Resumen de El pliegue sinsedimentario de Hinojares ( sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética ).
In the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the recent glacis, Pleistocene in age, shows two flexions parallel to the fold hinge and limbs.
This fold has been probably controlled by the Tiscar fault and formed within a NNE-SSW compressive setting.
