José Malagón, Pedro P. Hernáiz Huerta, C. Rodríguez Cañas, A. Serrano
The SW margin of the Basco-Cantabrian basin has suffered during the Alpine Orogeny the tectonic inversion of previous extensional structures and the overlapping of the Mesozoic series of the Plataforma Burgalesa over the Tertiary sediments of the Duero basin
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