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