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- W50482666 abstract "Lunar samples indicate efficient reduction of iron and formation of nanophase metallic iron particles in agglutinitic impact glasses and in amorphous rims of vapor deposits [1, 2]. Terrestrial impactites do not show sufficient reduction of iron but the presence of Fe-oxide spherules was reported for K-T boundary layer (e.g., [3]). It is highly probable that these Feoxide spherules had originated as Fe-metal droplets and then were oxidized during the long deposition. Our experimental investigation shows partial reduction of siderophile and even lithophile elements during the impact-simulated high-temperature processing of silicates." @default.
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- W50482666 date "2010-09-01" @default.
- W50482666 modified "2023-09-23" @default.
- W50482666 title "The Effect of Reduction of Elements on Their Dynamics During an Impact." @default.
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