Hostname: page-component-848d4c4894-hfldf Total loading time: 0 Render date: 2024-05-17T15:13:41.368Z Has data issue: false hasContentIssue false

Steps facing against the slip direction: a model

Published online by Cambridge University Press:  01 May 2009

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

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
Copyright
Copyright © Cambridge University Press 1974

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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