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The Production of Amphibolic and other Skarn Rocks from Limestone at Cor, Co. Donegal

Published online by Cambridge University Press:  01 May 2009

Amin Gindy
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Abstract

Diopside-skarns, epidote-skarns, and garnet-skarns together with very coarse amphibole-rocks are produced at the contact of limestone and epidiorite by diffusion of trondhjemitic material along the contact. The amphibole-rocks are unusual types, for the formation which material may have been drawn from the epidiorite side the contact.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 2 , April 1951 , pp. 103 - 112
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Cole, G. A. J., 1905. On the growth of crystals in the contact zone of granite and amphibolite. Proc. Roy. Irish Acad., xv, 117.Google Scholar
Wright, W. I., 1938. The composition and occurrence of garnets. Amer. Min., xxiii, 436.Google Scholar