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A Camptonitic Dyke Suite at Monar, Ross-shire and Inverness-shire

Published online by Cambridge University Press:  01 May 2009

John G. Ramsay
John G. Ramsay
Affiliation:
Department of Geology, Imperial College, London, S.W. 7.
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Abstract

A swarm of basaltic and camptonitic dykes in the Northern Highlands of Scotland has been studied. The dykes include monchiquite, olivine basalt, olivine dolerite, and camptonite, and a study of the relations of the various types in individual dykes suggests that the camptonites have arisen by the crystallization of late fractions from a magma of fairly normal dolerite type.

Type
Articles
Information
Geological Magazine , Volume 92 , Issue 4 , August 1955 , pp. 297 - 309
Copyright
Copyright © Cambridge University Press 1955

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References

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