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

  1. Juan Antonio Vera Torres 1
  2. J. Rodríguez-Fernández 1
  1. 1 Geociencias- Medio-Ambiente
Revista:
Geogaceta

ISSN: 0213-683X

Any de publicació: 1988

Número: 5

Pàgines: 26-29

Tipus: Article

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Altres publicacions en: Geogaceta

Resum

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

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