Tectónica alpina y morfogénesis en el Sistema Central español: Modelo de deformación intracontinental distribuida
The formation of the Spanish Central System is a adscribed to an intracontinental shear zone whose activity implies rotation of blocks within areas of intense deformation. This model of distributed deformation explains the fragmented shape of the relief and can be referred to the intraplate deformat...
| Autores: | , , |
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| Tipo de documento: | artigo |
| Data de publicação: | 1996 |
| 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:10272/18506 |
| Acesso em linha: | http://hdl.handle.net/10272/18506 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Distributed deformation Intracontinental shear Sistema Central |
| Resumo: | The formation of the Spanish Central System is a adscribed to an intracontinental shear zone whose activity implies rotation of blocks within areas of intense deformation. This model of distributed deformation explains the fragmented shape of the relief and can be referred to the intraplate deformation of Iberia |
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