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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1071
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dc.contributor.authorallGamberi, F.; ISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.authorallMarani, M.; ISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.authorallLanduzzi, V.; ISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.authorallMagagnoli, A.; ISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.authorallPenitenti, D.; ISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.authorallRosi, M.; Dipartimento di Scienze della Terra, Università di Pisaen
dc.contributor.authorallBertagnini, A.; Dipartimento di Scienze della Terra, Università di Pisaen
dc.contributor.authorallDi Roberto, A.; Dipartimento di Scienze della Terra, Università di Pisaen
dc.date.accessioned2006-03-24T13:48:41Zen
dc.date.available2006-03-24T13:48:41Zen
dc.date.issued2006-03-24en
dc.identifier.urihttp://hdl.handle.net/2122/1071en
dc.description.abstractThe VST02 cruise carried out in the summer of 2002 was focused at sedimentologic and volcanologic researches over selected areas of the deep portion of the Tyrrhenian sea. Chirp lines and seafloor samples were collected from the Calabrian slope surrounding Stromboli island, in the Marsili deep sea fan, in the Vavilov basin and in the Vavilov seamount. Submarine volcanic activity, both explosive and effusive, is occuring in the Stromboli edifice. Explosive submarine volcanism affects also the shallowest areas of the Vavilov seamount. Submarine carbonate lithification has been observed on the sediment-starved flanks of the Vavilov seamount. Acoustic transparent layers make up the recentmost infill of the Gortani basin, the easternmost portion of the Vavilov basin. Channels comprised of a variety of architectural elements and depositional lobes are the main elements of the Marsili deep-sea fan where, apparently, sedimentation occurs mainly through debris flow processes.en
dc.format.extent1437048 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofAnnals of geophysicen
dc.relation.ispartofseries2-3/49(2006)en
dc.subjectsubmarine volcanismen
dc.subjectsubmarine volcanic explosionsen
dc.subjectdeep-sea fanen
dc.subjectacoustic transparent layersen
dc.subjectcarbonate crustsen
dc.titleSedimentologic and volcanologic investigation of the deep tyrrhenian sea: preliminary result of cruise VST02en
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transporten
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocksen
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dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorGamberi, F.en
dc.contributor.authorMarani, M.en
dc.contributor.authorLanduzzi, V.en
dc.contributor.authorMagagnoli, A.en
dc.contributor.authorPenitenti, D.en
dc.contributor.authorRosi, M.en
dc.contributor.authorBertagnini, A.en
dc.contributor.authorDi Roberto, A.en
dc.contributor.departmentISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.departmentISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.departmentISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.departmentISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.departmentISMAR-CNR, Sezione di Geologia Marina, Bolognaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto di Scienze Marine – CNR, Sede di Geologia Marina di Bologna, Bologna, Italia-
crisitem.author.deptIstituto di Geologia Marina, CNR, Bologna, Italia-
crisitem.author.deptISMAR-CNR, Sezione di Geologia Marina, Bologna-
crisitem.author.deptISMAR-CNR, Sezione di Geologia Marina, Bologna-
crisitem.author.deptISMAR-CNR, Sezione di Geologia Marina, Bologna-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0003-4075-2242-
crisitem.author.orcid0000-0003-1167-8290-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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