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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10246
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dc.contributor.authorallCultrera, F.; Università di Catania, Sezione di Scienze della Terra, Italyen
dc.contributor.authorallBarreca, G.; Università di Catania, Sezione di Scienze della Terra, Italyen
dc.contributor.authorallScarfì, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallMonaco, C.; Università di Catania, Sezione di Scienze della Terra, Italyen
dc.date.accessioned2016-02-23T13:46:09Zen
dc.date.available2016-02-23T13:46:09Zen
dc.date.issued2015-10en
dc.identifier.urihttp://hdl.handle.net/2122/10246en
dc.description.abstractBetween the October 2011 and the July 2012, several seismic swarms occurred in the Hyblean foreland domain of SE Sicily (Italy) along the Cavagrande Canyon, one of the most impressive fluvial incisions of Sicily. Despite the low magnitude of the events (main shock with M~3.7), they represent the biggest strain release of the Hyblean area over the last ten years. A careful wave-form analysis of the earthquakes revealed that most of them form a family of ―multiplets‖. These findings allow us to reconstruct the attitude of the accountable fault plane by interpolating their highprecision 3D location parameters into a GIS platform. A detailed morpho-structural analysis, performed at the ideal updip projection of the modelled plane, showed that during the Middle-Late Pleistocene the epicentral area has been deformed by a belt of extensional faults, a segment of which matches well with the computer-generated surface. Despite the field evidence, computed focal solutions support contrasting strike-slip kinematics on the same fault plane, clearly indicating a dextral shearing on this pre-existing normal fault. The seismic swarms nucleated on a small rupture area along a ~10 km long, NW-SE trending fault segment, that could be able to generate M~6 earthquakes. Following our analysis and looking at seismicity distribution in the SE portion of Hyblean area, we asses that a stress pattern reorganization occurred all over the Hyblean foreland between the Late Pleistocene and present-day. Change in the trajectory of the max stress axes (from vertical to horizontal) seems to have involved a pre-existing large scale fault configuration with considerable seismotectonic implications.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Science Limiteden
dc.relation.ispartofTectonophysicsen
dc.relation.ispartofseries/661(2015)en
dc.subjectHyblean forelanden
dc.subjectseismic sequencesen
dc.subjectfault reactivationen
dc.subject3D fault modellingen
dc.subjectstress changingen
dc.subjectseismotectonicsen
dc.titleFault reactivation by stress pattern reorganization in the Hyblean foreland domain of SE Sicily (Italy) and seismotectonic implicationsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber215-228en
dc.identifier.URLhttp://www.sciencedirect.com/science/article/pii/S0040195115004722en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.identifier.doi10.1016/j.tecto.2015.08.043en
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dc.description.obiettivoSpecifico1T. Geodinamica e interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0040-1951en
dc.relation.eissn1879-3266en
dc.contributor.authorCultrera, F.en
dc.contributor.authorBarreca, G.en
dc.contributor.authorScarfì, L.en
dc.contributor.authorMonaco, C.en
dc.contributor.departmentUniversità di Catania, Sezione di Scienze della Terra, Italyen
dc.contributor.departmentUniversità di Catania, Sezione di Scienze della Terra, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentUniversità di Catania, Sezione di Scienze della Terra, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze Biologiche, Geologiche e Ambientali - Sezione di Scienze della Terra, Università di Catania-
crisitem.author.deptDipartimento di Scienze Biologiche, Geologiche e Ambientali - Sezione di Scienze della Terra, Università di Catania-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptDipartimento di Scienze Biologiche, Geologiche e Ambientali, Sezione di Scienze della Terra, Università di Catania-
crisitem.author.orcid0000-0003-1140-6172-
crisitem.author.orcid0000-0002-5995-3880-
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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