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- W2085367634 abstract "A study of clay mineralogy, particle size distribution and morphology of chalky rubble with overlying sediments, indicates the complex and polycyclic nature of the development of a highly irregular weathering interface. The results show a cold period disturbance of the Chalk, followed by the development of a deposit similar to Clay-with-Flints sensu lato . This was later covered by gravels, from which time solution of the underlying chalk has continued, to produce the irregular weathering front. The sequence; most probably developed entirely in the Quaternary without preceding solution in the Tertiary period." @default.
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- W2085367634 date "1975-01-01" @default.
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- W2085367634 title "Evidence for Late Quaternary solution of Chalk at Basingstoke, Hampshire" @default.
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- W2085367634 doi "https://doi.org/10.1016/s0016-7878(75)80027-7" @default.
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