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- W2331614215 abstract "I. Introduction.During the mapping of the Morar district by the Geological Survey prior to the recent war the writer noted a few occurrences of miniature drag-folds in the Moine Schists along the western limb of the Morar Anticline (Fig. 1). The rocks affected are certain highly-inclined thin alternating beds of psammitic and pelitic schists belonging to the Upper Psammitic Group of the Morar stratigraphical succession, which lies in the garnet zone of metamorphism. The folding takes the form of low closely-spaced parallel ridges where seen upon the bedding plane of a psammitic layer (Plate VIII., Fig. 1). The structures bear some resemblance to ripple-markings, but for the reasons following they are interpreted as small drag-folds. Cross-sections of the structures reveal that the beds are folded, and, further, that the down-dip limb of each miniature anticline is longer than the other limb. So, the shape of the structures is of the type to be expected in the case of drag-folds1 developed along the western limb of the Morar Anticline concurrently with the formation of the anticline. The structures, in fact, are congruous drag-folds (Hills, 1940, p. 90). The axes of the folds are parallel to the direction followed by nearby examples of two widely developed structures in the Morar area, namely, lineation and ‶roddlng,″ the latter being the result of intense puckering of psammitic rocks. All three types of structure are inclined at approximately the same angle and in the same direction as the local pitch of the Morar Anticline." @default.
- W2331614215 created "2016-06-24" @default.
- W2331614215 creator A5032210871 @default.
- W2331614215 date "1948-01-01" @default.
- W2331614215 modified "2023-10-14" @default.
- W2331614215 title "Pre-metamorphism cleavage in the Moine Schists of Morar, western Inverness-shire" @default.
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- W2331614215 doi "https://doi.org/10.1144/transed.14.2.200" @default.
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