Hostname: page-component-78c5997874-8bhkd Total loading time: 0 Render date: 2024-11-08T07:27:58.117Z Has data issue: false hasContentIssue false

Structural Features of the Grey Granites of Aberdeenshire

Published online by Cambridge University Press:  01 May 2009

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
Copyright
Copyright © Cambridge University Press 1945

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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