The Iberian microcontinent stands out because of its intense Alpine intraplate deformation.
This is reflected in a large number of Cenozoic basins of very different sizes. Most of the …

The evolution of the Pyrenees, a mountain range between Iberia and Eurasia, has remained
the subject of many debates between geologists and geophysicists for a long time. By …

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 …

This work characterizes for the first time the 500–700 m-thick uppermost Cretaceous
continental sedimentary succession of the Allueva Fm recorded in the northeastern margin …

Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …

The Iberian Chain is a wide intraplate deformation zone formed by the tectonic inversion
during the Pyrenean orogeny of a Permian–Mesozoic basin developed in the eastern part of …

The mechanisms responsible for the formation of huge volumes of dolomitized rocks
associated with faults are not well understood. We present a case study for high-temperature …

Constraining the way in which continental deformation is accommodated in time and space
is essential to reconcile past plate movements with geological observations. Kinematic …

The stress evolution of the central-eastern Iberian Chain during the Tertiary compression
has been a matter of discussion during the last decades. In particular, there is not a …

The interaction between aeolian dunes of the Iberian erg and Tethys waters during the mid‐
Cretaceous led to a variety of sedimentary facies associations such as subtidal deposits …