Reconocimiento del Cenomaniense medio y superior en el Prebético de Murcia:los rudistas de la Sierra del Cuchillo

  1. J. Philip 1
  2. J. Martín-Chivelet 2
  1. 1 Centre de .Sédimentologie-Paléontologie. C.N.R.S., Univ. de Provence. France
  2. 2 Instituto de Geología Económica, C.S.J.C.-U.C.M., Opto. de Estratigrafía, Facultad CC. Geológicas
Zeitschrift:
Geogaceta

ISSN: 0213-683X

Datum der Publikation: 1989

Nummer: 7

Seiten: 76-78

Art: Artikel

Andere Publikationen in: Geogaceta

Zusammenfassung

Rudists remains found in secondary dolostones or very recrystalized limestones permits, by once, to date plat form carbonate series of Upper Cenomanian age in the Prebetic area. The presence of Turonian has not been proved, but, if it exists, it should be restricted to few meters of dolomitic marls with paleosols