La transición de pliegues de despegue a pliegues de propagación: el ejemplo del anticlinal de Aguilón (Cordillera Ibérica)

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dc.contributor.authorCortés Gracia, A. L.
dc.contributor.authorCasas Sainz, Antonio
dc.date.accessioned2017-03-08T10:11:31Z
dc.date.available2017-03-08T10:11:31Z
dc.date.issued1995
dc.description.abstractThe northern border of the Iberian Chain shows detachment and fault-propagation folds that deform the mesozoic and tertiary sedimerits near Zaragoza. The regional detachment level are the lutitic and gypsyferous beds of the Upper Triassic. The thickness of the cover and the detachment level determine the kinematic evolution of folds that show intermediate geometry between detachment and faultpropagation typesen_US
dc.identifier.urihttp://hdl.handle.net/10272/13418
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherDetachment folden_US
dc.subject.otherFault-propagation folden_US
dc.subject.otherAlpine thrustingen_US
dc.subject.otherDetachment folden_US
dc.subject.otherIberian Chainen_US
dc.titleLa transición de pliegues de despegue a pliegues de propagación: el ejemplo del anticlinal de Aguilón (Cordillera Ibérica)en_US
dc.titleOn the transition from detachment folds to fault-propagation folds: example from the Aguilon anticline (Iberian Chain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 19, (1995)