Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/424
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dc.contributor.authorallBonaccorso, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallSansosti, E.; Istituto per il Rilevamento Elettromagnetico dell’Ambiente (IREA), National Research Council (CNR), Napoli, Italy.en
dc.contributor.authorallBerardino, P.; Istituto per il Rilevamento Elettromagnetico dell’Ambiente (IREA), National Research Council (CNR), Napoli, Italy.en
dc.date.accessioned2005-09-27T10:44:59Zen
dc.date.available2005-09-27T10:44:59Zen
dc.date.issued2004-07en
dc.identifier.urihttp://hdl.handle.net/2122/424en
dc.description.abstractWe compare the results obtained from the modelling of EDM, GPS, levelling and tilt data measured in the first part of the 19911993 eruption at Etna to the InSAR data acquired during the second part. The geodetic changes are very marked in the first half of the eruption and constrain a deflation source located at a few kilometers of depth ( 3 km b.s.l.), in agreement with other independent geophysical evidence. SAR data, available during the second part of the eruption, were analysed for different time intervals in the second part of the eruption. The interpretation of SAR interferograms reveals a large-scale but less marked deflation of the volcano that could be caused by a deeper source. This second source is in accord with a second deeper anomaly revealed by recent seismic investigations. The combination of geodetic data modelling and SAR images suggests a complex plumbing system composed at least of two possible storage regions located at different depths.en
dc.format.extent513 bytesen
dc.format.extent749532 bytesen
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dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofPure and Applied Geophysicsen
dc.relation.ispartofseries7/161(2004)en
dc.subjectGeodesyen
dc.subjectSAR Interferometryen
dc.subjectground deformationen
dc.subjectMt. Etna volcanoen
dc.titleComparison of Integrated Geodetic Data Models and Satellite Radar Interferograms to Infer Magma Storage During the 19911993 Mt. Etna Eruptionen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1345-1357en
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoringen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesyen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniquesen
dc.identifier.doi10.1007/s00024-004-2508-3en
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dc.description.fulltextpartially_openen
dc.contributor.authorBonaccorso, A.en
dc.contributor.authorSansosti, E.en
dc.contributor.authorBerardino, P.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto per il Rilevamento Elettromagnetico dell’Ambiente (IREA), National Research Council (CNR), Napoli, Italy.en
dc.contributor.departmentIstituto per il Rilevamento Elettromagnetico dell’Ambiente (IREA), National Research Council (CNR), Napoli, Italy.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptCNR-IREA-
crisitem.author.deptIREA-CNR, Naples, Italy.-
crisitem.author.orcid0000-0002-4770-6006-
crisitem.author.orcid0000-0001-5450-6566-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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