Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/474
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dc.contributor.authorallAcocella, V.; Dipartimento di Scienze Geologiche Roma TRE, Roma, Italyen
dc.contributor.authorallNeri, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.date.accessioned2005-10-14T13:34:52Zen
dc.date.available2005-10-14T13:34:52Zen
dc.date.issued2005-02en
dc.identifier.urihttp://hdl.handle.net/2122/474en
dc.description.abstractThe strike-slip Pernicana fault system (PFS) was activated along the eastern flank of Mt. Etna during an earthquake in September 2002 and, one month later, during the eruption of the NE Rift. Structural and volcanological data suggest that the PFS was activated as a result of the slide of the NE flank of Etna. This activation produced surface fracturing on walls and on paved and unpaved roads. The segments of the PFS, arranged in a right stepping en échelon configuration, show (a) an inverse proportion between length and frequency; (b) fractal behavior over scales of 10−2 –101 m, between their length, overstep and overlap; (c) consistent strike with regard to their fault array; and (d) a progressive eastward decrease in the displacement, along the smallest faults. The consistent geometric and kinematic features of the PFS, related to the sector collapse of Etna, are similar to those of faults in strike-slip settings.en
dc.format.extent520 bytesen
dc.format.extent1265348 bytesen
dc.format.mimetypetext/htmlen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Structural Geologyen
dc.relation.ispartofseries2/27(2005)en
dc.subjectActive faultingen
dc.subjectStrike-slip faultsen
dc.subjectFractal behavioren
dc.subjectVolcano collapseen
dc.subjectMt. Etnaen
dc.subjectPernicana fault systemen
dc.titleStructural features of an active strike-slip fault on the sliding flank of Mt. Etna (Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber343-355en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.identifier.doi10.1016/j.jsg.2004.07.006en
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dc.description.fulltextpartially_openen
dc.contributor.authorAcocella, V.en
dc.contributor.authorNeri, M.en
dc.contributor.departmentDipartimento di Scienze Geologiche Roma TRE, Roma, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-5890-3398-
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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