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High Resolution Stratigraphy and Peleoenvironmental Changes in The Southern North Sea during The Neogene
Today's continental shelves, such as the one covered by the North Sea, are products of the last post-glacial sea-level rise of the glacial era that began in the Late Pliocene and continued until today. The sedimentary history of shelf seas reflects the changing relationship between tectonic subsidence, sea level oscillations and (hydro-) dynamics processes.
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