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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
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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

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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