Estructuras de acortamiento lateral en el frente del cabalgamiento varisco de Espiel, Córdoba (Zona Centroibérica meridional)
In the southern part of the Central Iberian Zone (Iberian Massif), a Lower Carboniferous thrust superposed to the NE an allochthonous unit onto a paraautochthonous one. In the Espiel area, the thrust geometry includes several frontal horses. Furthermore, lateral confining of the nappe during transpo...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2000 |
| 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:10272/9783 |
| Acceso en línea: | http://hdl.handle.net/10272/9783 |
| Access Level: | acceso abierto |
| Palabra clave: | Thrust geometry Lateral imbrication Southern Central Iberian Zone Variscan Belt |
| Sumario: | In the southern part of the Central Iberian Zone (Iberian Massif), a Lower Carboniferous thrust superposed to the NE an allochthonous unit onto a paraautochthonous one. In the Espiel area, the thrust geometry includes several frontal horses. Furthermore, lateral confining of the nappe during transport produced a lateral hanging wall slice that branches out from the main thrust in the location of a lateral hanging wall ramp |
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