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On the Significance of Thermal Structure in the Scottish Highlands

Published online by Cambridge University Press:  01 May 2009

W. Q. Kennedy
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Extract

The formation of a fold mountain chain is, essentially, a thermal phenomenon, as may be deduced from the internal locus of the forces involved, the frequent association of magrriatic activity with erogenic movements, and the widespread thermal and regional metamorphism of the sediments within the deeper parts of the mountain belt.

Type
Articles
Information
Geological Magazine , Volume 85 , Issue 4 , August 1948 , pp. 229 - 234
Copyright
Copyright © Cambridge University Press 1948

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References

LITERATURE

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