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- W2087487316 abstract "Synopsis S.E.M. studies of the clastic components of calcareous concretions from the late-Devensian, glaciomarine Errol Beds near the type site, east-central Scotland, reveal fabrics indicative of deposition from originally flocculated suspensions. Previously undescribed spherical cavities 30–350 μm in diameter, characteristically fringed by aligned platy particles, are thought to have been former gas bubbles around which the grains adhered by surface tension. It is suggested that the gas was ammonia, believed to have been derived from the decay of proteinaceous organic matter which promoted localised CaCO 3 precipitation through a rise in pH. The delicate, porous fabrics preserved via cementation indicate that the concretions are of early diagenetic origin and formed rapidly, close to the sediment–water interface. In contrast, the fabrics shown by the host clays are consistent with consolidation of originally flocculated materials." @default.
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- W2087487316 date "1990-06-01" @default.
- W2087487316 modified "2023-10-16" @default.
- W2087487316 title "S.E.M. study of clastic fabrics preserved in calcareous concretions from the late-Devensian Errol Beds, Tayside" @default.
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- W2087487316 doi "https://doi.org/10.1144/sjg26010033" @default.
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