Ciclos deltaicos en el Jurásico Superior del flanco oeste del diapiro de Caldas da Rainha, Portugal

  1. C. Pérez Pérez 1
  2. C.A Bernardes 2
  3. Ángel Corrochano Sánchez 2
  1. 1 Dpto. de Geología, Univ. de Salamanca
  2. 2 Geociencias. Medio-Ambiente
Zeitschrift:
Geogaceta

ISSN: 0213-683X

Datum der Publikation: 1989

Nummer: 6

Seiten: 96-98

Art: Artikel

Andere Publikationen in: Geogaceta

Zusammenfassung

Three litoestratigraphic unites have been identified in the Sao Martinho do Porto sea cliffs, which correspond with three deltaic cycles. The paleocurrents analysis show that for the first two cycles, the sediments come from the Berlengas Massif situated in the SW; while the third come from the NE, controlled by the diapiric relief of the Caldas da Rainha