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 …

Integration of structural, stratigraphic, and paleomagnetic data from the N–S trending
structures of the Ainsa Oblique Zone reveals the kinematics of the major thrust salient in the …

The analysis of three different regions of the South-Pyrenean fold-and-thrust belt reveals that
during the Tertiary compression the hydrological system was compartmentalised in time and …

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 …

In many deep-marine clastic systems, mass-transport complexes (MTCs) constitute a major
component of the stratigraphy and represent an integral part of the evolution 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 …

Syntectonic fluids have been sampled through fluid inclusion microthermometry and crush-
leach analyses (cations and halogens) from a 50 km NS transect through the central …

Active faults within the southern Apennines fold-and-thrust belt modulate the present-day
upwelling of hydrothermal fluids at surface. In the Monte Alpi area, we investigated the …

During compressive events, deformation in sedimentary basins is mainly accommodated by
thrust faulting and related fold growth. Thrust faults are generally rooted in the basement and …

In orogenic systems, thrust faults play a major role in stacking different tectonic units and
may act as conduits for the expulsion of large amounts of fluid of different origins …