Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2585
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dc.contributor.authorallMorhange, C.; CEREGE, CJB, Universite´ Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, Franceen
dc.contributor.authorallMarriner, N.; CEREGE, CJB, Universite´ Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, Franceen
dc.contributor.authorallLaborel, J.; Universite´ de la Me´diterrane´e, Faculte´ des Sciences de Luminy, F-13288 Marseille, Franceen
dc.contributor.authorallTodesco, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallOberlin, C.; Centre de Datation par le Radiocarbone, Universite´ Lyon 1, F-69622 Villeurbanne, Franceen
dc.date.accessioned2007-10-09T09:29:34Zen
dc.date.available2007-10-09T09:29:34Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2585en
dc.description.abstractThe importance of Pozzuoli’s archaeological ruins in linking sea-level change and Earth deformation with volcanic activity has been recognized since the nineteenth century. The pillars of the Roman market were used as a paleotide gauge by pioneer geologists such as Lyell. For the first time, we have radiocarbon dated biological indicators on these remains, showing three 7 m relative sea-level highstands during the fifth century A.D., the early Middle Ages, and before the 1538 eruption of Monte Nuovo. These repeated uplift and subsidence cycles, not always followed by volcanic activity, have important implications for the evaluation of volcanic hazard.en
dc.language.isoEnglishen
dc.publisher.nameGSAen
dc.relation.ispartofGeologyen
dc.relation.ispartofseries2 / 34 (2006)en
dc.subjectvolcanologyen
dc.subjectarchaeologyen
dc.subjectsea levelen
dc.subjectcalderaen
dc.subjectPhlegrean Fieldsen
dc.subjectItalyen
dc.titleRapid lea-level movements and noneruptive crustal deformations in the Phlegrean Fields caldera, Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber93-96en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.identifier.doi10.1130/G21894.1en
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dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMorhange, C.en
dc.contributor.authorMarriner, N.en
dc.contributor.authorLaborel, J.en
dc.contributor.authorTodesco, M.en
dc.contributor.authorOberlin, C.en
dc.contributor.departmentCEREGE, CJB, Universite´ Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, Franceen
dc.contributor.departmentCEREGE, CJB, Universite´ Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, Franceen
dc.contributor.departmentUniversite´ de la Me´diterrane´e, Faculte´ des Sciences de Luminy, F-13288 Marseille, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentCentre de Datation par le Radiocarbone, Universite´ Lyon 1, F-69622 Villeurbanne, Franceen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCRNS,IRD,Coll France,CEREGE,Universitè Aix Marseille,Aix-en-Provence,France-
crisitem.author.deptUniversite´ de la Me´diterrane´e, Faculte´ des Sciences de Luminy, F-13288 Marseille, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0002-1910-151X-
crisitem.author.orcid0000-0002-7916-6059-
crisitem.author.orcid0000-0002-5939-0985-
crisitem.author.orcid0000-0002-5535-6181-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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