Fósiles ordovícicos del NO de Adamuz (Córdoba): aportación paleobiogeográfica a la concepción del limite entre las Zonas Centroibérica y Ossa Morena durante el Paleozoico
The Ordovician outcrop at NW Adamuz (Cordoba province), previously regarded as belonging to in the Ossa Morena Zone by some authors, contains several fossiliferous levels of Lower Llanvirn, Upper Llanvirn-Llandeilo and Caradoc (pre-Actonian) age. The Central Iberian affinities of the faunas constitu...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1987 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/65257 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/65257 |
| Access Level: | acceso abierto |
| Palabra clave: | 565.393 Ordovician Hesperian Massif trilobites Ossa Morena Zone Central-Iberian Zone Structural boundary Paleontología 2416 Paleontología |
| Sumario: | The Ordovician outcrop at NW Adamuz (Cordoba province), previously regarded as belonging to in the Ossa Morena Zone by some authors, contains several fossiliferous levels of Lower Llanvirn, Upper Llanvirn-Llandeilo and Caradoc (pre-Actonian) age. The Central Iberian affinities of the faunas constitute an additional argument for the consideration of the Obejo-Valsequillo-Puebla de la Reina Domain as the southern margin of the Central Iberian Zone during the Paleozoic. |
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