Differential subsidence within a coastal prism: late-glacial-holocene tectonics in the Rhine-Meuse delta, the Netherlands [Proefschrift]
Cohen, K.M. \ 2003
The Rhine-Meuse river system has been studied extensively over the past few decades. The Netherlands' coastal prism formed in response to Holocene sea level rise and buried the Weichselian (OIS-2) Rhine-Meuse valley. Although the geological-geomorpho ...
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