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The Continuity of Si and Se Surfaces in Garnets: An Observation

Published online by Cambridge University Press:  01 May 2009

M. N. Saxena
Affiliation:
Department of Geology, Panjab University, Chandigarh 3.

Abstract

Observations have shown that some garnets in the micaceous schists of the Chor area, Himachal Pradesh, India, still retain the continuity between the Se and Si planes. The Se and Si surfaces are continuous surfaces and not merely statistical as has been assumed by some.

Type
Articles
Copyright
Copyright © Cambridge University Press 1964

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References

REFERENCES

Fairbairn, H. W., 1949. Structural Petrology of deformed rocks. Cambridge.Google Scholar
Mügge, O., 1930. Bewegungen von Porphyroblasten. Neue Jahrb., 61, A.Google Scholar
Schmidt, W., 1918. Bewegungsspuren in Porphyroblasten Kristalliner Schiefer. S.B. Akad. Wiss. Wien., 1, 127, 293.Google Scholar
Spry, A., 1963. The Origin and Significance of Snowball Structure in Garnet. J. Petrol., Vol. 4, Part 2, 211222.CrossRefGoogle Scholar