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Early Tertiary Fold Movements in Mull

Published online by Cambridge University Press:  01 May 2009

R. F. Cheeney
R. F. Cheeney
Affiliation:
Department of Geology, Imperial College, London, S. W. 7.
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Abstract

Evidence is presented which suggests that there is a strong angular unconformity between the Mesozoic sediments and the Tertiary lavas in certain parts of the Island of Mull. The conclusion is drawn that folding movements peripheral to the volcanic centre occurred both before and after the eruption of the main lava succession.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 3 , June 1962 , pp. 227 - 232
Copyright
Copyright © Cambridge University Press 1962

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