作者: R. J. Williams , J. Akella , O. Mullins
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摘要: The partitioning of chromium between olivines, spinels and silicate liquids was studied as a function temperature, oxygen fugacity, cooling rate 1175 1300 C redox states near the Fe-FeO buffer. It is found that weight ratio Cr2O3 in olivine to liquid increases slightly fugacity decreases, but effect very small. experiments showed content does not re-equilibrate with cooling.