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A Note on the Development of Large Garnets in Sutherland Migmatites

Published online by Cambridge University Press:  01 May 2009

T. G. K. Charlu  and
H. H. Read
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Abstract

In the outer zone of the Sutherland Migmatite Complex, four-inch garnets are developed in “veins” in garnetiferous rocks which, adjacent to the “veins”, are devoid of garnet. The redistribution of material has been brought about by activity along certain privileged paths. Comparison is made with the gigantic 3-ft. garnets of the Adirondacks.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 3 , June 1951 , pp. 185 - 191
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

Becke, F., 1882. Die Gneissformation des wiederösterreichischen Waldviertels. Tscher. Min. Pet. Mitt., iv, 406.Google Scholar
Cheng, Y. C., 1943. The Migmatite Area around Bettyhill, Sutherland. Quart. Journ. Geol. Soc., xcix, 107.Google Scholar
Heddle, M. F., 1878. Chapters on the mineralogy of Scotland, Chapter 3— The garnets. Miner. Mag., ii, 230.Google Scholar
Holland, T. H., 1896. On the origin and growth of garnets and of their micropegmatite intergrowths in pyroxene rocks. Rec. Geol. Surv. India, xxix, pt. 1, 30.Google Scholar
Lacroix, A., 1889. Contributions à l'étude des gneiss à pyroxène et des roches a wernérite. Bull. Soc. Min. Fr., xii, 317.Google Scholar
Levin, S. B., 1950. Genesis of some Adirondack garnet deposits. Bull. Geol. Soc. Amer., lxi, 519.CrossRefGoogle Scholar
Read, H. H., 1931. Geology of Central Sutherland. Mem. Geol. Surv. Scotland.Google Scholar