Deformation monitoring in Zafarraya Fault and Sierra Tejeda Antiform (Betic Cordillera, Spain) using satellite radar interferometry

The Betic-Rif cordilleras are build-up in the western Mediterranean by the deformations related to the Eurasian-African plate boundary. The recent NW-SE convergence produces the simultaneous development of large folds and faults in the central part of the Internal Zones of the Betic Cordilleras, which continues active up to Present. The uplift...