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Partitioning of Fe2+ and Mg2+ between olivine and garnet

โœ Scribed by Toshisuke Kawasaki; Yoshito Matsui

Book ID
115854195
Publisher
Elsevier Science
Year
1977
Tongue
English
Weight
561 KB
Volume
37
Category
Article
ISSN
0012-821X

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๐Ÿ“œ SIMILAR VOLUMES

Fe2+-Mg2+partition between coexisting co
Fe2+-Mg2+partition between coexisting cordierite and garnet โ€” a discussion of the experimental data
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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.

Experimental calibration of the partitio
Experimental calibration of the partitioning of Fe and Mg between biotite and garnet
โœ J. M. Ferry; F. S. Spear ๐Ÿ“‚ Article ๐Ÿ“… 1978 ๐Ÿ› Springer ๐ŸŒ English โš– 445 KB

The cation exchange reaction Fe3A12Si30 a 2 + KMg3A1Si3Olo(OH)2 = Mg3AlzSi30 m + KFe3-A1Si3Olo(OH)/ has been investigated by determining the partitioning of Fe and Mg between synthetic garnet, (Fe, Mg)3A11Si3012, and synthetic biotite, K(Fe, Mg)3A1Si3Olo(OH) 2. Experimental results at 2.07 kbar and