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....
Главный автор: | Wood, B |
---|---|
Формат: | Journal article |
Язык: | English |
Опубликовано: |
Springer-Verlag
1973
|
Схожие документы
-
EXPERIMENTAL-STUDY OF FE-MG PARTITIONING BETWEEN GARNET AND OLIVINE AND ITS CALIBRATION AS A GEOTHERMOMETER
по: Oneill, H, и др.
Опубликовано: (1979) -
An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
по: O'Neill, H, и др.
Опубликовано: (1979) -
EXPERIMENTAL-DETERMINATION OF FE AND MG EXCHANGE BETWEEN GARNET AND OLIVINE AND ESTIMATION OF FE-MG MIXING PROPERTIES IN GARNET
по: Hackler, R, и др.
Опубликовано: (1989) -
Atomistic simulation of trace element incorporation into garnets - comparison with experimental garnet-melt partitioning data
по: van Westrenen, W, и др.
Опубликовано: (2000) -
SOLUBILITY OF ALUMINA IN ORTHOPYROXENE COEXISTING WITH GARNET
по: Wood, B
Опубликовано: (1974)