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- W2060332607 abstract "Sedimentation in the Shepherd's Chine Member of the Vectis Formation is characterised by a cyclicity of four principal facies on which a strong asymmetry has been imprinted by erosional events. The four lithofacies are: (1) very fine to fine sandstones; (2) heterolithic sand/silt and mudstones; (3) parallel-laminated (pinstripe) mudstones; and (4) black mudstones. The biota, principally associated with lithofacies 2 and 3 (as shelly partings and coquinas), can be grouped into five molluscan associations which range from freshwater to quasi-marine. These associations are poorly correlated with the lithofacies, but fluctuate within and between cycles. Salinity and storm frequency increase towards the top of the formation, heralding the main marine Aptian transgression. Lithofacies and biotas indicate deposition in a lagoon that was shallow and temporarily emergent. The cyclicity is thought to represent the more distal phases of the advance and retreat of deltaic sand bodies, derived from a westerly direction, into the lagoon. Major storm events broke the symmetry of the cycles. A deltaic facies, represented by the Barnes High Sandstone Member, is thought to be laterally linked, reworked deltaic sandstone lobes." @default.
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- W2060332607 date "1991-06-01" @default.
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- W2060332607 title "Lagoonal sedimentation and fluctuating salinities in the Vectis Formation (Wealden Group, Lower Cretaceous) of the Isle of Wight, southern England" @default.
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- W2060332607 doi "https://doi.org/10.1016/0037-0738(91)90126-x" @default.
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