Abstract
In the central Netherlands, the Rhine follows a course imposed by Late Quaternary
glaciation, forcing it to cross several tectonic blocks of the Roer Valley
Graben system before entering the south-eastern North Sea Basin. Holocene sealevel
rise resulted in the formation of a coastal prism (Holocene Rhine–Meuse
delta). Across the Peel Boundary Fault-zone (PBF)
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