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- W2249100044 abstract "This paper aims at a better understanding of the mechanisms and sedimentological processes that caused the lithological variations in the Late Holocene deposits of the Belgian coastal lowlands. According to the traditional Belgian literature these deposits overlying the surface peat are the result of the Dunkirk transgressions. This transgression model with a fluctuating sea level is also used in northern Germany. However, a critical review of the index points used to construct the sea-level curve showed that they can not be considered as reliable. Since the sea-level curves of the Southern North Sea lowlands do not show sea-level fluctuations for the past 2500 years, the sedimentary characteristics and chronology of the post-peat deposits have been investigated in detail in shallow outcrops with special attention to the final infill of tidal channels. The results show that the sedimentation was discontinuous and changes happened rapidly. Frequent reworking of the final fill of the channels have been documented on the basis of age determination of shells and the consideration of the position of the shells in a broader stratigraphic context. It is suggested that the main controls on the sedimentation was the availability of sediment and the change in size of the tidal prism of the channels due to the compaction of the peat with consequently an increase of accommodation space." @default.
- W2249100044 created "2016-06-24" @default.
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- W2249100044 date "2007-01-01" @default.
- W2249100044 modified "2023-09-27" @default.
- W2249100044 title "De laat Holocene evolutie van de Belgische kustvlakte: sedimentatieprocessen versus zeespiegelschommelingen en Duinkerke transgressies" @default.
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