Publication | Closed Access

Fluid evolution during burial and Variscan deformation in the Lower Devonian rocks of the High-Ardenne slate belt (Belgium): sources and causes of high-salinity and C–O–H–N fluids

Fluid EvolutionEngineeringHigh-ardenne Slate BeltSedimentary GeologyVariscan DeformationGeologySedimentary PetrologyGeochronologyPetrologyIgneous PetrologyEarth ScienceRock PropertiesTectonics