Engrosamiento de la corteza y relieve intraplaca en el centro de Iberia
A moderate thickening of the crust beneath the Spanish Central System has been determined by means of a wide angle seismic experiment. The value of this thickeníng - 5 km in form of 3 km of the Moho topography, 2 km of surface relief is coherent with the surface model of intracontinental distributed...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1987 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/65262 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/65262 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.24(234.1) Crustal thickenníng Intraplate uplift Central Iberian Península Geodinámica 2507 Geofísica |
| Sumario: | A moderate thickening of the crust beneath the Spanish Central System has been determined by means of a wide angle seismic experiment. The value of this thickeníng - 5 km in form of 3 km of the Moho topography, 2 km of surface relief is coherent with the surface model of intracontinental distributed deformatíon already descríbed. In addition, the present model is in agreement with the intraplate uplíft, the reverse faults that bound the relief and to sorne extent with the intraplate shortening of Iberia. |
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