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Cummingtonite-bearing Rocks from the Lewisian

Published online by Cambridge University Press:  01 May 2009

C. E. Tilley
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Extract

Manganiferous schists carrying cummingtonite or grunerite are now known from several areas of the Lewisian of Scotland. Cummingtonite in paragneisses was first described from the Gairloch area (1)1 and it has since been met with at two localities in the Lewisian inlier of Glenelg—at Druideag Lodge, Loch Duich (2), in association with eulysites, and in the gorge of Glen Beag, 5½ miles south of this points—here associated with rhodonite and pyroxman-gite (3).

Type
Original Articles
Information
Geological Magazine , Volume 75 , Issue 2 , February 1938 , pp. 76 - 81
Copyright
Copyright © Cambridge University Press 1938

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References

REFERENCES

(1)Mem. Geol. Surv. Great Britain (N.W. Highlands), 1907, p. 82.Google Scholar
(2)Tilley, C. E., Min. Mag., 1936, vol. 24, p. 331.Google Scholar
(3)Tilley, C. E., Amer. Min., 1937, vol. 22, p. 720.Google Scholar
(4)Eskola, P., and Kervinen, T., Compt. Rendu Soc. Geéol. de Finlande, 1936, No. 9, p. 475.Google Scholar
(5)Gustafson, J. K., Econ. Geol., 1933, vol. 28, p. 123.Google Scholar
(6)B., Rama Rao, Bull. Mysore Geol. Dept., 1934, No. 15, pp. 1–36.Google Scholar