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A Note on the Gneisses of Rum

Published online by Cambridge University Press:  01 May 2009

C. E. Tilley
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Extract

The recent reinterpretation of the structure of Rum presented by E. B. Bailey (1944) involves a revision of the age of the gneisses of that island. Harker's description of these banded and foliated rocks had referred them to a late date in the Tertiary igneous sequence of the plutonic centre (Harker, 1908). This interpretation had been arrived at in face of the earlier belief of Geikie that they formed part of the Lewisian Series and it is now known that Harker's contemporaries on the Geological Survey who had opportunity of examining his collections dissented from his conclusions though this opinion had until recently not been committed to print (Flett, 1944).

Type
Articles
Information
Geological Magazine , Volume 81 , Issue 3 , June 1944 , pp. 129 - 131
Copyright
Copyright © Cambridge University Press 1944

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References

REFERENCES

Bailey, E. B., 1944. Tertiary Igneous Tectonics of Rhum (Inner Hebrides) Proc. Geol. Soc., London, No. 1041, 38–9.Google Scholar
Flett, J. S., 1944. In discussion, Ibid., London, No. 1041, 39–40.Google Scholar
Harker, A., 1908. The Geology of the Small Isles of Inverness-shire. Mem. Geol. Surv. Scotland, 105–114.Google Scholar
Tilley, C. E., 1924. Contact Metamorphism in the Comrie area of the Perthshire Highlands. Quart. Journ. Geol. Soc., lxxx, 65–6.Google Scholar