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The part played by tholeiitic magma in the Carbo-Permian vulcanicity of central Scotland

Published online by Cambridge University Press:  14 March 2018

Frederick Walker
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Summary

The end-Carboniferous quartz-dolerites form a curious tholeiitic interlude in the alkaline olivine-basalt vulcanicity which characterized central Scotland from the top of the Old Red Sandstone to the Lower Permian. The relationship of the two magma-types is discussed in the light of fresh evidence.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 34 , Issue 268 , 1965 , pp. 498 - 516
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1965

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