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- W2129938250 abstract "The Orfordness shingle consists largely of flint. However, depending on particle size, non-flint components usually form 5–10 per cent of the material. Composition of the non-flint fraction indicates derivation from Pleistocene outcrops to the north. Typical of such outcrops are relative scarcity of quartz and the common presence of Rhaxella and Carboniferous cherts. Features typical of outcrops to the south are scarce." @default.
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- W2129938250 date "1990-01-01" @default.
- W2129938250 modified "2023-09-27" @default.
- W2129938250 title "Composition of the Orfordness shingle" @default.
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- W2129938250 doi "https://doi.org/10.1016/s0016-7878(08)80009-0" @default.
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