Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-10T07:16:24.263Z Has data issue: false hasContentIssue false
  • English
  • Français

Corona structures formed by near-isochemical reaction between olivine and plagioclase in a metamorphosed dolerite

Published online by Cambridge University Press:  05 July 2018

R. N. England
R. N. England*
Affiliation:
Bureau of Mineral Resources Canberra, Australia
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Short Communications
Information
Mineralogical Magazine , Volume 39 , Issue 307 , September 1974 , pp. 816 - 818
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1974

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.)

Footnotes

1

Published with permission of the Director, Bureau of Mineral Resources, Canberra, A.C.T., Australia.

References

Griffin, (W. L.), 1971. Journ. Petrology, 12,219.CrossRefGoogle Scholar
Mason, (R.), 1967. Min. Mag., 36, 504.Google Scholar
Murthy, (M. V. N.), 1958. Bull. Geol. Soc. Amer., 69, 23.CrossRefGoogle Scholar
Robie, (R. A.), Bethke, (D. M.), and Beardsley, (K. M.), 1967. U.S. Geol. Surv. Bull., 1248.Google Scholar
Whitney, (P. R.) and Mclelland, (J. M.), 1973. Contr. Min. Petr., 39, 81–98.CrossRefGoogle Scholar