Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-06T07:05:16.106Z Has data issue: false hasContentIssue false

A comparison of gel and glass starting materials for phase equilibrium studies

Published online by Cambridge University Press:  05 July 2018

G. M. Biggar
Affiliation:
Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh 9
M. J. O'Hara
Affiliation:
Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh 9

Summary

A method of preparing compositions suitable for phase equilibrium studies in systems containing CaO-MgO-Al2O3-SiO2-Fe-O2-Na2O employing a gelling technique is described. The subsolidus assemblages obtained from the recrystallization of some of these gels and from the recrystallization of devitrified glasses of the same composition are compared. It is not yet clear whether either starting material has any advantage as the gels may retain early formed metastable phases and the glasses may fail to nucleate stable phases.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1969

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

Boyd, (F. R.) and Schairer, (J. F.), 1964. Journ. Petrology, 5, 275-309.10.1093/petrology/5.2.275CrossRefGoogle Scholar
Hamilton, (D. L.) and Henderson, (C, M. B.), 1968. Min. Mag. 36, 832-8.Google Scholar
Hytönen, (K.) and Schairer, (J. F.), 1961. Carnegie Inst. Wash. Year Book, 60, 134-9.Google Scholar
O'Hara, (M. J.) and Biggar, (G. M.). Amer. Journ. Sci. (in press).Google Scholar
O'Hara, (M. J.) and Schairer, (J. F.), 1963. Caenegie Inst. Wash, Year Book, 62, 107-15.Google Scholar
Sakata, (Y.), 1957. Japan Journ. Geol. Geogr., Trans. 28, 161-8.Google Scholar