Hostname: page-component-cd9895bd7-hc48f Total loading time: 0 Render date: 2024-12-23T16:00:34.762Z Has data issue: false hasContentIssue false
  • English
  • Français

The form of the Beinn an Dubhaich granite, Skye, Scotland

Published online by Cambridge University Press:  01 May 2009

J. G. Raybould
J. G. Raybould
Affiliation:
Department of Geology, University College of Wales, Aberystwyth
Get access Rights & Permissions [Opens in a new window]

Summary

The Beinn an Dubhaich granite has previously been interpreted as a boss, and as a sheet intrusion. The present paper suggests that the structure of the granite is more complex than either of these interpretations implies, and the form is probably that of a shallow funnel intrusion.

Type
Articles
Information
Geological Magazine , Volume 110 , Issue 4 , July 1973 , pp. 341 - 350
Copyright
Copyright © Cambridge University Press 1973

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

Harker, A. 1904. The Tertiary igneous rocks of Skye. Mem. geol. Surv. 132–5.Google Scholar
King, B. C. 1953. Structure and igneous activity in the Creag Strollamus area of Skye. Trans. R. Soc. Edin. 62, 357–402.CrossRefGoogle Scholar
King, B. C. 1960. The form of the Beinn an Dubhaich granite, Skye. Geol. Mag. 97, 326–33.CrossRefGoogle Scholar
Tilley, C. E. 1951. The zoned contact skarns of the Broadford area, Skye. Mineralog. Mag. 29, 621–66.Google Scholar
Tuttle, O. F. & Bowen, N. L. 1958. The origin of granite in the light of experimental studies. Mem. geol. Soc. Amer. 74, 153 pp.Google Scholar
Tuttle, O. F. & Keith, M. L. 1954. The granite problem: evidence from the quartz and feldspar of a Tertiary granite. Geol. Mag. 91, 61–72.CrossRefGoogle Scholar
Whitten, E. H. T. 1961. Modal analysis and the form of the Beinn an Dubhaich granite, Skye. Geol. Mag. 98, 467–72.CrossRefGoogle Scholar