@article{10272/8401,
year = {2007},
url = {http://hdl.handle.net/10272/8401},
abstract = {The Cenozoic deformation of the Iberian lithosphere along a NW-SE profile from the northern Duero Basin
to the southern Tajo Basin, crossing Spanish Central System, has been analysed by means of a numerical
simulation based in the finite element method. Lateral and vertical rheological heterogeneities, Tertiary
sedimentary overburden and the Alpine compressional tectonic stresses have been considered. Numerical
results support a mechanism of lithospheric folding for the development of the chain and basins and a
thicker lower crust below the central part of Iberia},
title = {Deformación cenozoica de la litosfera Ibérica: Sistema Central y cuencas del Duero y Tajo},
title = {Cenozoic deformation of the Iberian lithosphere: Spanish Central System and Duero and Tajo Basins},
author = {Martín Velázquez, Silvia and Elorza, F. J.},
}