R. Gras 1995. The Late Cretaceous in northwest Europe is characterised by general sealevel rise, leading to extensive platform carbonate sedimentation of the Chalk Group, and by tectonic inversion, as witnessed by uplift and erosion of the Late Jurassic to Early Cretac. Netherlands Journal of Geosciences. 74, (Jan. 1995), 117-127. DOI:https://doi.org/10.70712/njg.v74.12410.