Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3156
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dc.contributor.authorallBurrato, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.authorallPoli, M. E.; Dipartimento di Georisorse e Territorio, University of Udine-
dc.contributor.authorallVannoli, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.authorallZanferrari, A.; Dipartimento di Georisorse e Territorio, University of Udine-
dc.contributor.authorallBasili, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.authorallGaladini, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italia-
dc.date.accessioned2007-12-12T16:36:41Z-
dc.date.available2007-12-12T16:36:41Z-
dc.date.issued2007-
dc.identifier.urihttp://hdl.handle.net/2122/3156-
dc.description.abstractWe present an overview of the seismogenic sources of northeastern Italy and western Slovenia, included in the last version of the Database of Individual Seismogenic Sources (DISS 3.0.2) and a new definition of the geometry of the Montello Source that will be included in the next release of the database. The seismogenic sources included in DISS are active faults capable of generating Mw > 5.5 earthquakes. We describe the method and the data used for their identification and characterization, discuss some implications for the seismic hazard and underline controversial points and open issues. In the Veneto-Friuli area (NE Italy), destructive earthquakes up to Mw 6.6 are generated by thrust faulting along N-dipping structures of the Eastern Southalpine Chain (ESC). Thrusting along the mountain front responds to about 2 mm/a of regional convergence, and it is associated with growing anticlines, tilted and uplifted Quaternary palaeolandsurfaces and forced drainage anomalies. In western Slovenia, dextral strike-slip faulting along the NW-SE trending structures of the Idrija fault system dominates the seismic release. Activity and style of faulting are defined by recent earthquakes (e.g. the Ms 5.7, 1998 Bovec-Krn Mt. and the Mw 5.2, 2004 Kobarid earthquakes), while the related recent morphotectonic imprint is still a debated matter. We reinterpreted a large set of tectonic data and developed a segmentation model for the outermost ESC thrust front. We also proposed the association of the four major shocks of the 1976 Friuli earthquake sequence with individual segments of three major thrust fronts. Although several sub-parallel active strike-slip strands exist in western Slovenia, we were able to positively identify only two segments of the Idrija fault system. A comparison of the regional GPS velocity with long-term geological slip-rates of the seismogenic sources included in DISS shows that from a quarter to half of the deformation is absorbed along the external alignment of thrust faults in Veneto and western Friuli. The partitioning of the deformation in western Slovenia among the different strike-slip strands could not be quantified.en
dc.description.sponsorshipINGV-DPC, Project S2, Grant to Research Units 2.4 and 1.1en
dc.language.isoengen
dc.relation.ispartofTectonophysicsen
dc.subjectearthquakesen
dc.subjectseismogenic sourcesen
dc.subjectNE Italyen
dc.subjectW Sloveniaen
dc.titleSources of Mw 5+ earthquakes in northeastern Italyand western Slovenia: an updated view based on geological and seismological evidenceen
dc.typemanuscript-
dc.description.statusIn pressen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.03. Geomorphologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.identifier.doi10.1016/j.tecto.2007.07.009-
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.obiettivoSpecifico5.1. TTC - Banche dati e metodi macrosismicien
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBurrato, P.-
dc.contributor.authorPoli, M. E.-
dc.contributor.authorVannoli, P.-
dc.contributor.authorZanferrari, A.-
dc.contributor.authorBasili, R.-
dc.contributor.authorGaladini, F.-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.departmentDipartimento di Georisorse e Territorio, University of Udine-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.departmentDipartimento di Georisorse e Territorio, University of Udine-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italia-
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