Fe2+-Mg2+ partition between coexisting cordierite and garnet — a discussion of the experimental data期刊界 All Journals 搜尽天下杂志传播学术成果专业期刊搜索期刊信息化学术搜索

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

Authors:	Bernard J Wood

Institution:	(1) Department of Geology and Geophysics, University of California, 94720 Berkeley, California

Abstract:	The partition of iron and magnesium between cordierite and garnet depends on $P_{{\text{H}}_{\text{2}} {\text{O}}}$ as well as temperature. The apparently conflicting experimental data on the values of K _D may be reconciled by considering the $P_{{\text{H}}_{\text{2}} {\text{O}}}$ pertaining during the different experiments.

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