Una modificación al modelo genético para la Formación Molicias (Tortoniense superior, Depresión de Guadix, S de España)

• Juan Antonio Vera Torres ^[1] ; J. Rodríguez-Fernández ^[1]
  1. [1] Geociencias- Medio-Ambiente
• Localización: Geogaceta, ISSN 0213-683X, Nº. 5, 1988, págs. 26-29
• Idioma: español
• Enlaces
  • Texto completo (pdf)
• Dialnet Métricas: 1 Cita
• Resumen

  • The Molidas Formation has traditionally been interpreted as being a basinward prograding, plarform-talus-basin system, deposited in a relatively rising-sea-level environment.

    The proposed modification to this model is that the greater part of the turbidite ar the result of brusque drops in sea level which caused erosion of part of the platform and the consequent redeposition of reworked material within the deeper parts of the basin