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So-called Amygdaloidal Gabbro, Skye

Published online by Cambridge University Press:  01 May 2009

E. B. Bailey
E. B. Bailey
Affiliation:
19 Greenhill Gardens, Edinburgh
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Abstract

Certain amygdaloidal rocks in Skye have formerly been interpreted as lavas in which the matrix of the amygdales has been replaced by, or alternatively metamorphosed into, material such as one expects in intrusions. It is now claimed that the amygdales formed in intrusions in normal fashion

Type
Articles
Information
Geological Magazine , Volume 89 , Issue 5 , October 1952 , pp. 369 - 375
Copyright
Copyright © Cambridge University Press 1952

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References

REFERENCES

Bailey, E. B., 1924. In Tertiary and Post-Tertiary Geology of Mull. Mem. Geol. Surv.Google Scholar
Falconer, J. D., 1906. The Igneous Geology of the Bathgate and Linlithgow Hills. Trans. Roy. Soc. Edin., xlv, p. 133.Google Scholar
Harker, A., 1904. The Tertiary Igneous Rocks of Skye. Mem. Geol. Surv.Google Scholar
Reynolds, D. L., 1951. The Geology of Slieve Gullion, Foughill, and Carrickarnan: an Actualistic Interpretation of a Tertiary Gabbro-Granophyre Complex. Trans. Roy. Soc. Edin., lxii, p. 85.Google Scholar
Teall, J. J. H., 1889. On the Amygdaloids of the Tynemouth Dyke. Geol. Mag., p. 481.CrossRefGoogle Scholar