Las facies terrígenas del Muschelkalk basal en el extremo noroccidental de la Cordillera Ibérica

  1. F. Pérez Mazario 1
  2. E. Aracil 2
  3. S. Hernando 1
  4. R. Rincón 1
  1. 1 Dpto. Estratigrafía U.C.M
  2. 2 Instituto de Geología Económica C.S.l.C
Revue:
Geogaceta

ISSN: 0213-683X

Année de publication: 1989

Número: 7

Pages: 18-20

Type: Article

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D'autres publications dans: Geogaceta

Résumé

Clastic Materials of basal Muschelkafk in the northestern edge of lberian Ranges represent subtidal environments and even high energy events in the inner platform (presence of H.C.S.). Such events disturb the ínter and supratidal sedimentation development of both under and overlaying units.

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