Fe2+-Mg2+ partition between coexisting cordierite and garnet - a discussion of the experimental data

Bernard J. Wood*

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    18 Citations (Scopus)

    Abstract

    The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments.

    Original languageEnglish
    Pages (from-to)253-258
    Number of pages6
    JournalContributions to Mineralogy and Petrology
    Volume40
    Issue number3
    DOIs
    Publication statusPublished - Sep 1973

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