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- W2003423908 abstract "Abstract We have studied the isotope properties of carbon phases including carbon source, diamond, carbon dissolved in metal melt and the gas phase formed at diamond crystallization experiment in the closed system Fe–Ni–C at 1450 °С and 5.5 GPa during 17.5 h. The δ 13 C value of the grown diamond decreases in direction of growth from − 26.5 to − 27.1‰, when the δ 13 C value of initial carbon is − 27.1‰. Carbon isotope composition of the melt is by 3.2‰ lower than that of coexisting diamond. The data obtained agree well with the model calculations of isotope fractionation on crystallization from solution in a closed system." @default.
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- W2003423908 date "2008-11-01" @default.
- W2003423908 modified "2023-09-26" @default.
- W2003423908 title "Carbon isotope fractionation associated with HPHT crystallization of diamond" @default.
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- W2003423908 doi "https://doi.org/10.1016/j.diamond.2008.06.003" @default.
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