In the interior of the Iberian Peninsula, the main geomorphic features, mountain ranges and
basins, seems to be arranged in several directions whose origin can be related to the N–S …

The Variscan deformation in the Iberian Massif is related to the large-scale plate tectonic
scenario that drove to the destruction of the Rheic and other intervening oceans, to finally …

Hydrothermal quartz–apatite veins, called “Iberian-type”, occur exclusively in the southern
Central Iberian Zone. This study presents a multidisciplinary approach leading to the …

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 …

Abstract Marianian (Cambrian Series 2) trilobites from the area between Totanés and Noez
(Central Iberian Zone) are described and their biostratigraphical significance is discussed …

Apatite fission track (AFT) and (U–Th)/He data from the High Atlas have been obtained for
the first time to constrain the tectono‐thermal evolution of the central part of the chain …

Inferences from analogue models support lithospheric folding as the primary response to
large‐scale shortening manifested in the present day topography of Iberia. This process was …

The lateral termination of the Alpine-Pyrenean Orogen relief onshore is located in the NW
Iberian Peninsula. It overlies a Variscan basement (Iberian Massif), where the sedimentary …

The Catalan Coastal Ranges (CCR) form part of the northeastern Iberian Mediterranean
margin. This margin typifies the transition zone between the thickened crust of the Pyrenees …

This paper presents the results of a study concerning the total and extractable
concentrations of eight elements (As, Cd, Cr, Cu, Ni, Pb, Se and Zn) in soils and sediments …