Abstract During the Paleogene and Neogene the NE Iberian plate underwent significant
paleogeographic changes driven by the Iberian and European plate collision and the …

This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …

Construction of a crustal balanced cross-section across the Pyrenean chain shows a
minimum shortening of 147 km, 112 km of which are related to stacking of basement thrust …

Estimating shortening in collision belts is critical to reconstruct past plate motions. Balanced
cross‐section techniques are efficient in external domains but lack resolution in the …

Geodynamical numerical modeling has been combined with crustal structural restoration of
the central Pyrenees in order to gain insight into fundamental processes that control the …

The geometry and the infill of the south Pyrenean foreland basin mainly depend on the
tectonic subsidence history due to the flexure of the crust, which in turn can be related to the …

A new crustal-scale cross-section through the Eastern Pyrenees shows a minimum of 125
km of total shortening across the belt. Convergence rates of 6 mm/yr (during early and …

The Pyrenees are a collisional mountain belt formed by convergence between the Afro–
Iberian and European plates. Apatite fission track thermochronology from three vertical …

An analysis of the Upper Jurassic–Lower Cretaceous Morrison and Cedar Mountain
Formations of Utah and Colorado has resulted in a general sequence-stratigraphic model …

Well‐preserved, actively deforming folds in the Tien Shan of Kyrgyzstan provide a natural
laboratory for the study of the evolution of thrust‐related folds. The uplifted limbs of these …