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
โฆ LIBER โฆ
An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer: Corrections
โ Scribed by Hugh St. C. O'Neill
- Publisher
- Springer
- Year
- 1980
- Tongue
- English
- Weight
- 31 KB
- Volume
- 72
- Category
- Article
- ISSN
- 0010-7999
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