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An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer: Corrections

โœ 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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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

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