High-resolution continuous core material, geophysical measurements, and hundreds of
archived core descriptions enabled to identify 13 Late Pleistocene Rhine-Meuse …

An almost 50-m-deep core from the Weichselian Rhine–Meuse palaeovalley, near the
present Dutch coast, reveals new insights into how this continental-scale fluvial system …

Eight continuous corings in the west-central Netherlands show a 15 to 25 m thick stacked
sequence of sandy to gravelly channel-belt deposits of the Rhine-Meuse system. This …

Fluvial longitudinal profiles reconstructed from abandoned floodplains contain significant
evidence about the role of relative sea level vs. climatic and tectonic controls on depositional …

A new reconstruction of the interaction between the Saalian Drente glaciation ice margin
and the Rhine–Meuse fluvial system is presented based on a sedimentary analysis of …

This study presents a detailed reconstruction of the palaeogeography of the Rhine valley
(western Netherlands) during the Holocene transgression with systems tracts placed in a …

A chronostratigraphic framework has been established for Upper Neogene sediments from
the northern Netherlands offshore sector, southern North Sea. Data of dinoflagellate cysts …

Around 10 million years ago, the interplay of tectonics, climate and sea level changed
markedly in the southern North Sea Basin. One of the results was the start of rapid …

The landscape evolution of the southern North Sea basin is complex and has left a
geographically varying record of marine, lacustrine, fluvial and glacial sedimentation and …

A large number of lithological borehole descriptions, 14C dates, archaeological artefacts,
and gradients of palaeochannels were used to reconstruct the Holocene development of the …