La faciès Muschelkalk en la franja Mijares-Monserrat (Cordillera Ibérica Meridional, Valencia)
The stratigraphical and sedimentological study of the Muschelkalk facies (Middle Triassic) carbonated unit in Mijares-Monserrat sector, (E. Spain), allows the recognition of subunits with different characteristics. The vertical evolution of these subunits represents the transition from alternate int...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2005 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/52490 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/52490 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.7 Muschelkalk Ladinian Carbonate platforms Iberian Ranges Geología estratigráfica 2506.19 Estratigrafía |
| Sumario: | The stratigraphical and sedimentological study of the Muschelkalk facies (Middle Triassic) carbonated unit in Mijares-Monserrat sector, (E. Spain), allows the recognition of subunits with different characteristics. The vertical evolution of these subunits represents the transition from alternate inter-subtidal shallow platform environments to inter-supratidal environments. Presence of the bivalves Leptochondria alberti, Bakevellia costata, Entolium discites and "Placunopsis"and the foraminifers Lamelliconus ex gr. ventroplanus-biconvexus, L. multispirus, L. procerus and Triado- discus eomesozoicus indicate a Ladinian-Carnian age in a broad sense. These general characteristics are common of the so- called "Mediterranean Triassic type" and particularly to the upper part of the carbonate unit of the Muschelkalk facies. |
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