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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8850
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dc.contributor.authorallMuñoz, J.-A.; Institut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.authorallBeamud, E.; Institut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.authorallFernández, O.; Repsol Exploración – Dirección de Geología, Madrid, Spain.en
dc.contributor.authorallArbués, P.; Institut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.authorallDinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallPoblet, J.; Departamento de Geología, Universidad de Oviedo, Oviedo, Spain.en
dc.date.accessioned2013-12-18T09:12:23Zen
dc.date.available2013-12-18T09:12:23Zen
dc.date.issued2013en
dc.identifier.urihttp://hdl.handle.net/2122/8850en
dc.description.abstractIntegration of structural, stratigraphic, and paleomagnetic data from the N–S trending structures of the Ainsa Oblique Zone reveals the kinematics of the major thrust salient in the central Pyrenees. These structures experienced clockwise vertical axis rotations that vary from 70° in the east (Mediano anticline) to 55° in the west (Boltaña anticline). Clockwise vertical axis rotations of 60° to 45° occurred from early Lutetian to late Bartonian when the folds and thrusts of the Ainsa Oblique Zone developed. This vertical axis rotation stage resulted from a difference of about 50 km in the amount of displacement on the Gavarnie thrust and an accompanying change in structural style at crustal scale from the central to the western Pyrenees, related to the NE–SW trending pinch out of Triassic evaporites at its basal detachment. A second rotation event of at least 10° took place since Priabonian, as a result of a greater displacement of the Serres Marginals thrust sheet with respect to the Gavarnie thrust sheet above the Upper Eocene-Oligocene salts. The deduced kinematics demonstrates that the orogenic curvature of the central Pyrenees is a progressive curvature resulting from divergent thrust transport direction. Layer parallel shortening mesostructures and kilometer-scale folds also developed by a progressive curvature related to divergent shortening directions during vertical axis rotation. Rotation space problems were solved by along-strike extension which triggered the formation of transverse extensional faults and diapirs at the outer arcs of structural bends.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofTectonicsen
dc.relation.ispartofseries/ 32 (2013)en
dc.subjectvertical-axis rotationen
dc.subjectthrust-sheeten
dc.subjectEoceneen
dc.subjectorogenen
dc.titleThe Ainsa Fold and thrust oblique zone of the central Pyrenees: Kinematics of a curved contractional system from paleomagnetic and structural dataen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1142–1175en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.identifier.doi10.1002/tect.20070en
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dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0278-7407en
dc.relation.eissn1944-9194en
dc.contributor.authorMuñoz, J.-A.en
dc.contributor.authorBeamud, E.en
dc.contributor.authorFernández, O.en
dc.contributor.authorArbués, P.en
dc.contributor.authorDinarès-Turell, J.en
dc.contributor.authorPoblet, J.en
dc.contributor.departmentInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.departmentInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.departmentRepsol Exploración – Dirección de Geología, Madrid, Spain.en
dc.contributor.departmentInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartamento de Geología, Universidad de Oviedo, Oviedo, Spain.en
item.openairetypearticle-
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item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.-
crisitem.author.deptInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.-
crisitem.author.deptRepsol Exploración – Dirección de Geología, Madrid, Spain.-
crisitem.author.deptInstitut Geomodels, Departament de Geodinàmica i Geofísica, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptDepartamento de Geología, Universidad de Oviedo, Oviedo, Spain.-
crisitem.author.orcid0000-0002-5546-2291-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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