Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5378
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dc.contributor.authorallIsaia, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallMarianelli, P.; Dipartimento di Scienze della Terra, Universita` degli Studi di Pisaen
dc.contributor.authorallSbrana, A.; Dipartimento di Scienze della Terra, Universita` degli Studi di Pisaen
dc.date.accessioned2009-12-23T14:06:30Zen
dc.date.available2009-12-23T14:06:30Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5378en
dc.description.abstractThe Campi Flegrei caldera is one of the highest risk volcanic areas on the Earth. Our research documents a 150 year-long period of intense volcanism following less than 200 years of repose after the Agnano-Monte Spina Plinian eruption (4.1 ka). The new data show that the renewal of volcanism was preceded by an uplift of a few tens of meters, triggered by mafic refilling of reservoirs at depths of 3 km or less. Our studies also indicate for the first time the occurrence of contemporaneous eruptions from at locations in different sectors of the caldera. These results suggest that a future eruptive crisis will likely be preceded by several meters of caldera-wide uplift in response to magma movements at depth. The trend of uplift of the caldera since 1969 may thus represent the unrest expected before a renewal of volcanism within an interval of decades to centuries.en
dc.language.isoEnglishen
dc.publisher.nameAguen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries/36(2009)en
dc.subjectCalderaen
dc.subjectCampi Flegreien
dc.titleCaldera unrest prior to intense volcanism in Campi Flegrei (Italy) at 4.0 ka B.P.: Implications for caldera dynamics and future eruptive scenariosen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL21303en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.subject.INGV05. General::05.02. Data dissemination::05.02.03. Volcanic eruptionsen
dc.identifier.doi10.1029/2009GL040513en
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dc.description.obiettivoSpecifico3.5. Geologia e storia dei vulcani ed evoluzione dei magmien
dc.description.obiettivoSpecifico4.3. TTC - Scenari di pericolosità vulcanicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorIsaia, R.en
dc.contributor.authorMarianelli, P.en
dc.contributor.authorSbrana, A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Universita` degli Studi di Pisaen
dc.contributor.departmentDipartimento di Scienze della Terra, Universita` degli Studi di Pisaen
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 OV, Napoli, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Via S. Maria 53, 56126 Pisa, Italy.-
crisitem.author.orcid0000-0001-7277-2358-
crisitem.author.orcid0000-0001-9535-8635-
crisitem.author.orcid0000-0003-1373-0603-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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