La Formación Marínredepósito de material jurásico durante el Mioceno (zona Subbética).
- Rey Sanz, Javier
- Martínez Gallego, Jorge
ISSN: 0213-683X
Argitalpen urtea: 1990
Zenbakia: 8
Orrialdeak: 94-97
Mota: Artikulua
Beste argitalpen batzuk: Geogaceta
Garapen Iraunkorreko Helburuak
Laburpena
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