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

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

ISSN: 0213-683X

Ano de publicación: 1990

Número: 8

Páxinas: 94-97

Tipo: Artigo

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Outras publicacións en: Geogaceta

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Resumo

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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