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...
Main Authors: | Hackler, R, Wood, B |
---|---|
格式: | Journal article |
語言: | English |
出版: |
1989
|
相似書籍
-
EXPERIMENTAL-DETERMINATION OF MN-MG MIXING PROPERTIES IN GARNET, OLIVINE AND OXIDE
由: Wood, B, et al.
出版: (1994) -
EXPERIMENTAL-STUDY OF FE-MG PARTITIONING BETWEEN GARNET AND OLIVINE AND ITS CALIBRATION AS A GEOTHERMOMETER
由: Oneill, H, et al.
出版: (1979) -
An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
由: O'Neill, H, et al.
出版: (1979) -
FE2+-MG2+ PARTITION BETWEEN COEXISTING CORDIERITE AND GARNET - DISCUSSION OF EXPERIMENTAL-DATA
由: Wood, B
出版: (1973) -
EXPERIMENTAL-DETERMINATION OF ACTIVITIES IN FE-MG OLIVINE AT 1400-K
由: Wiser, N, et al.
出版: (1991)