Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-02T09:57:58.362Z Has data issue: false hasContentIssue false
  • English
  • Français

An extension of the granophyric quartz-dolerite intrusion of Centre 2, Ardnamurchan, Argyllshire

Published online by Cambridge University Press:  01 May 2009

C. S. Butchins
C. S. Butchins
Affiliation:
Department of Geology, University College London, Gower Street, London, WCIE 6BT
Get access Rights & Permissions [Opens in a new window]

Summary

Sheet-like bodies of dolerite with granophyre within the Hypersthene-gabbro on the NE shore of Sanna Bay are shown to be akin to the granophyric quartz-dolerite, and suggest that the latter originally extended for a considerable distance N of its previously mapped limits.

Type
Articles
Information
Geological Magazine , Volume 110 , Issue 5 , September 1973 , pp. 473 - 475
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

Richey, J. E. & Thomas, H. H. et al. 1930. The geology of Ardnamurchan, North-west Mull and Coll. Mem. geol. Surv. U.K. (Scotland).Google Scholar
Skelhorn, R. R. & Elwell, R. W. D. 1966. The structure and form of the Granophyric Quartz-Dolerite Intrusion, Centre II, Ardnamurchan, Argyllshire. Trans. R. Soc. Edinb. 66, 285–306.CrossRefGoogle Scholar
Skelhorn, R. R. & Elwell, R. W. D. 1971. Central subsidence in the layered Hypersthene-gabbro of Centre II, Ardnamurchan, Argyllshire. J. geol. Soc. 127, 535–51.CrossRefGoogle Scholar
Wells, M. K. 1954. The structure of the Granophyric Quartz-Dolerite Intrusion of. Centre 2, Ardnamurchan, and the problem of net-veining. Geol. Mag. 91, 293–307CrossRefGoogle Scholar