M. Gutiérrez Claverol, Miguel Torres Alonso
The top of the Cretaceous section at Oviedo has been studied from the stratigraphic, petrogra phic and paleontological point of view, in arder to increase the know!edge of a previosly little know sequence. An abundant microfossil assemblage found there permitted dating it, far the first time, as of Santonian age.
© 2001-2024 Fundación Dialnet · Todos los derechos reservados