Resumen de Engrosamiento de la ·corteza y relieve intraplaca en el centro de Iberia 40
Ramón Vegas Martínez, Emma Suriñach Cornet
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 sorne extent with the intraplate shortening of Iberia.
