Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-10T13:31:05.305Z Has data issue: false hasContentIssue false
  • English
  • Français

An unusual distribution of precipitates in a diamond

Published online by Cambridge University Press:  14 March 2018

C. J. Shah  and
A. R. Lang
C. J. Shah
Affiliation:
Royal Holloway College, University of London1
A. R. Lang
Affiliation:
H. H. Wills Physics Laboratory, University of Bristol
Get access Rights & Permissions [Opens in a new window]

Summary

The central region of a type 1 stone was found by optical and X-ray topographic examination to be densely populated with small inclusions. The X-ray studies indicated that these were precipitates formed after growth of the stone. Precipitate sizes fell into two groups, 1 µ or less, and around 5 µ. Many cases of decoration of grown-in dislocations by these precipitates were observed.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 33 , Issue 262 , September 1963 , pp. 594 - 599
Copyright
Copyright © 1963, The Mineralogical Society

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

2 A. R., Lung, Acta Cryst., 1959, vol. 12, p. 249 Google Scholar.

3 Idem,Acta Metallurgica, 1957, vol. 5, p.358.

1 N., Kato and A. R., Lang, Acta Cryst., 1959, vol. 12, p. 787.Google Scholar