Sanz de Galdeano, Carlos2014-10-292014-10-292003http://hdl.handle.net/10272/9012In the area of Torre Cardela, situated to the NE of Granada, there are NE-SW to NNE-SSW folds comprised among ENE-WSW dextral strike-slip fauts. The formation of all these structures are interpreted as singenetic, within a compressional elipsoid which o1 varies from WNW-ESE to NW-SE direction. These structures form part of the zone of deformations produced by the Cadiz-Alicante strike-slip faultsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/FaultsFoldsTranspressionBetic CordilleraSubbeticjournal articleopen access