Variations in Cr content of magnetite from the upper zone of the Bushveld Complex — evidence for heterogeneity and convection currents in magma chambers-Reference-Cited by-同舟云学术

Variations in Cr content of magnetite from the upper zone of the Bushveld Complex — evidence for heterogeneity and convection currents in magma chambers

Published:1980-02 Issue:3 Volume:46 Page:335-343
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Cawthorn R. Grant,McCarthy T.S.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference26 articles.

1. A review of experimental studies of crystal/liquid trace element partitioning;Irving;Geochim. Cosmochim. Acta,1978

2. Empirical estimation of magnetite/liquid distribution coefficients for some transition elements;Leeman;Contrib. Mineral. Petrol.,1978

3. Kinetic disequilibrium in trace element partitioning between phenocrysts and host lava;Albarède;Geochim. Cosmochim. Acta,1972

4. Analysis of the zoned plagioclase of different magmatic environments: a preliminary ion-microprobe study;Shimizu;Earth Planet. Sci. Lett.,1978

5. Layered Igneous Rocks;Wager,1968

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