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

✍ Scribed by Bernard J. Wood

Publisher
Springer
Year
1973
Tongue
English
Weight
358 KB
Volume
40
Category
Article
ISSN
0010-7999

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✦ Synopsis

The partition of iron and magnesium between cordierite and garnet depends on P]~o as well as temperature. The apparently conflicting experimental data on the values of K D may be reconciled by considering the P]~O pertaining during the different experiments.

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