Las Calizas de Oko: un humedal fluvial a palustre-lacustre carbonático del Mioceno tardío-Plioceno encajado en el Frente Cabalgante Surpirenaico (Navarra, España)
This work presents the sedimentological study of the Upper Miocene-Pliocene Oko Limestones, exposed in the Antzin-Murieta Basin, in Navarre. Two stratigraphic sections of the carbonate unit have been studied: the Oko cemetery and Ega road sections. The former exposes facies that characterize a fluvi...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2023 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | inglés |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/23854 |
| Acceso en línea: | https://hdl.handle.net/10272/23854 |
| Access Level: | acceso abierto |
| Palabra clave: | South-Pyrenean Thrust Front Oko Limestones Upper Miocene-Pliocene Fluvial to palustrine-lacustrine environments Ambientes fluviales a palustres-lacustres Frente Cabalgante Surpirenaico Calizas de Oko Mioceno Superior-Plioceno |
| Sumario: | This work presents the sedimentological study of the Upper Miocene-Pliocene Oko Limestones, exposed in the Antzin-Murieta Basin, in Navarre. Two stratigraphic sections of the carbonate unit have been studied: the Oko cemetery and Ega road sections. The former exposes facies that characterize a fluvial carbonate environment, with a distinct development of microbial oncolitic deposits. The coeval deposits exposed in the Ega road section, instead, largely represent a palustrine-lacustrine setting that evolved under alternating conditions of ponding and desiccation. Data integration from these sections and the intermediate areas, allows the interpretation of a fluvial to palustrine-lacustrine wetland with a marked east-southeast trend, which developed coevally to the uplift of the Piedramillera thrust sheet |
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