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• W2003431714 abstract "Two iron meteorites are now known to contain chlorapatite-silicate-schreibersite assemblages. Thus, phosphorus is present in two oxidation states. Electron microprobe analytical results on the minerals present in these occurrences are combined with thermochemical data in order to examine the oxidation-reduction conditions implied by this assemblage. The silicate phases (olivine, orthopyroxene, clinopyroxene) were found to be out of equilibrium, however, it is still possible to estimate the oxidation state of these meteorites and make direct comparisons with eight other irons and pallasites which contain other phosphate minerals, calcium-free sarcopside and farringtonite, as well as ordinary equilibrated chondrite meteorites. All these metallic meteorites represent approximately the same degree of oxidation as the ordinary chondrites. Some implications regarding the size of a zoned parent body are discussed." @default.
• W2003431714 created "2016-06-24" @default.
• W2003431714 creator A5022586098 @default.
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• W2003431714 date "1967-01-01" @default.
• W2003431714 modified "2023-09-26" @default.
• W2003431714 title "The state of oxidation of some iron meteorites" @default.
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• W2003431714 doi "https://doi.org/10.1016/0019-1035(67)90021-8" @default.
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