La Formación Marín: redepósito de material jurásico durante el Mioceno (zona Subbética).

• Autores: Javier Rey Sanz, Jorge Martínez Gallego
• Localización: Geogaceta, ISSN 0213-683X, Nº. 8, 1990, págs. 94-97
• Idioma: español
• Enlaces
  • Texto completo
• Resumen

  • 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