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Metamorphic Differentiation of Talc-Magnesite-Chlorite Rocks in Shetland

Published online by Cambridge University Press:  01 May 2009

M. S. Amin
M. S. Amin
Affiliation:
Department of Geology, Imperial College, London, S.W. 7.
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Abstract

Practically monomineralic masses of talc, of magnesite, and of chlorite are formed in talc-magnesite-chlorite-rocks as a result of localized shearing and associated hydrothermal activity within deformation-belts.

Type
Articles
Information
Geological Magazine , Volume 89 , Issue 2 , April 1952 , pp. 97 - 105
Copyright
Copyright © Cambridge University Press 1952

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References

REFERENCES

Chapman, C. A., 1950. Quartz Veins Formed by Metamorphic Differentiation of Aluminous Schists. Amer. Min., xxxv, 693.Google Scholar
Cooke, H. C., 1937. Thetford, Disraeli, and Eastern Half of Warwick Map-Area, Quebec. Geol. Surv. Can. Mem. 211.Google Scholar
Eskola, P., 1932. On the Principles of Metamorphic Differentiation. Compt. Rend. Soc. Géol. Finlande, No. 5, 68.Google Scholar
Gilson, J. L., 1927. Origin of the Vermont Talc Deposits. Econ. Geol., xxii, 246.Google Scholar
Hess, H. H., 1933. Hydrothermal Metamorphism of an Ultrabasic Intrusive at Schuyler, Virginia. Amer. Jour. Sci. (5), xxvi, 377.CrossRefGoogle Scholar
Macgregor, A. M., 1932. The Geology of the Country around Que Que, Gwelo District. S. Rhod. Geol. Surv. Bull. No. 20.Google Scholar
Phillips, F. C., 1927. The Serpentine and Associated Rocks and Minerals of the Shetland Islands. Quart. Jour. Geol. Soc., lxxxiii, 622.CrossRefGoogle Scholar
Phillips, A. H., and Hess, H. H., 1936. Metamorphic Differentiation at contacts between Serpentine and siliceous country rocks. Amer. Min., xxi, 333.Google Scholar
Read, H. H., 1934. The metamorphic Geology of Unst in the Shetland Islands. Quart. Jour. Geol. Soc., xc, 637.CrossRefGoogle Scholar
Read, H. H., 1933. On quartz-kyanite veins in Unst, Shetland Islands, and their bearing on metamorphic differentiation. Miner. Mag., xxiii, 317.Google Scholar
Stillwell, F. L., 1918. The metamorphic rocks of Adelie Land. Australian Antarctic Expedition, vol. iii, pt. 1.Google Scholar
Wilcockson, W. H., and Tyler, W. H., 1933. On an Area of Ultra-basic Rocks in the Kassala Province of the Anglo-Egyptian Sudan. Geol. Mag., lxx, 317.Google Scholar
Wilson, G. V., and Phemister, J., 1941. Talc, Other Magnesian Minerals and Chromite with British Serpentines. Geol. Surv. Great Britain. War-time Pamphlet No. 9.Google Scholar