Deformaciones plio-cuaternarias en la region de Rabat
The Rabat region, located in the northern border of the Moroccan Meseta, is generally considered as a present-day stable region. However, the fluvial and marine sedimentary rocks, with Pliocene and Quaternary ages, are deformed by joints, generally tensional, and by normal and strike-slip faults. Th...
| Autores: | , , , , , , |
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| Tipo de documento: | artigo |
| Data de publicação: | 2000 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositório: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | espanhol |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9765 |
| Acesso em linha: | http://hdl.handle.net/10272/9765 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Moroccan Meseta Rabat Recent tectonics Brittle deformations |
| Resumo: | The Rabat region, located in the northern border of the Moroccan Meseta, is generally considered as a present-day stable region. However, the fluvial and marine sedimentary rocks, with Pliocene and Quaternary ages, are deformed by joints, generally tensional, and by normal and strike-slip faults. The brittle structures indicate N-S compressional deformations, probably related to the present-day regional stresses in the crust, and extensional deformations related to the proximity to the Gharb basin |
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