La Formación Marínredepósito de material jurásico durante el Mioceno (zona Subbética).

  1. Rey Sanz, Javier
  2. Martínez Gallego, Jorge
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1990

Issue: 8

Pages: 94-97

Type: Article

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

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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

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