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The Occurrence of Chloritoid in the Hecla Hoek Formation of Prince Charles Foreland, Spitsbergen

Published online by Cambridge University Press:  01 May 2009

D. J. Atkinson
D. J. Atkinson
Affiliation:
Department of Geology, Imperial College, London, S.W.7.
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Abstract

In the Hecla Hoek rocks of Prince Charles Foreland, field evidence indicates that chloritoid has developed only where conditions of extreme stress have affected pelitic rocks of a certain type. Microscopic examination confirms that many of the chloritoid-bearing rocks are extremely strained, and demonstrates that growth of the mineral was contemporaneous with movement. The distribution of chloritoid is in complete discordance with the pattern of regional metamorphism.

Type
Articles
Information
Geological Magazine , Volume 93 , Issue 1 , February 1956 , pp. 63 - 71
Copyright
Copyright © Cambridge University Press 1956

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References

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