EXPERIMENTAL-DETERMINATION OF FE AND MG EXCHANGE BETWEEN GARNET AND OLIVINE AND ESTIMATION OF FE-MG MIXING PROPERTIES IN GARNET
The partitioning of Fe and Mg between garnet and olivine has been determined as a function of Fe/Mg ratio at 1000°C and 9.1 kbar. Garnets of composition XgtFe = 0.90, 0.82, 0.60, 0.51, and 0.35 were mixed with olivines of various compositions in a ratio of 10:1 by mass, and the equilibrium olivine c...
主要な著者: | Hackler, R, Wood, B |
---|---|
フォーマット: | Journal article |
言語: | English |
出版事項: |
1989
|
類似資料
-
EXPERIMENTAL-DETERMINATION OF MN-MG MIXING PROPERTIES IN GARNET, OLIVINE AND OXIDE
著者:: Wood, B, 等
出版事項: (1994) -
EXPERIMENTAL-STUDY OF FE-MG PARTITIONING BETWEEN GARNET AND OLIVINE AND ITS CALIBRATION AS A GEOTHERMOMETER
著者:: Oneill, H, 等
出版事項: (1979) -
An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
著者:: O'Neill, H, 等
出版事項: (1979) -
FE2+-MG2+ PARTITION BETWEEN COEXISTING CORDIERITE AND GARNET - DISCUSSION OF EXPERIMENTAL-DATA
著者:: Wood, B
出版事項: (1973) -
EXPERIMENTAL-DETERMINATION OF ACTIVITIES IN FE-MG OLIVINE AT 1400-K
著者:: Wiser, N, 等
出版事項: (1991)