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The structural features of the precambrian and paleozoic sediments have been studied in the outcrops located to the NE o Calatayud, in the Iberian Range. The zone was affected by three deformation phases. The first gave rise to folds with a NW-SE orientation and a generalized cleavage. The second produced reverse faults and thrusts, homoaxial with the former structures. The third is characterized by folds WNW-NW and a crenulation cleavage. These deformation phases took place during the hercynian times.  Se estudian los aspectos estructurales de los materiales prec&#225;mbricos y paleozoicos aflorantes al NE de Calatayud, en la Cordillera Ib&#233;rica. La zona ha sido afectada por tres fases de deformaci&#243;n. La primera fase da lugar a pliegues de orientaci&#243;n NW-SE y una esquistosidad generalizada. La segunda fase produce fallas inversas y cabalgamientos homoaxiales con las estructuras anteriores. La tercera fase est&#225; caracterizada por pliegues WNW-NW y una esquistosidad de crenulaci&#243;n. Estas fases de deformaci&#243;n tuvieron lugar durante los tiempos herc&#237;nicos

La deformación hercínica en los Macizos Paleozoicos Nororientales de la Cordillera Ibérica