The occurrence of endorheic basins on the Tibetan Plateau, both in its Pleistocene history
and (fewer in number) at the present day, has been attributed to the 'basin-and …

The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly
present, but not only, in areas affected by the Alpine Orogeny. They are located in several …

The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and
deformation belts with a wide variety of structural trends. The Spanish‐Portuguese Central …

The purpose of this paper is to analyze the quasi-elastic deformational behavior that has
been induced by groundwater withdrawal of the Tertiary detrital aquifer of Madrid (Spain) …

Large‐scale faults in the continental crust are significant features that control the evolution of
sedimentary basins and intraplate mountain chains. Deciphering their evolution is a …

A NS crustal transect of the whole Iberian Plate is presented. The displacement transfer
during the Alpine deformation from the border ranges (Cantabrian and Betic chains) toward …

Abstract The northern Madrid Basin contains paleosols and lacustrine sequences composed
of ordered dolomite. Smectite-rich mudstones with analcime deposited in distal alluvial fans …

The SW of Iberia is currently undergoing compression related to the convergence between
Nubia and Iberia. Multiple compressive structures, and their related seismic activity, have …

In this work, three important Pleistocene sites of the Madrid basin located close to the
junction of the Manzanares (PRERESA site) and the Jarama (Valdocarros site and Maresa …

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