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
Fe-Mn partitioning between garnet and ilmenite: experimental calibration and applications
β Scribed by Mark I. Pownceby; Victor J. Wall; Hugh St. C. O'Neill
- Publisher
- Springer
- Year
- 1987
- Tongue
- English
- Weight
- 21 KB
- Volume
- 97
- Category
- Article
- ISSN
- 0010-7999
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