Estructura y evolución del borde sur-occidental de la Fosa de Calatayud-Daroca
The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloca fault. The evolution of the Basin during the Miocene, was conditioned by dextral slip on this fault. During the Pliocene the Jiloca fault had a normal slip, resulting in the Jiloca Basin formation
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1988 |
| 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:10272/18395 |
| Acceso en línea: | http://hdl.handle.net/10272/18395 |
| Access Level: | acceso abierto |
| Palabra clave: | Thrust Strike-slip Neogene Calatayud-Daroca Basin |
| Sumario: | The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloca fault. The evolution of the Basin during the Miocene, was conditioned by dextral slip on this fault. During the Pliocene the Jiloca fault had a normal slip, resulting in the Jiloca Basin formation |
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