Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3682
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dc.contributor.authorallMantovani, E.; Dipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.authorallViti, M.; Dipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.authorallBabbucci, D.; Dipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.authorallAlbarello, D.; Dipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.date.accessioned2008-02-26T13:35:10Zen
dc.date.available2008-02-26T13:35:10Zen
dc.date.issued2007-06en
dc.identifier.urihttp://hdl.handle.net/2122/3682en
dc.description.abstractIt is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSWNNE convergence between Africa (Nubia) and Eurasia and that the significant difference between this kinematics and the one provided by global models (SSE-NNW convergence e.g., the NUVEL-1) may be due to the fact that those models interpret North Atlantic data by adopting an oversimplified two-plate configuration, which cannot account for the occurrence of significant seismotectonic activity inside the presumed Nubia and Eurasia blocks. It is shown that the adoption of a new plate configuration involving the Iberia and Morocco microplates, strongly suggested by geological and seismotectonic evidence, makes it possible to identify a kinematic model compatible within errors with the constraints recognized in the Mediterranean region and with the NUVEL-1 North Atlantic data set. Some considerations are made about why the present-day Nubia-Eurasia kinematic models inferred from geodetic observations are significantly different from long-term models, such as model NUVEL- 1 and the one proposed in this work.en
dc.language.isoEnglishen
dc.relation.ispartofseries3/50 (2007)en
dc.subjectNubia-Eurasia kinematicsen
dc.subjectMediterranean regionen
dc.subjectPlio-Quaternary deformationen
dc.titleNubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidenceen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
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dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorMantovani, E.en
dc.contributor.authorViti, M.en
dc.contributor.authorBabbucci, D.en
dc.contributor.authorAlbarello, D.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Siena, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Siena, Italy-
crisitem.author.deptUniversity of Siena, Italy-
crisitem.author.deptUniversity of Siena, Italy-
crisitem.author.deptDipartimento di Scienze Fisiche, della Terra e dell’Ambiente, University of Siena-
crisitem.author.orcid0000-0002-9226-4681-
crisitem.classification.parent04. Solid Earth-
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