Sanz de Galdeano, CarlosGalindo Zaldívar, JesúsLópez Garrido, Ángel CarlosAlfaro García, PedroRuiz Bustos, A.Marín Lechado, Carlos2014-07-092014-07-092006http://hdl.handle.net/10272/8466In 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 settingspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Growth synclineNeotectonicsActive TectonicsGuadix-Baza basinRodent toothjournal articleopen access