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Mylonite, Slickensides, and the Great Glen Fault1
Published online by Cambridge University Press: 01 May 2009
Abstract
It is shown that mylonite is extremely rare in the plane of the Great Glen fault, and that horizontal slickensides or friction-grooves directed along the Glen are virtually absent. Grave doubt is consequently thrown on the alleged horizontal displacement in the fault zone.
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- Copyright © Cambridge University Press 1951
Footnotes
Communicated to the British Association for the Advancement of Science, Section C, 13th August, 1951.
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