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dc.contributor.authorMacchiavelli, Chiaraes_ES
dc.contributor.authorVergés, Jaumees_ES
dc.contributor.authorSchettino, Antonioes_ES
dc.contributor.authorFernandez, Maneles_ES
dc.contributor.authorTurco, E.es_ES
dc.contributor.authorCasciello, Emilioes_ES
dc.contributor.authorTorné, Montserrates_ES
dc.contributor.authorPierantoni, Pietro Paoloes_ES
dc.contributor.authorTunini, Laviniaes_ES
dc.date.accessioned2018-01-16T09:02:21Z-
dc.date.available2018-01-16T09:02:21Z-
dc.date.issued2018-01-
dc.identifier.citationJournal of Geophysical Research: Solid Earth: (2018)es_ES
dc.identifier.issn2169-9356-
dc.identifier.urihttp://hdl.handle.net/10261/159073-
dc.description.abstractThis paper presents a new southern North Atlantic plate model from Late Cretaceous to present, with the aim of constraining the kinematics of the Iberian plate during the last 83.5 Myr. This model is presented along with a detailed isochron map generated through the analysis of 3 aeromagnetic tracks and ~400 ship tracks from the National Centers for Environmental Information database. We present a new technique to obtain well-constrained estimates of the Iberia-North America plate motions from magnetic anomalies, overcoming the scarcity of large-offset fracture zones and transform faults. We build an integrated kinematic model for NW Africa, Morocco, Iberia, Europe, and North America, which shows that the deformation is partitioned between Pyrenees and Betic-Rif orogenic domain during the Late Cretaceous-Oligocene time interval. In the Eastern Betics domain, the calculated amount of NW Africa-Iberia convergence is ~80 km between 83.5 and 34 Ma, followed by ~150 km since the Oligocene. The motion of Iberia relative to Europe in the Central Pyrenees is characterized by overall NE directed transpressional motion during the Campanian and the Paleocene, followed by NW directed transpressional movement until the Lutetian and overall NNW directed convergence from Bartonian to Chattian. This motion occurs along the axis of the Bay of Biscay from the Santonian-Campanian boundary to the middle Priabonian, subsequently jumping to King's Trough at Anomaly 17 (36.62 Ma). ©2017. American Geophysical Union.es_ES
dc.description.sponsorshipThe present work has been supported by ALPIMED (PIE-CSIC-201530E082) project.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccessen_EN
dc.subjectBetic-Rif systemes_ES
dc.subjectIberian kinematicses_ES
dc.subjectLigurian-Tethys closurees_ES
dc.subjectNW Africa-Europe convergencees_ES
dc.subjectPyreneeses_ES
dc.subjectSouthern North Atlantices_ES
dc.titleA New Southern North Atlantic Isochron Map: Insights Into the Drift of the Iberian Plate Since the Late Cretaceouses_ES
dc.typeArtículoes_ES
dc.identifier.doi10.1002/2017JB014769-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1002/2017JB014769es_ES
dc.identifier.e-issn2169-9313-
dc.embargo.terms2018-09-30es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
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