La Formación Marínredepósito de material jurásico durante el Mioceno (zona Subbética).
- Rey Sanz, Javier
- Martínez Gallego, Jorge
ISSN: 0213-683X
Year of publication: 1990
Issue: 8
Pages: 94-97
Type: Article
More publications in: Geogaceta
Abstract
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