Diaclasas de tensión regionales en el Complejo Nevado-FiIábride y su relación con el contacto Alpujárride/Nevado-FiIábride (Sierra Nevada, Cordilleras Béticas)
Nevado-Filábride rocks have been strained by a NW-SE principal set of systematic tension joints. The orientation of the least principal stress derived from the NevadoFilábride/Alpujárride contact fault gouge agree with the one obtained from joint analysis
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1989 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18238 |
| Acesso em linha: | http://hdl.handle.net/10272/18238 |
| Access Level: | acceso abierto |
| Palavra-chave: | Joints Extensional tectonic Betic Cordillera |
| Resumo: | Nevado-Filábride rocks have been strained by a NW-SE principal set of systematic tension joints. The orientation of the least principal stress derived from the NevadoFilábride/Alpujárride contact fault gouge agree with the one obtained from joint analysis |
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