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