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...

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Main Authors: Ruffell, A, Hesselbo, S, Wach, G, Simpson, M, Wray, D
Format: Journal article
Language:English
Published: 2002
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author Ruffell, A
Hesselbo, S
Wach, G
Simpson, M
Wray, D
author_facet Ruffell, A
Hesselbo, S
Wach, G
Simpson, M
Wray, D
author_sort Ruffell, A
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:1b7c1200-1a5f-46f4-8338-f59ac4cb1a4c2022-03-26T11:00:40ZFuller'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:1b7c1200-1a5f-46f4-8338-f59ac4cb1a4cEnglishSymplectic Elements at Oxford2002Ruffell, AHesselbo, SWach, GSimpson, MWray, DA <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 Ruffell, A
Hesselbo, S
Wach, G
Simpson, M
Wray, D
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
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AT hesselbos fullersearthbentoniteinthelowercretaceousupperaptianofshanklinisleofwightsouthernengland
AT wachg fullersearthbentoniteinthelowercretaceousupperaptianofshanklinisleofwightsouthernengland
AT simpsonm fullersearthbentoniteinthelowercretaceousupperaptianofshanklinisleofwightsouthernengland
AT wrayd fullersearthbentoniteinthelowercretaceousupperaptianofshanklinisleofwightsouthernengland