文摘
The Bajocian-Bathonian aquifier in the Caen region is largely exploited for drinking water and agriculture. When this coastal carbonated aquifer becomes confined, groundwater presents an increasing TDS both vertically and along the flow path. This is explained by water-carbonate interaction and by a mixing with marine water (up to 4 % ). Radiocarbon dating, after correction of the initial activity according to different models, shows a wide range of groundwater ages, from 40 000 years B.P. to the present. The marine transgression has thus been estimated as having occurred during the Early Holocene period.