The Bartonian to Lower Priabonian sediments of the St. Feliu de Codines-Gallifa deltaic complex belong to the Ebro basin filling, and are in contact with the Prelitoral Catalan Range. In these materials we have defiped several facies associations, from continental to deltaic and bioconstructed environments. The facies associations allow to establish genetic units with specific stacking patterns, wich are grouped in stratigraphic genetic units bounded by unconformities. These genetic units are the Rellinars and Mura sequences
© 2001-2024 Fundación Dialnet · Todos los derechos reservados