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- W2024462250 abstract "A new allotropic form of carbon occurs in shock-fused graphite gneisses in the Ries Crater, Bavaria. The assemblage in which it occurs consists of hexagonal graphite, rutile, pseudobrookite, magnetite, nickeliferous pyrrhotite, and baddeleyite. Electron-probe analyses indicate that the new phase is pure carbon. It is opaque and much more strongly reflecting than hexagonal graphite. Measurement of x-ray diffraction powder patterns leads to cell dimensions a = 8.948 +/- 0.009, c = 14.078 +/- 0.017 angstroms, with a primitive hexagonal lattice." @default.
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- W2024462250 date "1968-07-26" @default.
- W2024462250 modified "2023-10-18" @default.
- W2024462250 title "A New Allotropic Form of Carbon from the Ries Crater" @default.
- W2024462250 doi "https://doi.org/10.1126/science.161.3839.363" @default.
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