We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …

Orogenic forelands host interactions between deformation and static or migrating fluids.
Given their accessibility and dimensions, these areas are not only historic landmarks for …

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 …

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 …

It is difficult to quantify the timing of the deformation processes in brittle fold–thrust belts
because minerals suitable for dating and well-preserved growth strata sediments are scarce …

Fluid systems in inverted rifted margins are challenging to interpret because fractures
formed before compression were often reactivated acting as fluid pathways as new ones …

In the Western Alps, the Penninic Frontal Thrust (PFT) is the main crustal-scale tectonic
structure of the belt. This thrust transported the high-pressure metamorphosed internal units …

As one of the predominant diagenetic products in clastic rocks, calcite cements are typical
fingerprints of cement‐forming fluids and are key controls on reservoir quality. The Puig‐reig …

Sedimentary rocks of foreland fold-and-thrust belts typically undergo intensive fracturing as
folds grow. The resulting fracture networks can present significant variations depending on …