Correlation of the Hythe Beds Formation (Lower Greensand Group: early-mid-Aptian), southern England

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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.

Original languageEnglish
Pages (from-to)273-291
JournalProceedings of the Geologists' Association
Volume103
Issue number4
DOIs
Publication statusPublished - 02 Sept 1992

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