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 …

The evolution of the Apennine wedge has seen the time‐space migration of the forebulge,
foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward …

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

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 …

We report the results of a multiproxy study that combines structural analysis of a fracture–
stylolite network and isotopic characterization of calcite vein cements and/or fault coating …

Bedding-parallel calcite veins (BPCVs) occur widely in Upper Cretaceous lacustrine shales
of the Qingshankou Formation in the Northern Songliao Basin, China. Research on the …

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 …

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 …