The Experimental Determination of Partition Coefficients for CR Between Orthopyroxene and a Synthetic Bushveld/stillwater Parent Melt, as a Function of Oxygen Fugacity and Temperature: Implications for the Distribution of Chromite in Layered Intrusions

Details The Experimental Determination of Partition Coefficients for CR Between Orthopyroxene and a Synthetic Bushveld/stillwater Parent Melt, as a Function of Oxygen Fugacity and Temperature: Implications for the Distribution of Chromite in Layered Intrusions The Experimental Determination of Partition Coefficients for CR Between Orthopyroxene and a Synthetic Bushveld/stillwater Parent Melt, as a Function of Oxygen Fugacity and Temperature: Implications for the Distribution of Chromite in Layered Intrusions

Mar 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985lpi....16...29b&link_type=gif

LUNAR AND PLANETARY SCIENCE XVI, PP. 29-30. Abstract.

Computer Science

Earth, Bushveld Complex, South Africa, Stillwater Complex, Montana, Melts, Experiments, Partitioning, Orthopyroxene, Chromite, Chromitite, Chromium, Analogs, Oxygen, Fugacity, Temperature, Thermal Effects, Intrusions

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