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- W2002369884 abstract "The lithological variations shown by the Upper Greensand within the Wessex area are first considered. Glauconite, phosphate, limestone and chert, all of which characterise the series, are then discussed in turn. Five distinct types of glauconite occur, often in different sedimentary associations; the mineral has formed from a variety of source materials, but in all cases seems to have solidified from an original gelatinous state. Phosphatic nodules may form by replacement of calcareous shells, sponges or limestone concretions, and are particularly associated with depositional breaks and richly glauconitic horizons. Calcareous stone is mostly rich in detrital grains, being produced by the cementation by calcite of the surrounding sand. Nodules of pure limestone at certain horizons are thought to result from the recrystallisation of calcareous patches in the original sediment. The Upper Greensand cherts appear to have formed in fairly shallow but tranquil waters. A mass of silica gel, precipitated on the sea-floor, solidified into a nodule of porous stone which was subsequently converted into true chert by deposition of silica from solution. The arenaceous sediment was brought into the sea from a land-mass to the west." @default.
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- W2002369884 date "1960-01-01" @default.
- W2002369884 modified "2023-10-16" @default.
- W2002369884 title "Aspects of the lithology of the Wessex Upper Greensand" @default.
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- W2002369884 doi "https://doi.org/10.1016/s0016-7878(60)80014-4" @default.
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