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
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1989

Zenbakia: 7

Orrialdeak: 76-78

Mota: Artikulua

Beste argitalpen batzuk: Geogaceta

Laburpena

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