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Structure and Kinematics of the Alpeñés fault (Iberian Chain)

dc.contributor.authorTena, S.
dc.contributor.authorCasas Sainz, Antonio
dc.description.abstractThe Alpenes anticline is a detachment fold of the Jurassic-Cretaceous cover, whose location and geometry is controlled by the Alpenes NNE-SSW-trending basement fault. This fault constituted the southwestern margin of the Aliaga basin (Iberian Chain) during the Cretaceous, with a normal movement slipping northwards and was re-activated during the Tertiary compression as a right-lateral strike-slipreverse fault The cumulative heave of the Alpehes fault in the detached mesozoic cover is about 400 m, the western block being uplifted with respect to the eastern block during the mesozoic extension and tertiary inversion.en_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherDetachment folden_US
dc.subject.otherBasement faulten_US
dc.subject.otherAlpenes faulten_US
dc.subject.otherIberian Chainen_US
dc.titleEstructura y cinemática de la falla de Alpeñés (Cordillera Ibérica)en_US
dc.titleStructure and Kinematics of the Alpeñés fault (Iberian Chain)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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