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Modern deposits, quasi-deposits and some Holocene sequences in the Southern Bight, North Sea in The Quaternary and Tertiary geology of the Southern Bight, North Sea.

The varied types of modern deposit of the present-day Southern Bight are used as a partial guide for a review of the diachronous deposits of the Holocene marine transgression. The flooding of the barrier separating the Southern Bight from the North

Dynamics of gravel in the superficial sediments of the Flemish Banks, southern North Sea in The Quaternary and Tertiary geology of the Southern Bight, North Sea.

Although it is obvious that the gravels in the Flemish Banks consist of three main deposits, it is very hard to stake them out. Due to the Holocene marine transgressions the gravels are becoming a mixture of southern coming, Rhine and Meuse

Upper Pliocene and Lower Pleistocene stratigraphy in the Southern Bight of the North Sea in The Quaternary and Tertiary geology of the Southern Bight, North Sea.

on seismic profiles, defining the boundaries between six separate seismostratigraphic units with characteristic lithology, seismic facies and fossil assemblages. The total succession describes a history of repeated and widespread marine transgression

Middle and Upper pleistocene and Holocene stratigraphy in the southern North Sea between 52o and 54o N, 2o to 4o E in The Quaternary and Tertiary geology of the Southern Bight, North Sea.

, where up to 15 m of till was deposited during late Weichselian times. Marine sands and clays were deposited in the southern North Sea during the Holsteinian and Eemian interglacial periods. The sediments of the Holocene transgression have been subdivided