Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3533
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dc.contributor.authorallPiromallo, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallSpada, G.; Dipartimento di Fisica, Universita' di Bolognaen
dc.contributor.authorallSabadini, R.; Dipartimento di Scienze della Terra, Universita' di Milanoen
dc.contributor.authorallRicard, Y.; Laboratoire de Sciences de la Terre, ENS-Lyonen
dc.date.accessioned2008-01-14T11:53:54Zen
dc.date.available2008-01-14T11:53:54Zen
dc.date.issued1997en
dc.identifier.urihttp://hdl.handle.net/2122/3533en
dc.description.abstractBy means of a stratified Earth model with viscoelastic rheology, we have studied the long-term global fluctuations of Relative Sea Level (RSL) induced by subducting slabs. We have computed RSL variations for both a single subduction and a realistic distribution of slabs by a numerical simulation based on a simplified model of the subduction process. RSL is determined by the offset between the geoid and the dynamic topography; our analysis demonstrates that the latter provides the prevailing contribution. We have studied, in addition, the effects of rheological stratification upon the amplitude and time-evolution of these two quantities and, consequently, of RSL fluctuations. According to our results, an upper bound for the rate of RSL associated with subduction is of the order of 0.1 mm/yr, in agreement with previous studies. This rate of sea level variation is comparable with that attributed to changes in the tectonic regime on a large scale. This preliminary result corroborates the suggestion by other authors to include subduction in the list of geophysical mechanisms which contribute to long-term RSL fluctuations.en
dc.language.isoEnglishen
dc.publisher.nameKluwer Academic Publishersen
dc.relation.ispartofSurvey in Geophysicsen
dc.relation.ispartofseries/18(1997)en
dc.subjectdynamic topographyen
dc.subjectgeoiden
dc.subjectsea levelen
dc.subjectsubductionen
dc.subjectviscosity profileen
dc.titleRelative sea level variations caused by subductionen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber225–238en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
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dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPiromallo, C.en
dc.contributor.authorSpada, G.en
dc.contributor.authorSabadini, R.en
dc.contributor.authorRicard, Y.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDipartimento di Fisica, Universita' di Bolognaen
dc.contributor.departmentDipartimento di Scienze della Terra, Universita' di Milanoen
dc.contributor.departmentLaboratoire de Sciences de la Terre, ENS-Lyonen
item.openairetypearticle-
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 Roma1, Roma, Italia-
crisitem.author.deptInsitute of Physics, University of Urbino, Italy-
crisitem.author.deptUniversit`a di Milano - Milan, Italy-
crisitem.author.deptLaboratoire de Sciences de la Terre, ENS-Lyon-
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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