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 thickening — 5 km in form of 3 km of the Moho topography, 2 km of surface relief — is coherent with the surface model of intracontinental distribut...
| Autores: | , |
|---|---|
| Formato: | artículo |
| Fecha de publicación: | 1987 |
| 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:10272/18452 |
| Acesso em linha: | http://hdl.handle.net/10272/18452 |
| Access Level: | acceso abierto |
| Palavra-chave: | Crustal thickenning Intraplate uplift Central Iberian Peninsula |
| Resumo: | 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 thickening — 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 deformation already described. In addition, the present model is in agreement with the intraplate uplift, the reverse faults that bound the relief and to some extent with the intrap/ate shortening of Iberia |
|---|