Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)

A 35 cm fuller's earth (bentonite) bed is recorded from the Upper Aptian (Lower Cretaceous) Ferruginous Sands Formation (Lower Greensand Group), southwest of Shanklin, Isle of Wight. The stratigraphic location and sedimentological context of the bed are described: the host succession is cyclica...

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Format: Journal article
Published: Geological Society Publishing House 2002
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collection OXFORD
description A 35 cm fuller's earth (bentonite) bed is recorded from the Upper Aptian (Lower Cretaceous) Ferruginous Sands Formation (Lower Greensand Group), southwest of Shanklin, Isle of Wight. The stratigraphic location and sedimentological context of the bed are described: the host succession is cyclical, containing evidence of non-deposition, faunal colonization and current reworking of sediments. Mineralogical and petrographic analyses demonstrate the dominance of smectite (Ca-montmorillonite) and the presence of feldspar shards in the fuller's earth bed. Geochemical data indicate a close similarity to the fuller's earth beds formerly exposed at Redhill(Surrey), for which an intra-plate, trachytic volcanic source is suggested. The sedimentological, stratigraphic and volcanic implications of the discovery are discussed.
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spelling oxford-uuid:588580ab-2d68-418b-8917-a6563b971d602022-03-26T17:03:58ZFuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:588580ab-2d68-418b-8917-a6563b971d60Earth sciencesGeographyOxford University Research Archive - ValetGeological Society Publishing House2002A 35 cm fuller's earth (bentonite) bed is recorded from the Upper Aptian (Lower Cretaceous) Ferruginous Sands Formation (Lower Greensand Group), southwest of Shanklin, Isle of Wight. The stratigraphic location and sedimentological context of the bed are described: the host succession is cyclical, containing evidence of non-deposition, faunal colonization and current reworking of sediments. Mineralogical and petrographic analyses demonstrate the dominance of smectite (Ca-montmorillonite) and the presence of feldspar shards in the fuller's earth bed. Geochemical data indicate a close similarity to the fuller's earth beds formerly exposed at Redhill(Surrey), for which an intra-plate, trachytic volcanic source is suggested. The sedimentological, stratigraphic and volcanic implications of the discovery are discussed.
spellingShingle Earth sciences
Geography
Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title_full Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title_fullStr Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title_full_unstemmed Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title_short Fuller's earth (bentonite) in the Lower Cretaceous (Upper Aptian) of Shanklin (Isle of Wight, southern England)
title_sort fuller s earth bentonite in the lower cretaceous upper aptian of shanklin isle of wight southern england
topic Earth sciences
Geography