Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3541
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dc.contributor.authorallMacera, P.; Dipartimento di Scienze della Terra, Universita’ di Pisaen
dc.contributor.authorallGasperini, D.; Dipartimento di Scienze della Terra, Universita’ di Pisaen
dc.contributor.authorallPiromallo, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallBlichert-Toft, J.; Ecole Normale Superieure, Lyonen
dc.contributor.authorallBosch, D.; Universite ‘‘Montpellier 2", Montpellieren
dc.contributor.authorallDel Moro, A.; Istituto di Geoscienze e Georisorse, C.N.R., Pisaen
dc.contributor.authorallMartin, S.; Dipartimento di Chimica Fisica Matematica, Universita` Insubria, Comoen
dc.date.accessioned2008-01-15T07:59:05Zen
dc.date.available2008-01-15T07:59:05Zen
dc.date.issued2003en
dc.identifier.urihttp://hdl.handle.net/2122/3541en
dc.description.abstractMajor and trace element and Sr–Nd–Hf–Pb isotopic data for the most primitive Tertiary lavas from the Veneto region (South-Eastern Alps, Italy) show the typical features of HIMU hotspot volcanism, variably diluted by a depleted asthenospheric mantle component (87Sr/86Sri=0.70306–0.70378; "Ndi=+3.9 to +6.8; "Hfi=+6.4 to +8.1, 206Pb/204Pbi=18.786–19.574). P-wave seismic tomography of the mantle below the Veneto region shows the presence of low-velocity anomalies at depth, which is consistent with possible upwellings of plume material. Between the depths of 100–250 km the velocity anomalies are approximately 2–2.5% slower than average, implying a temperature excess of about 220–280 K, in agreement with estimates for other mantle plumes in the world. In this context, the Veneto volcanics may represent the shallow expression of a mantle upflow. The presence of a HIMU-DM component in a collision environment has significant geodynamic implications. Slab detachment and ensuing rise of deep mantle material into the lithospheric gap is proposed to be a viable mechanism of hotspot magmatism in a subduction zone setting.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Geodynamicsen
dc.relation.ispartofseries/36 (2003)en
dc.subjecttrace-elementen
dc.subjectisotopic compositionen
dc.subjectalkali basaltsen
dc.subjectcentral-Europeen
dc.subjectslab break-offen
dc.subjectplumeen
dc.titleGeodynamic implications of deep mantle upwelling in the source of Tertiary volcanics from the Veneto region (South-Eastern Alps)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber563–590en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
dc.identifier.doi10.1016/j.jog.2003.08.004en
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dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMacera, P.en
dc.contributor.authorGasperini, D.en
dc.contributor.authorPiromallo, C.en
dc.contributor.authorBlichert-Toft, J.en
dc.contributor.authorBosch, D.en
dc.contributor.authorDel Moro, A.en
dc.contributor.authorMartin, S.en
dc.contributor.departmentDipartimento di Scienze della Terra, Universita’ di Pisaen
dc.contributor.departmentDipartimento di Scienze della Terra, Universita’ di Pisaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentEcole Normale Superieure, Lyonen
dc.contributor.departmentUniversite ‘‘Montpellier 2", Montpellieren
dc.contributor.departmentIstituto di Geoscienze e Georisorse, C.N.R., Pisaen
dc.contributor.departmentDipartimento di Chimica Fisica Matematica, Universita` Insubria, Comoen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Ingegneria Civile, Edile-Architettura e Ambientale, Università dell’Aquila-
crisitem.author.deptDipartimento di Scienze della Terra, Universita’ di Pisa-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptEcole Normale Superieure, Lyon-
crisitem.author.deptUniversite ‘‘Montpellier 2", Montpellier-
crisitem.author.deptIstituto di Geoscienze e Georisorse, C.N.R., Pisa-
crisitem.author.deptDipartimento di Chimica Fisica Matematica, Universita` Insubria, Como-
crisitem.author.orcid0000-0003-3478-5128-
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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