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Irregularities in patterns of element partition

Published online by Cambridge University Press:  05 July 2018

Paul Henderson*
Affiliation:
Department of Mineralogy, British Museum (Natural History), London SW 75BD

Summary

In clinopyroxene-melt systems the distribution of chromium and vanadium ions departs from the general pattern of element partition as a function of ionic radius. These departures may be explained by crystal-field effects. Melt structure and the nature of the coordination of cations in the melt also help to determine the pattern of distribution and the extent of the departures from regularity.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1979

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