Structural analysis of the eastern sector of the Murguía diapir permits to disclose and map a number of geological structures related to the middle to late Cretaceous evolution of the diapir. These structures, not described so far in the literature, comprise syntectonic unconformities and synsedimentary scars related to rim synclines and anticlines that represent, respectively, the secondary and primary (inverted) peripheral troughs of the diapir.
© 2001-2025 Fundación Dialnet · Todos los derechos reservados