Las facies terrígenas del Muschelkalk basal en el extremo noroccidental de la Cordillera Ibérica
- F. Pérez Mazario 1
- E. Aracil 2
- S. Hernando 1
- R. Rincón 1
- 1 Dpto. Estratigrafía U.C.M
- 2 Instituto de Geología Económica C.S.l.C
ISSN: 0213-683X
Year of publication: 1989
Issue: 7
Pages: 18-20
Type: Article
More publications in: Geogaceta
Abstract
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.