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The origin of the granitic sheets and veins in the Loch Coire migmatites, Scotland

Published online by Cambridge University Press:  05 July 2018

P. E. Brown
P. E. Brown*
Affiliation:
Department of Geology, The University, Sheffield
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Summary

Most of the granitic sheets and veins in the Loch Coire migmatite complex do not have chemical compositions in accordance with a formation by local anatexis. Regional metasomatism by fluids from outside the exposed confines of the complex was an important factor in the development of the sheets and veins, although there was probably some overlap with magmatic conditions.

Type
Research Article
Information
Mineralogical Magazine , Volume 38 , Issue 296 , December 1971 , pp. 446 - 450
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1971

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References

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