Paleoesfuerzos alpinos en el borde suroccidental de la cuenca de Madrid (Montes de Toledo)
The paleostress analysis are used here to outline the Alpine deformation of the contact between the Toledo Mountains and the Madrid Basin. This limit results from a system of E-W-trending reverse faults, NW-SE-trending dextral normal strike-slip faults and NNE-SSW-trending sinistral normal strike-sl...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1995 |
| 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:10272/13549 |
| Acceso en línea: | http://hdl.handle.net/10272/13549 |
| Access Level: | acceso abierto |
| Palabra clave: | Faults population analysis, Paleostress analysis Cuenca de Madrid. |
| Sumario: | The paleostress analysis are used here to outline the Alpine deformation of the contact between the Toledo Mountains and the Madrid Basin. This limit results from a system of E-W-trending reverse faults, NW-SE-trending dextral normal strike-slip faults and NNE-SSW-trending sinistral normal strike-slip faults |
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