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- W2138630654 abstract "Abstract Quartz nodules, exhibiting the morphology of nodular anhydrite, occur in two zones near the top of the Sangomore Formation (Cambro-Ordovician Durness Group) in a section on Balnakiel Bay, northwest Scotland. The nodules, up to 4 cm in diameter, occur in thinly laminated dolomite and are composed of megaquartz and length-slow chalcedony (lutecite and quartzine). Lath-like textural relicts, outlined by opaque inclusions, and minute crystals of anhydrite occur in the megaquartz and lutecite. The quartz nodules are interpreted as silica pseudomorphs after early diagenetic anhydrite nodules which developed in a peritidal setting. Quartz nodules in stratigraphically higher parts of the Durness Group may record the existence of other peritidal sediments in the same geographic area." @default.
- W2138630654 created "2016-06-24" @default.
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- W2138630654 date "1979-03-01" @default.
- W2138630654 modified "2023-09-27" @default.
- W2138630654 title "Evidence of former evaporites in the Cambro-Ordovician Durness Group, northwest Scotland" @default.
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- W2138630654 doi "https://doi.org/10.1016/0037-0738(79)90057-5" @default.
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