Abstract
SummaryCurved and other variably oriented minor F1 folds with a common axial–planar cleavage are described from the Dalradian of the South-West Scottish Highlands. An explanation for the varying orientations is offered in terms of progressive deformation following the arguments of Flinn (1962) and Ramsay (1967).
Publisher
Cambridge University Press (CUP)
Cited by
41 articles.
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