Reconocimiento del Cenomaniense medio y superior en el Prebético de Murcia: los rudistas de la Sierra del Cuchillo
Rudists remains found in secondary do/ostones 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 w...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1990 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/120506 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/120506 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.7 Cenomanian Turonian Prebetic area Rudists Geología estratigráfica 2506.19 Estratigrafía |
| Sumario: | Rudists remains found in secondary do/ostones 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 paleosols. |
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