Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4634
DC FieldValueLanguage
dc.contributor.authorallBonini, M.en
dc.contributor.authorallCorti, G.en
dc.contributor.authorallSoukoutis, D.en
dc.contributor.authorallVannucci, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallGasperini, P.en
dc.contributor.authorallCloetingh, S.en
dc.date.accessioned2008-12-12T08:26:53Zen
dc.date.available2008-12-12T08:26:53Zen
dc.date.issued2003en
dc.identifier.urihttp://hdl.handle.net/2122/4634en
dc.description.abstractWe show how analogue modelling provides insights into complex crustal block kinematics and the seismotectonics of active areas undergoing contraction, such as the Iranian region. The seismotectonic model deriving from this analysis is consistent with partitioning of the N-directed Arabia indentation into a composite system of collision-oblique and collision-parallel seismogenetic belts. These features include (1) two main conjugate transpressive belts (the dextral NW – SE-trending Zagros belt and the NE – SW-trending sinistral Elburz-Aran-Torud (EAT) belt), and (2) a modest lateral escape of Central Iran towards the Lut block along the Nayband belt. This cinematic model fits the seismic activity and the current fault pattern of the region. Also, the velocity field scaled from the model to nature shows a good similarity with previous numerical modelling as well as with deformation rates along the first-order seismogenetic belts determined by plate tectonic models and GPS data. D 2003 Elsevier B.V. All rights reserved.en
dc.language.isoEnglishen
dc.relation.ispartofTectonophysicsen
dc.relation.ispartofseries376en
dc.subjectContinental collisionen
dc.subjectIranen
dc.subjectSeismotectonicsen
dc.subjectAnalogue modellingen
dc.subjectMoment tensor sumen
dc.titleInsights from scaled analogue modelling into the seismotectonics of the Iranian regionen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber137-149en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorBonini, M.en
dc.contributor.authorCorti, G.en
dc.contributor.authorSoukoutis, D.en
dc.contributor.authorVannucci, G.en
dc.contributor.authorGasperini, P.en
dc.contributor.authorCloetingh, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCNR-IGG, Firenze-
crisitem.author.deptIstituto di Geoscienze e Georisorse, CNR, Firenze, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptUniversità di Bologna-
crisitem.author.orcid0000-0003-4818-8076-
crisitem.author.orcid0000-0001-7399-4438-
crisitem.author.orcid0000-0003-0918-0784-
crisitem.author.orcid0000-0002-5314-0563-
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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