Neotectónica en el antepaís castellano de las cordilleras Béticas orientales
The major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crust...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| 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:10272/12661 |
| Acceso en línea: | http://hdl.handle.net/10272/12661 |
| Access Level: | acceso abierto |
| Palabra clave: | Stress configuration Morphotectonics Crustal flexures Intraplate accommodation Eastern Betics foreland |
| Sumario: | The major morphotectonic features in the foreland of the Eastern Betics can be explained within the frame of the weak compressive stress field originated in the Prebetic fold and thrust belt. This NW directed compression is partitioned by N130°-150° dextral strike-slip corridors and orthogonal crustal flexures. The Neogene-Quaternary volcanism and the distribution of seismicity can be also considered within this compressive neotectonic regimen |
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