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Continuity in the monazite-huttonite series

Published online by Cambridge University Press:  05 July 2018

Henryk Kucha
Henryk Kucha*
Affiliation:
Institute of Geology and Mineral Deposits, 30-059 Kraków, Av. Mickiewicza 30, Poland
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Summary

Electron diffraction and electron-microprobe investigations have revealed the presence of order in the monazite-huttonite series. Chemical analyses from the literature and electron-microprobe analyses in this study show that the monazite-huttonite series, REPO4-ThSiO4, is only continuous if the contribution of F, M 2+, and OH to the charge balance is taken into account. The electron-diffraction study points to ordered domain structures in the series.

Information

Type
Research Article
Information
Mineralogical Magazine , Volume 43 , Issue 332 , December 1980, pp. 1031 - 1034
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1980

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