Models for incompatible trace-element abundances in cumulus minerals and their application to plagioclase and pyroxenes in the Bushveld Complex
The capacity of trapped residual liquid to reset the major element composition of minerals in layered intrusions has been established. This principle is extended to provide a mathematical treatment of incompatible trace-element distribution in minerals during crystallization of trapped interstitial...
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Veröffentlicht in: | Contributions to mineralogy and petrology 1996-02, Vol.123 (1), p.109 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The capacity of trapped residual liquid to reset the major element composition of minerals in layered intrusions has been established. This principle is extended to provide a mathematical treatment of incompatible trace-element distribution in minerals during crystallization of trapped interstitial fluid. |
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ISSN: | 0010-7999 1432-0967 |