Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6222
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dc.contributor.authorallDe Beni, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallGroppelli, G.; Istituto per la Dinamica dei Processi Ambientali–Sezione di Milano, Consiglio Nazionale delle Ricerche, via Mangiagalli 34, 20133 Milano, Italyen
dc.contributor.editorallGroppelli, G.; Istituto per la Dinamica dei Processi Ambientali–Sezione di Milano, Consiglio Nazionale delle Ricerche, via Mangiagalli 34, 20133 Milano, Italyen
dc.contributor.editorallViereck-Goette, L.; Intitut fùr Geowissenschaften Friedrich-Schiller-Universitàt Jena D-07749 Jena Germanyen
dc.date.accessioned2010-11-11T08:45:21Zen
dc.date.available2010-11-11T08:45:21Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6222en
dc.description.abstractAlthough ~50 radiometric age analyses have been performed on Etna, and there are many historical references, these are not enough to temporally constrain the geo- logical evolution of the volcano. In particular, a new stratigraphic framework based on lithostratigraphic and unconformity-bounded units has pointed out the presence of some stratigraphic uncertainty that can be resolved only with radiometric dating. For this reason, a dating project applying the 40 Ar/ 39 Ar incremental heating technique started in 2002. The results obtained improve our understanding and provide con- straints for Etna’s geological evolution; in addition, they show that the applied tech- nique is very useful for dating young basalts and quantifying the hiatus represented by unconformities, as well as for understanding their meaning.en
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Americaen
dc.relation.ispartofStratigraphy and Geology of Volcanic Areasen
dc.subjectAr/Ar datingen
dc.subjectEtnaen
dc.title40 Ar/ 39 Ar radiometric dating to constrain the volcanic stratigraphy: The Mt. Etna methodological case.en
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber241-248en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.identifier.doi10.1130/2010.2464(11)en
dc.description.obiettivoSpecifico3.5. Geologia e storia dei vulcani ed evoluzione dei magmien
dc.description.fulltextrestricteden
dc.contributor.authorDe Beni, E.en
dc.contributor.authorGroppelli, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto per la Dinamica dei Processi Ambientali–Sezione di Milano, Consiglio Nazionale delle Ricerche, via Mangiagalli 34, 20133 Milano, Italyen
dc.contributor.editorGroppelli, G.en
dc.contributor.editorViereck-Goette, L.en
dc.contributor.editordepartmentIstituto per la Dinamica dei Processi Ambientali–Sezione di Milano, Consiglio Nazionale delle Ricerche, via Mangiagalli 34, 20133 Milano, Italyen
dc.contributor.editordepartmentIntitut fùr Geowissenschaften Friedrich-Schiller-Universitàt Jena D-07749 Jena Germanyen
item.openairetypebook chapter-
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.deptC.N.R. – Istituto per la Dinamica dei Processi Ambientali, Milano, Italy-
crisitem.author.orcid0000-0002-9867-1704-
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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