FE2+-MG2+ PARTITION BETWEEN COEXISTING CORDIERITE AND GARNET - DISCUSSION OF EXPERIMENTAL-DATA
The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments....
主要作者: | Wood, B |
---|---|
格式: | Journal article |
语言: | English |
出版: |
Springer-Verlag
1973
|
相似书籍
-
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) -
EXPERIMENTAL-DETERMINATION OF FE AND MG EXCHANGE BETWEEN GARNET AND OLIVINE AND ESTIMATION OF FE-MG MIXING PROPERTIES IN GARNET
由: Hackler, R, et al.
出版: (1989) -
Atomistic simulation of trace element incorporation into garnets - comparison with experimental garnet-melt partitioning data
由: van Westrenen, W, et al.
出版: (2000) -
SOLUBILITY OF ALUMINA IN ORTHOPYROXENE COEXISTING WITH GARNET
由: Wood, B
出版: (1974)