Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8027
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dc.contributor.authorallBressan, G.; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
dc.contributor.authorallGentile, G. F.; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
dc.contributor.authorallTondi, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallde Franco, R.; Consiglio Nazionale delle Ricerche, Ist. Dinamica dei Processi Ambientali, Milano, Italyen
dc.contributor.authorallUrban, S.; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
dc.date.accessioned2012-08-23T12:42:06Zen
dc.date.available2012-08-23T12:42:06Zen
dc.date.issued2012-06en
dc.identifier.urihttp://hdl.handle.net/2122/8027en
dc.description.abstractThe three-dimensional pattern of elastic moduli (bulk modulus, Young modulus, shear modulus) of the upper crust (0-10 km depth) has been determined in the Friuli area (north-eastern Italy) from the 3D Vp, Vp/Vs and density structures. Firstly, 3D Pwave velocity and P to S velocity ratio were modeled by joint inversion for hypocentres and velocity structure. Then, we apply the tomographic inversion method of Sequential Integrated Inversion (SII) to recover the three dimensional density structure. The pattern of the elastic moduli is characterized by marked lateral and depth variations that reflect the geologic-structural heterogeneity of the area, produced by the superposition of several tectonic phases with different orientations of the principal axes of stress. The bulk (K), Young (E) and shear (G) moduli image a high rigidity body with an irregular shape, at 4-8 km depth. The body is characterized by G ≥ 3.2·1010 N·m-2, K ≥ 6.8·1010 N·m-2 and E ≥ 8.4·1010 N·m-2 and is associated to platform limestones and dolomitic rocks. The seismicity is mainly located along the sharp variations of the moduli pattern, in or adjacent to high rigidity zones. The most severe earthquakes (ML between 4.5 and 6.4), occurred in the study area from 1976 to the present day, are located in a transition zone from high to low rigidity patterns. Our interpretation is that the elastic moduli variations, closely related to variability in rock mechanical properties, influence the occurrence of earthquakes by processes of stress concentrations. The values of the elastic moduli recently obtained from laboratory measurements on the main lithologic units fall in the middlehigh range of the values obtained with the present investigation. Keywords: Seismic tomography, gravity anomalies, seismicity, elastic moduli, Friuli, NE Italyen
dc.language.isoEnglishen
dc.publisher.nameIstituto Nazionale di Oceanografia e di Geofisica Sperimentale-OGSen
dc.relation.ispartofBollettino di Geofisica Teorica ed Applicataen
dc.relation.ispartofseries2/53 (2012)en
dc.subjectSeismic tomographyen
dc.subjectgravity anomaliesen
dc.subjectseismicityen
dc.subjectelastic modulien
dc.subjectFriulien
dc.subjectNE Italyen
dc.titleSequential integrated inversion of tomographic images and gravity data: an application to the Friuli area (Northeastern Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber191-212en
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocksen
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.02. Gravity methodsen
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methodsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
dc.identifier.doi10.4430/bgta0059en
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dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0006-6729en
dc.contributor.authorBressan, G.en
dc.contributor.authorGentile, G. F.en
dc.contributor.authorTondi, R.en
dc.contributor.authorde Franco, R.en
dc.contributor.authorUrban, S.en
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentConsiglio Nazionale delle Ricerche, Ist. Dinamica dei Processi Ambientali, Milano, Italyen
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italyen
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 Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italy-
crisitem.author.deptIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptIstituto Metodologie Analisi Ambientali CNR-
crisitem.author.deptIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Cussignacco (UD), Italy-
crisitem.author.orcid0000-0001-9400-3904-
crisitem.author.orcid0000-0002-7037-2833-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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