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- W2045498959 abstract "The fusion crust of meteorites is modified by many factors (orientation during flight, heat conductivity in the whole meteorite and in the components, chemical reactivity, etc.). In spite of that, some properties can be astonishingly alike, and the zonal arrangement of mineral associations shows many relations nearly everywhere. Of special interest may be the formation of magnetite, wüstite and a ‘high temperature maghemite’, the alterations in chromite, ilmenite, iron, alabandite and niningerite, ‘Henderson phase’ and graphite." @default.
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- W2045498959 date "1967-05-01" @default.
- W2045498959 modified "2023-10-18" @default.
- W2045498959 title "Die schmelzkruste der meteoriten" @default.
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- W2045498959 doi "https://doi.org/10.1016/0012-821x(67)90129-x" @default.
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