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- W2078942362 abstract "In Strath Oykell and Lower Loch Shin, Sutherland, several outcrops of Lewisian-Gneiss-like rocks occur, previously described at the Airde of Shin and Durcha as being part of the Moinian. They form a discontinuous sill-like body up to 300 m. thick, extending in a 180° arc round a centre 8 km. north of Cassley Falls, dipping 15–50° outward throughout. They show little evidence of folding of other than isoclinal style. Contrary to previous published statements, hornblende-bearing gneisses are confined to a distinct, mappable unit, largely composed of biotite-oligoclase-quartz gneisses which do not grade laterally into Moine psammites. Diopside marbles with later tremolite in the Shin Group may indicate retrogressive metamorphism of earlier high-grade rocks. Chemical analysis shows that the Shin Group is low in TiO2, has high FeO total/TiO2, low K2O and low Rb/Sr, all Lewisian characteristics. The calcsilicates are MgO- and K2O-rich compared with normal Moinian calc-silicates. It is concluded that the Shin Group is another Lewisian inlier." @default.
- W2078942362 created "2016-06-24" @default.
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- W2078942362 date "1970-01-01" @default.
- W2078942362 modified "2023-09-25" @default.
- W2078942362 title "Geochemical distinctions between the Lewisian of Cassley, Durcha and Loch Shin, Sutherland, and the surrounding Moinian" @default.
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- W2078942362 doi "https://doi.org/10.1016/s0016-7878(70)80026-8" @default.
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