Abstract
The outcrop and sub-surface stratigraphy of the Hythe Beds Formation shows a coarsening-up cyclicity in the arenaceous successions of the western Weald Basin (Hants. & Surrey), and in the glauconitic/argillaceous deposits of Sussex/Kent. Correlation can be achieved through the identification of hiatus surfaces, the most distinctive of which are dark, smectite-enriched clays with belemnites and phosphate nodule beds. These beds are interpreted to be the product of transgressive conditions. Correlation may be difficult in clastic shelf successions: the use of distinctive transgressive event beds provides a model for other successions displaying similar facies.
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