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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.

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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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