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Structural Features of the Grey Granites of Aberdeenshire

Published online by Cambridge University Press:  01 May 2009

James Cameron
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Introduction

The area containing the quarries discussed in this paper extends inland from the City of Aberdeen for a distance of about twenty miles and is bounded on the north and south by the rivers Don and Dee. This is the area of the Newer Granites of Aberdeenshire, which C. B. Bisset has described in “A Contribution to the Study of Some Granites near Aberdeen” and has divided the acid igneous rocks into:—

1. The Skene Complex: consisting of diorite, adamellite, grey granites, transition types and minor intrusions.

2. Later Group: consisting of coarse red granites.

Type
Articles
Information
Geological Magazine , Volume 82 , Issue 5 , October 1945 , pp. 189 - 204
Copyright
Copyright © Cambridge University Press 1945

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References

REFERENCES

Anderson, J. G. C., 1939. Granites of Scotland. Mem. Geol. Sur. Min. Resources, vol. xxxii.Google Scholar
Balk, R., 1937. Structural Behaviour of Igneous Rocks. Mem. Geol. Soc. Amer., No. 5.Google Scholar
Bisset, C. B., 1932. A Contribution to the Study of Some Granites near Aberdeen. Trans. Edin. Geol. Soc. vol. xiii, part 1.Google Scholar
Dale, T. N., 1923. Commercial Granites of New England. U.S. Geol. Sur. Bull., 738.Google Scholar
Fairburn, H. W., 1937. Structural Petrology, Queen’s Univ., Kingston, Canada.Google Scholar
Hills, E. Sherbon, 1940. Outlines of Structural Geology, London.Google Scholar