El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica
The Muel-Jaulin region shows structures related to the Lower Cretaceous extension and the Tertiary compression respectively. Cretaceous normal faults constitute the northern border of the Aguilôn Cretaceous basin, appearing Lower Cretaceous deposits (Villanueva de Huerva Fm.) to the South. During th...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1997 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/10540 |
| Acceso en línea: | http://hdl.handle.net/10272/10540 |
| Access Level: | acceso abierto |
| Palabra clave: | Normal fault Fold Thrust Inversion tectonics Cretaceous Tertiary |
| Sumario: | The Muel-Jaulin region shows structures related to the Lower Cretaceous extension and the Tertiary compression respectively. Cretaceous normal faults constitute the northern border of the Aguilôn Cretaceous basin, appearing Lower Cretaceous deposits (Villanueva de Huerva Fm.) to the South. During the Tertiary compression, minor normal faults were reactivated and folded. Main faults limiting the Cretaceous basin are slightly reactivated and they are responsible for the nucléation of the Muel-Jaulin anticline |
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