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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3936
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dc.contributor.authorallSatolli, S.; Dipartimento di Scienze della Terra, Università G. D’Annunzio, Chieti Scalo, Italyen
dc.contributor.authorallSperanza, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallCalamita, F.; Dipartimento di Scienze della Terra, Università G. D’Annunzio, Chieti Scalo, Italyen
dc.date.accessioned2008-07-07T13:06:02Zen
dc.date.available2008-07-07T13:06:02Zen
dc.date.issued2005en
dc.identifier.urihttp://hdl.handle.net/2122/3936en
dc.description.abstractWe report on the paleomagnetism (39 new sites) of Gran Sasso, an indenter-controlled salient of the external central Apennines formed by two orthogonal limbs. We find that Gran Sasso is a complex salient, paleomagnetically corresponding to neither a nonrotating nor an oroclinal end-member. Data from the core of the arc show that the indenter itself did not undergo any rotation. Conversely, rotations of variable magnitude and sign are observed along the curveshaped thrust fronts. Rotations are virtually absent at both end points of the arc. Moving toward the apex, progressively greater counterclockwise (CCW) and clockwise (CW) rotations occur along the E-Wand N-S fronts, respectively. The rotations increase continuously and more than linearly, reaching their maximum values (80 CCWand 50 CW) around the apex. Here, the more strongly CCW and CW rotated fronts are separated by a domain characterized by local block rotations. The inequality between the maximum CCW and CW rotation values is likely a consequence of the asymmetry of the indenter displacement direction (N70 E) with respect to the preorogenic trends of its margins (E-W and N-S). From an oroclinal point of view, the fronts close to the end points virtually define a nonrotating arc, while the pattern around the apex is similar to that of an orocline. We conclude that close to end points, nonrotational thrusting normal to the indenter margins occurred, while in the vicinity of the apex, the peritidal carbonates acted as an "ice breaker", pushing apart (and strongly rotating) the weaker multilayer located ahead.en
dc.language.isoEnglishen
dc.publisher.nameAGUen
dc.relation.ispartofTectonicsen
dc.relation.ispartofseries/ 24 (2005)en
dc.subjectPaleomagnetismen
dc.subjectGran Sassoen
dc.subjectTectonic rotationsen
dc.subjectArcuate belten
dc.titlePaleomagnetism of the Gran Sasso range salient (central Apennines, Italy): Pattern of orogenic rotations due to translation of a massive carbonate indenteren
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberTC4019en
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.identifier.doi10.1029/2004TC001771en
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dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorSatolli, S.en
dc.contributor.authorSperanza, F.en
dc.contributor.authorCalamita, F.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università G. D’Annunzio, Chieti Scalo, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università G. D’Annunzio, Chieti Scalo, 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 della Terra, Università di Chieti, Chieti, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy-
crisitem.author.orcid0000-0001-5492-8670-
crisitem.author.orcid0000-0002-1966-3061-
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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