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- W1963544491 abstract "The Mössbauer effect in 57Fe was used to investigate iron minerals in meteorites. The ratio of olivine iron to pyroxene iron (calculated from the absorption intensities and the recoilless fractions) was found to be 1.6 ± 0.2 for the bronzite chondrites Collescipoli, Ochansk, and Oakley. The relative amounts of iron in olivine and pyroxene may be combined with the electron microprobe analyses of iron and magnesium in the separate minerals to obtain the number of formula units of pyroxene relative to olivine in an unseparated meteorite sample. The similar abundance ratios of pyroxene to olivine indicate that these meteorites were derived from a common parent ferromagnesian silicate reservoir. For each meteorite, the FeO content of the olivine-pyroxene system is given as calculated from the MgO content of the chemical analysis, the ratio of magnesium to iron in each silicate, and the relative amounts of iron in olivine and pyroxene." @default.
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- W1963544491 date "1968-01-01" @default.
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- W1963544491 title "Ferromagnesian silicate abundances in bronzite chondrites as determined by the Mössbauer effect" @default.
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- W1963544491 doi "https://doi.org/10.1016/0019-1035(68)90063-8" @default.
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