Pliegues limitados por fallas en el subbético medio (sector de torre cardela, Granada)

Abstract

In 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 faults