Javier Rey Sanz, Jorge Martínez Gallego
An important volume about resedimented materials during the Burdigalian has been confused with the oolite Dogger even today. This article determines the Marin Formation, litostratigraphic unit that includes this rocks. It Will be caracterized by the prevalence of the conglomeratic beds (A facies), with planktonic foraminifera in the matrix
© 2001-2024 Fundación Dialnet · Todos los derechos reservados