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 …

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 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 …

This work aims to present the Les Avellanes diapir as a field analog to inquire how the
origin, advance, and emplacement of an allochthonous salt body in continental settings …

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 …

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

Reinterpretation of the Organyà Basin, based on new detailed field observations and
subsurface data, emphasizes the key contribution of Upper Triassic evaporites in the tectono …