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- W1999366930 abstract "Distinction is drawn between mullions which look like ‘clustered columns’ and are composed of the local country-rock, and rodding which consists of quartz-rods derived from silica secreted from the rocks during movement and metamorphism. The mullions of Oykell Bridge in South Sutherland are described, and are found to consist of varieties formed by folded bedding, intersecting bedding and cleavage, and of irregular types. Their elongation plunges to the south-east and is parallel to the local fold-axes. The quartz-rods of Ben Hutig in North Sutherland (Beinn Thutaig in the NW. Highland Memoir, pp. 601-3) plunge gently to the east and are parallel to the axes of recumbent folds seen between Ben Hutig and the Kyle of Tongue. The rods have been formed by rolling or shearing movements acting at right-angles to their lengths. Neither the quartz-rods, nor the mullions, nor the folds with which they are associated, seem to bear any relationship to the Caledonian thrust-movements. The structural evidence supports Horne's, Read's and Coles Phillips' views that the age and folding of the Moine Series was pre-Torridonian." @default.
- W1999366930 created "2016-06-24" @default.
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- W1999366930 date "1953-06-01" @default.
- W1999366930 modified "2023-09-27" @default.
- W1999366930 title "Mullion and rodding structures in the Moine Series of Scotland" @default.
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- W1999366930 doi "https://doi.org/10.1016/s0016-7878(53)80012-x" @default.
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