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VI.—On Slickensides and the Origin of some Marl-Bands in the Chalk

Published online by Cambridge University Press:  01 May 2009

Percy F. Kendall
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Extract

The phenomenon of “Slickensides” is considered to occur only in connexion with faulting, and it has frequently happened that another name has been conferred upon it when not accompanied by signs of fracture; but some recent observations have led me to doubt the propriety of making such a distinction.

Type
Original Articles
Information
Geological Magazine , Volume 1 , Issue 12 , December 1884 , pp. 551 - 555
Copyright
Copyright © Cambridge University Press 1884

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