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...
প্রধান লেখক: | Hackler, R, Wood, B |
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বিন্যাস: | Journal article |
ভাষা: | English |
প্রকাশিত: |
1989
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অনুরূপ উপাদানগুলি
অনুরূপ উপাদানগুলি
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EXPERIMENTAL-DETERMINATION OF MN-MG MIXING PROPERTIES IN GARNET, OLIVINE AND OXIDE
অনুযায়ী: Wood, B, অন্যান্য
প্রকাশিত: (1994) -
EXPERIMENTAL-STUDY OF FE-MG PARTITIONING BETWEEN GARNET AND OLIVINE AND ITS CALIBRATION AS A GEOTHERMOMETER
অনুযায়ী: Oneill, H, অন্যান্য
প্রকাশিত: (1979) -
An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
অনুযায়ী: O'Neill, H, অন্যান্য
প্রকাশিত: (1979) -
FE2+-MG2+ PARTITION BETWEEN COEXISTING CORDIERITE AND GARNET - DISCUSSION OF EXPERIMENTAL-DATA
অনুযায়ী: Wood, B
প্রকাশিত: (1973) -
EXPERIMENTAL-DETERMINATION OF ACTIVITIES IN FE-MG OLIVINE AT 1400-K
অনুযায়ী: Wiser, N, অন্যান্য
প্রকাশিত: (1991)