RT Journal Article
T1 Engrosamiento de la corteza y relieve intraplacaen el centro de Iberia
A1 Vegas Martínez, Ramón
A1 Suriñach Cornet, Emma
AB 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.
PB Sociedad Geológica de España
SN 0213-683X
YR 1987
FD 1987
LK https://hdl.handle.net/20.500.14352/65262
UL https://hdl.handle.net/20.500.14352/65262
LA spa
DS Docta Complutense
RD 10 ago 2024