Las facies terrígenas del Muschelkalk basal en el extremo noroccidental de la Cordillera Ibérica
Clastic Materials of basal Muschelkafk in the northestern edge of lberian Ranges represent subtidaf environments and even high energy events in the inner platform (presence of H.C.S.). Such events disturb the ínter and supratidal sedimentation development of both under and overlaying units.
| 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:20.500.14352/111267 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/111267 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.7(460) Muschelkalk Iberian Ranges Tidal environment Geología estratigráfica 2506.19 Estratigrafía |
| Sumario: | Clastic Materials of basal Muschelkafk in the northestern edge of lberian Ranges represent subtidaf environments and even high energy events in the inner platform (presence of H.C.S.). Such events disturb the ínter and supratidal sedimentation development of both under and overlaying units. |
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