Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-26T07:44:48.022Z Has data issue: false hasContentIssue false
  • English
  • Français

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

Published online by Cambridge University Press:  01 May 2009

M. N. Saxena
M. N. Saxena
Affiliation:
Department of Geology, Panjab University, Chandigarh 3.
Get access Rights & Permissions [Opens in a new window]

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
Information
Geological Magazine , Volume 101 , Issue 6 , 30 December 1964 , pp. 502 - 503
Copyright
Copyright © Cambridge University Press 1964

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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, 211–222.CrossRefGoogle Scholar