitoring data shows that the systematic rise of the CO2/SO2gas values is associated with the gradual (preand syn-eruptive) supply of batches of gas-rich mafic magma into segments of Etna’s shallow plumbing system, where mixing with pre-existing and more evolved magma occurred. | en |
dc.description.sponsorship | This work was funded by the German Science Foundation as part of the collaborative research centre (SFB) on Rheology of the Crust—from the upper crust to the subduction zone (SFB 526). | en |
dc.language.iso | English | en |
dc.publisher.name | Springer Berlin Heidelberg | en |
dc.relation.ispartof | Bulletin of volcanology | en |
dc.relation.ispartofseries | /75 (2013) | en |
dc.subject | Crystal zoning | en |
dc.subject | Plumbing system Mt. Etna | en |
dc.subject | Magma mixing | en |
dc.subject | Gas monitoring | en |
dc.title | Compositionally zoned crystals and real-time degassing data reveal changes in magma transfer dynamics during the 2006 summit eruptive episodes of Mt. Etna | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 692 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.01. Gases | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.03. Magmas | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring | en |
dc.subject.INGV | 05. General::05.02. Data dissemination::05.02.01. Geochemical data | en |
dc.subject.INGV | 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions | en |
dc.subject.INGV | 05. General::05.09. Miscellaneous::05.09.99. General or miscellaneous | en |
dc.identifier.doi | 10.1007/s00445-013-0692-7 | en |
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J Petrol 53(4):801–840 Viccaro M, Giacomoni PP, Ferlito C, Cristofolini R (2010) Dynamics of magma supply at Mt. Etna volcano (Southern Italy) as revealed by textural and compositional features of plagioclase phenocrysts. Lithos 116:77–91 Zellmer GF, Blake S, Vance D, Hakesworth C, Turner S (1999) Plagioclase residence times at two island arc volcanoes (Kameni islands, Santorini and Soufriere, St. Vincent) determined by Sr diffusion systematics. Contrib Mineral Petrol 136:345–357 | en |
dc.description.obiettivoSpecifico | 2V. Dinamiche di unrest e scenari pre-eruttivi | en |
dc.description.obiettivoSpecifico | 3V. Dinamiche e scenari eruttivi | en |
dc.description.obiettivoSpecifico | 5V. Sorveglianza vulcanica ed emergenze | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 0258-8900 | en |
dc.relation.eissn | 1432-0819 | en |
dc.contributor.author | Kahl, M. | en |
dc.contributor.author | Chakraborty, S. | en |
dc.contributor.author | Costa, F. | en |
dc.contributor.author | Pompilio, M. | en |
dc.contributor.author | Liuzzo, M. | en |
dc.contributor.author | Viccaro, M. | en |
dc.contributor.department | Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität Bochum, Bochum 44780, Germany | en |
dc.contributor.department | Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität Bochum, Bochum 44780, Germany | en |
dc.contributor.department | Earth Observatory of Singapore, Nanyang Technological University, Singapore 639798, Singapore | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.department | Dipartimento di Scienze Biologiche, Geologiche e Ambientali— Sezione di Scienze della Terra, Università di Catania, Corso Italia 57, Catania 95129, Italy | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität Bochum, Bochum 44780, Germany | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
crisitem.author.dept | Università degli Studi di Catania | - |
crisitem.author.orcid | 0000-0001-5766-2417 | - |
crisitem.author.orcid | 0000-0002-1409-5325 | - |
crisitem.author.orcid | 0000-0002-0742-0679 | - |
crisitem.author.orcid | 0000-0002-3099-7505 | - |
crisitem.author.orcid | 0000-0002-7050-9879 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 05. General | - |
crisitem.classification.parent | 05. General | - |
crisitem.classification.parent | 05. General | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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