Manuel A. Camacho Cerro, Manuel Abad de los Santos, Elena María Mantero Romero, Mercedes Cantano Martín, Raquel Martín Banda
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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