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- W1567309671 abstract "Fluvial successions of Devensian age are described from exposures within river terraces of drainage basins south of the glacial ice limit. Examples are presented from the Bain Valley of Lincolnshire and the Thames Valley. Reconstructions using sedimentological, geomorphological and biostratigraphical evidence indicate that deposition occurred in a permafrost environment. Primary sedimentary structures indicate deposition by rivers of the Scott–and possibly Donjek–type of Miall (1977). The sequence of facies changes suggest a near-continuous aggradation of the sediments with periodic exposure to sub-aerial conditions. During exposure ice wedges developed within the sediments. Subsequent channel migration appears to have been associated with talik extension (permafrost degradation) leading to the decay of the ice wedge ice and subsequent casting. The resultant planar erosion surfaces which truncate ice wedge casts are taken as evidence for the former existence of higher topographic levels of floodplain sediments during the aggradation of the sediment body. These surfaces truncate complete fluvial cycles with a resultant preferential preservation of bar platform sediments." @default.
- W1567309671 created "2016-06-24" @default.
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- W1567309671 date "1983-02-07" @default.
- W1567309671 modified "2023-09-23" @default.
- W1567309671 title "Facies Sequences Associated with Some Braided River Deposits of Late Pleistocene Age from Southern Britain" @default.
- W1567309671 doi "https://doi.org/10.1002/9781444303773.ch21" @default.
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