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- W2053737275 abstract "Quantitative concentration differences of the elements Fe, Si, Mg, Ca, Al, Ti, Mn, K and P between the L and H group common chondrites are compared. The Fe difference (26%) is by far the largest. P is positively correlated with Fe, indicating that P may have some siderophile character despite the fact that it occurs either as apatite or merrilite in the common chondrites. P is distinctly enriched in the Fe-high enstatite chondrites. The degree of fractionation of most of the lithophile elements examined is 7–12%; fractionation of Ti appears to be a little less. A critical comparison of the SiMg relationship in the L and H groups of chondrites indicates that these two abundant lithophile elements are slightly fractionated between these two chondrite groups." @default.
- W2053737275 created "2016-06-24" @default.
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- W2053737275 date "1970-11-01" @default.
- W2053737275 modified "2023-10-03" @default.
- W2053737275 title "The composition of stony meteorites (VII) observations on fractionation between the L and H chondrites" @default.
- W2053737275 cites W1978709008 @default.
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- W2053737275 doi "https://doi.org/10.1016/0012-821x(70)90133-0" @default.
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