Palaeohydrogeology using geochemical, isotopic and mineralogical analyses: Salinity and redox evolution in a deep groundwater system through Quaternary glacial cycles

Mineralogical and geochemical studies add further information to the understanding of past geochemical conditions in deep groundwaters in this area. Interpretations provide semi-quantitative constraints on the evolution and likely variations and directions of movement of groundwater salinity and redox over the Quaternary timescale.