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 …

The kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …

Stringers represent fragments of competent, brittle layers, formerly interstratified within a
layered evaporite sequence (LES) that are entrained and deformed by viscous flow. To …

This study integrates field structural data, petrographic and geochemical (δ 18 O, δ 13 C, Δ
47, 87 Sr/86 Sr, and elemental composition) analyses and U–Pb dating of calcite veins …

Analog modeling is used to study the role played by the inherited salt‐sediment architecture
of a salt‐bearing rifted margin, developed by minibasin downbuilding and margin‐scale …

This paper contributes to an understanding of the tectono‐sedimentary evolution of the
South Pyrenean foreland system by reviewing the chronostratigraphic framework of the …

The Pyrenees is a collisional orogen built by inversion of an immature rift system during
convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The …

Abstract The Oliana anticline (Southern Pyrenees) has been characterized as an outcrop
analogue of a geothermal reservoir using field data (stratigraphy and fracturing) and …

Inspired by the structural evolution of the South-Central Pyrenean Thrust Salient we have
designed an experimental program to investigate the role of the geometry of viscous …