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- W2000239039 abstract "Summary Conical, not cylindrical, folding is dominant in the Charnian rocks. Passing south-eastwards across the Forest the axial trend of the major anticline changes from south-east to east. The folding is concentric. The minor folds and cleavage are oblique to the axis of the major fold; a possible stress system which might account for this is briefly discussed. The cleavage fans into the cores of some of the minor folds (but not of the major anticline) and into the vertex of one of them; it follows a sinuous course across the Forest and has an average strike of 280 degrees. It is concluded that the Charnoid trend may not be everywhere north-west to south-east." @default.
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- W2000239039 date "1963-05-01" @default.
- W2000239039 modified "2023-09-23" @default.
- W2000239039 title "CONICAL FOLDING AND OBLIQUE STRUCTURES IN CHARNWOOD FOREST, LEICESTERSHIRE" @default.
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- W2000239039 doi "https://doi.org/10.1144/pygs.34.1.67" @default.
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