@article{10272/9012,
year = {2003},
url = {http://hdl.handle.net/10272/9012},
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},
publisher = {Sociedad Geológica de España},
title = {Pliegues limitados por fallas en el subbético medio (sector de torre cardela, Granada)},
title = {Folds comprised among faults in the Median Subbetic (Torre Cardela sector, Granada, Spain)},
author = {Sanz de Galdeano, Carlos},
}