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• 10:37, 26 July 2019 Dbk talk contribs uploaded File:P008263.jpg (Scourie dykes intrude a late Scourian shear zone in Lewisian gneiss. The gneiss to the left of the dyke still retains a largely Scourian fabric. Aird Fenish, West Lewis (D02693). From: Plate 5. Johnstone, G S and Mykura, W. 1989. British regional geolo...)