Galindo Zaldívar, JesúsJabaloy, A.Campos, J.Fernández Fernández, Estefanía2015-04-292015-04-291997http://hdl.handle.net/10272/10464The 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 areaspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Recumbent foldsSierra de Las EstanciasAlpujárridesSE Spainjournal articleopen access