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: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 1986 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/65256 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/65256 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.2(234.1) Distributed deformation Intracontinental shear Sistema Central Geodinámica 2507 Geofísica |
| Sumario: | 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. |
|---|