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Origin of Minor Structures Associated with Folding

Published online by Cambridge University Press:  01 May 2009

Emyr Williams
Affiliation:
Department of Mines, G.P.O. Box 124B, Hobart, Tasmania.
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Abstract

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Type
Correspondence
Copyright
Copyright © Cambridge University Press 1964

References

REFERENCES

de Sitter, L. U., 1957. Cleavage Folding in Relation to Sedimentary Structure. International Geological Congress, 20th Session, Mexico (1956). Section V, 5364.Google Scholar
de Sitter, L. U., 1958. Boudins and Parasitic Folds in Relation to Cleavage and Folding. Geol. en Mijnbouw, 20, 277286.Google Scholar
Fyson, W. K., 1962. Tectonic Structures in the Devonian Rocks near Plymouth, Devon. Geol. Mag., 99, 208226.CrossRefGoogle Scholar
Ramberg, H., 1963. Evolution of Drag Folds. Geol. Mag., 100, 97105.CrossRefGoogle Scholar
Ramsay, J. G., 1962. The Geometry and Mechanics of Formation of “Similar” Type Folds. Jour. Geol., 70, 309327.CrossRefGoogle Scholar
Williams, E., 1959. The Sedimentary Structures of the Upper Scamander Sequence and their Significance. Pap. Proc. Roy. Soc. Tas., 93, 2932.Google Scholar
Williams, E., 1961 a. The Deformation of Confined, Incompetent Layers in Folding. Geol. Mag., 98, 317323.CrossRefGoogle Scholar
Williams, E., 1961 b. Flow Folding in Rocks. Nature, 189, 474–5.CrossRefGoogle Scholar