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Development of Schistosity in Flexural Folds

Published online by Cambridge University Press:  01 May 2009

D. Mukhopadhyay
Affiliation:
Department of Geology, Presidency College, Calcutta-12, India.

Abstract

An example of the development of axial plane schistosity close to a buckled competent band is described. There is a difference in the degree of development of the schistosity on the convex and the concave sides of the fold arch. This is explained as due to variation in contact strain. A similar pattern has been produced experimentally and it is concluded that the axial plane schistosity in the example under consideration is a mechanical phenomenon and has developed perpendicular to the direction of maximum compressive strain.

Type
Articles
Copyright
Copyright © Cambridge University Press 1965

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References

REFERENCES

Flinn, D., 1962. On folding during three-dimensional progressive deformation. Quart. J. geol. Soc. Lond., 118, 385433.CrossRefGoogle Scholar
Ramberg, H., 1959. Evolution of ptygmatic folding. Norsk. geol. Tidsskr., 39, 99151.Google Scholar
Ramberg, H. 1962. Contact strain and folding instability in layered rocks. Geol. Rdsch., 51, 405440.CrossRefGoogle Scholar
Ramsay, J. G., 1962. The geometry and mechanics of formation of “similar” type folds. J. Geol. 70, 309327.CrossRefGoogle Scholar
Maxwell, J. C., 1962. Origin of slaty and fracture cleavage in the Delaware Water Gap area, New Jersey and Pennsylvania. Petrologic Studies— A volume to honour A. F. Buddington. Geol. Soc. Amer. pp. 281311.Google Scholar
Sander, B., 1950. Einführung in die Gefügekunde der geologischen Körper, Zweiter Teil. Vienna.CrossRefGoogle Scholar