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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8521
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dc.contributor.authorallTurtù, A.; Dipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.authorallSatolli, S.; Dipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.authorallManiscalco, R.; Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università degli Studi di Catania, Catania, Italy.en
dc.contributor.authorallCalamita, F.; Dipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.authorallSperanza, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2013-02-18T11:10:22Zen
dc.date.available2013-02-18T11:10:22Zen
dc.date.issued2013-02-07en
dc.identifier.urihttp://hdl.handle.net/2122/8521en
dc.description.abstractWe report on a paleomagnetic study of the southern sector of the Olevano-Antrodoco-Sibillini (OAS) thrust front, which corresponds to the southern limb of the Northern Apennines (Italy) orogenic salient. A lively debate has developed regarding the oroclinal/progressive-arc versus non-rotational nature of the OAS, which has been alternatively interpreted as a dextral strike-slip fault, dextral transpressive fault, or frontal to oblique ramp that reactivated pre-existing Jurassic normal faults. Here, we document the paleomagnetism, integrated with biostratigraphic and structural data, of 52 new sites from both the OAS hanging wall and footwall. On the basis of 39 retained sites, we find a peculiar pattern of tectonic rotations along the OAS thrust that evidences four rotational domains. The thrust footwall is characterized by a southern domain that undergoes an approximately 30 counterclockwise rotation with respect to the stable foreland, and an approximately nonrotated domain. The data from the hanging wall indicate the occurrence of a dextral strike-slip component along the southern sector of the OAS thrust supported by a strong clockwise rotation close to the NE-SW lateral ramp, which rapidly fades 1 km from the thrust front. A slight but significant CW rotation observed in the remaining sites from the hanging wall confirms the progressive nature of the OAS, and its structural position as the southern limb of the Northern Apennines salient. Our detailed paleomagnetic study is crucial in discriminating between progressive-arc- and strike-slip-related components in the main curved orogenic front of the Northern Apennines.en
dc.language.isoEnglishen
dc.publisher.nameAGUen
dc.relation.ispartofJournal Of Geophysical Research: SOLID EARTHen
dc.relation.ispartofseries/ 118 (2013)en
dc.subjectNorthern Apenninesen
dc.subjectOlevano-Antrodoco-Sibillini thrusten
dc.subjectoblique thrustsen
dc.subjectprogressive-arcen
dc.subjecttectonic rotationsen
dc.subjectpaleomagnetismen
dc.titleUnderstanding progressive-arc- and strike-slip-related rotations in curve-shaped orogenic belts: The case of the Olevano-Antrodoco-Sibillini thrust (Northern Apennines, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1-15en
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.identifier.doi10.1002/jgrb.50096en
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dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.contributor.authorTurtù, A.en
dc.contributor.authorSatolli, S.en
dc.contributor.authorManiscalco, R.en
dc.contributor.authorCalamita, F.en
dc.contributor.authorSperanza, F.en
dc.contributor.departmentDipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.departmentDipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.departmentDipartimento di Scienze Biologiche, Geologiche e Ambientali, Università degli Studi di Catania, Catania, Italy.en
dc.contributor.departmentDipartimento di Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
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 Ingegneria e Geologia, Università “G. D’Annunzio” di Chieti-Pescara, Chieti, Italy.-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy-
crisitem.author.deptDipartimento di Scienze Biologiche, Geologiche e Ambientali, Sezione Scienze della Terra – Università di Catania, Corso Italia 57, 95129, Catania, Italy-
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.orcid0000-0003-1026-044X-
crisitem.author.orcid0000-0002-1966-3061-
crisitem.author.orcid0000-0001-5492-8670-
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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