Pliegues tumbados en los Alpujárrides de Sierra de Las Estancias (Cordilleras Béticas orientales)

dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorJabaloy, A.
dc.contributor.authorCampos, J.
dc.contributor.authorFernández Fernández, Estefanía
dc.date.accessioned2015-04-29T09:07:42Z
dc.date.available2015-04-29T09:07:42Z
dc.date.issued1997
dc.description.abstractThe structure of Los Blanquizares-Oria Alpujárríde unit in northern Sierra de Las Estancias is mainly determined by kilometric recumbeot North vergent folds. Foliation axial planar to these folds is a crenulation foliation in schists. Large folds are deformed by mylonite bands and by the Alpujárríde-Maláguide fault structures. The interference with late open folds develops large 'tête plongeante' structures in the area. In addition, other late deformation structures (normal and strike-slip faults and dykes) have been recognized in the areaen_US
dc.identifier.urihttp://hdl.handle.net/10272/10464
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.otherRecumbent foldsen_US
dc.subject.otherSierra de Las Estanciasen_US
dc.subject.otherAlpujárridesen_US
dc.subject.otherSE Spainen_US
dc.titlePliegues tumbados en los Alpujárrides de Sierra de Las Estancias (Cordilleras Béticas orientales)en_US
dc.titleRecumbent folds in the Alpujárrides of the Sierra de Las Estancias (Eastern Betic Cordilleras)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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