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- W2105132360 abstract "Synopsis Arkoses of the Sleat and Torridon groups in south-east Skye form a continuous succession 4500 m thick. Palaeocurrents came from the west. The source rocks were hornblende-biotite-gneisses, granite or granite-gneisses, quartzose sediments and acid volcanics, all with upper crustal geochemical signatures. Detritus from the basic gneisses predominates in the lowest sediments, but is gradually replaced by granitic material stratigraphically up the succession. The lowest sediments accumulated in palaeovalleys with a relief of The climate was initially arid. But the development of rift highlands attracted rainstorms, and the higher runoff leached Ca from hornblende as it weathered to chlorite. Small amounts of Na may also have been lost from plagioclase during weathering. The ratio of material transported in solid form to that in solution is estimated to lie in the range 15–20 for the lowest formation, but to have been" @default.
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- W2105132360 date "1991-12-01" @default.
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- W2105132360 title "Geochemistry, provenance and palaeoclimate of the Sleat and Torridon groups in Skye" @default.
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- W2105132360 doi "https://doi.org/10.1144/sjg27020081" @default.
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