The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …

Since the late nineteenth century, the Guadarrama mountain range (listed as a National
Park in 2013) has attracted the attention of intellectuals, naturalists and mountaineers, for …

The Spanish Central System is a Cenozoic pop-up with an E–W to NE–SW orientation that
affects all the crust (thick-skinned tectonics). It shows antiform geometry in the upper crust …

A brittle deformation tectonic analysis was performed in central Spain (Spanish Central
System and Madrid Basin) in order to decipher and understand the deformation processes …

Shallow and deep sources generate a gravity low in the central Iberian Peninsula. Long-
wavelength shallow sources are two continental sedimentary basins, the Duero and the Tajo …

Late Cenozoic landscape evolution in intracratonic basins represents an illustrative example
of the interaction between surface processes, climate, lithologic and tectonics factors. Here …

Data from deep boreholes, seismic surveys, and surface geology are used to reconstruct the
sedimentary infilling of the Cenozoic Madrid Basin. Eight main depositional sequences and …

Three subsequent Tertiary paleostress fields that are deduced from fault-slip data for the
eastern part of the Tajo Basin are analyzed by finite-element studies. The modelling results …

The spatial distribution of faults is usually described as a fractal set characterised by the
fractal dimension. In this work, we have filtered fault patterns interpreted from digital …

The landscape of today's central Iberian Peninsula has been shaped by ongoing tectonic
activity since the Tertiary. This landscape comprises a mountain ridge trending E–W to NW …