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Steps facing against the slip direction: a model

Published online by Cambridge University Press:  01 May 2009

M. Lindström
M. Lindström
Affiliation:
Fachbereich Geowissenschaften(Geologie/Paläontologie)D-355 MarburgLahnbergeFed. Rep. Germany
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Summary

Dry starch-flour provides a light, suitably cohesive material in which slip structures can be produced. These resemble slickensides and offer some insight into one of the possible processes whereby structures occurring on natural slickensides may be produced. Steps consistently face against the movement direction. They form by the partial disintegration of temporarily coherent lumps dragged along the surface.

Type
Articles
Information
Geological Magazine , Volume 111 , Issue 1 , January 1974 , pp. 71 - 74
Copyright
Copyright © Cambridge University Press 1974

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References

Hills, E. Sherbon. 1972. Elements of Structural Geology, 2nd ed. Chapman & Hall, London, 502 pp.CrossRefGoogle Scholar
Höfer von Heimhalt, H. 1917. Die Verwerfungen (Paraklase, exokinetische Spalten). Vieweg Verl., Braunschweig, 128 pp.CrossRefGoogle Scholar
Paterson, M. S. 1958. Experimental deformation and faulting in Wombeyan marble. Bull. geol. Soc. Am. 69, 465–76.CrossRefGoogle Scholar
Riecker, R. F. 1965. Fault plane features: an alternative explanation. J. sedim. Petrol. 35, 746–8.CrossRefGoogle Scholar