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- W1983535849 abstract "An ion probe study of rare earth element (REE) geochemistry of silicate inclusions in the Miles HE iron meteorite was carried out. Individual mineral phases among inclusions have distinct REE patterns and abundances. Most silicate grains have homogeneous REE abundances but show considerable intergrain variations between inclusions. A few pyroxene grains display normal igneous REE zoning. Phosphates (whitlockite and apatite) are highly enriched in REEs (50 to 2000 X CI) with a relatively light rare earth element (LREE)-enriched REE pattern. They usually occurred near the interfaces between inclusions and Fe host. In Miles, albitic glasses exhibit two distinctive REE patterns: a highly fractionated LREE-enriched (CI normalized La/Sm similar to 15) pattern with a large positive Eu anomaly and a relatively heavy rare earth element (HREE)-enriched pattern (CI-normalized Lu/Gd similar to4) with a positive Eu anomaly and a negative Yb anomaly. The glass is generally depleted in REEs relative to CI chondrites." @default.
- W1983535849 created "2016-06-24" @default.
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- W1983535849 date "2003-12-01" @default.
- W1983535849 modified "2023-09-28" @default.
- W1983535849 title "Rare earth element geochemistry and petrogenesis of miles (IIE) silicate inclusions" @default.
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- W1983535849 doi "https://doi.org/10.1016/s0016-7037(03)00207-2" @default.
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