Estructuras post-sedimentarias en el margen noroccidental de la Cuenca del Guadalquivir (Niebla, Candón, Valverde del Camino), SO de España

Abstract

Description of deformational structures in tertiary sediments, which have been interprerted as a result of a fluids migration process, along with the presence of preferential structural directions of fracture planes developed in the substratum. This fracture net could have been recently reactivated, so leading to the development of the described structures