Philip, J.Martín Chivelet, Javier2020-06-112020-06-111989http://hdl.handle.net/10272/18260Rudists remains found in secondary dolostones or very recrystalized limestones permits, by once, to date platform 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 paleosolsRestos rudistas encontrados en dolomías secundarias o calizas muy recristalizadas permiten datar series de plataformas carbonatadas del Alto Cenomaniense en el área Prebética. No se ha demostrado la presencia de Turonenses, pero, si existiera, se debería limitar a algunos metros de margas dolomíticas con paleosuelos.spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/CenomanianTuronianPrebetic areaRudistsjournal articleopen access