Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2950
DC FieldValueLanguage
dc.contributor.authorallMattei, M.; Università Roma Treen
dc.contributor.authorallCifelli, F.; Università Roma Treen
dc.contributor.authorallD'Agostino, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2007-12-04T15:00:10Zen
dc.date.available2007-12-04T15:00:10Zen
dc.date.issued2007-09-14en
dc.identifier.urihttp://hdl.handle.net/2122/2950en
dc.description.abstractThe present-day arcuate shape of the Calabrian Arc has been accomplished during Neogene and Early Pleistocene by large and opposite vertical axis rotations along the two arms of the Arc. Clockwise (CW) rotations have been systematically registered in Sicily and Calabria, whereas counterclockwise (CCW) rotations were measured in Southern Apennines. Such opposite vertical axis rotations ceased in the uppermost part of the Lower Pleistocene (about 1 Ma ago) along almost the entire Calabrian Arc and are not observed in the present-day GPS velocity field. The end of the Calabrian Arc bending during the Quaternary marks a decrease in the efficiency of the tectonic processes related to the long-lived subduction of the Ionian slab, which caused the halting of the back-arc opening in the Southern Tyrrhenian Sea.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEarth Planetary Science Lettersen
dc.relation.ispartofseries3-4 / 263 (2007)en
dc.subjectCalabrian Arcen
dc.subjectsubductionen
dc.subjectpaleomagnetismen
dc.subjectGPSen
dc.titleThe evolution of the Calabrian Arc: Evidence from paleomagnetic and GPS observationsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber259-274en
dc.identifier.URLhttp://www.sciencedirect.com/en
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformationsen
dc.identifier.doi10.1016/j.epsl.2007.08.034en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMattei, M.en
dc.contributor.authorCifelli, F.en
dc.contributor.authorD'Agostino, N.en
dc.contributor.departmentUniversità Roma Treen
dc.contributor.departmentUniversità Roma Treen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli studi di Roma TRE-
crisitem.author.deptUniversità degli studi di Roma TRE-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0002-0444-6240-
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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