Abstract
Electron-diffraction patterns both with hexagonal and trigonal symmetry were obtained from graphite. The trigonal patterns are shown to arise from a stacking fault on the basal plane. This observation is a consequence of the dependence of the pattern symmetry on the symmetry of the whole crystal, not only the symmetry of the unit cell.
Original language | English |
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Pages (from-to) | 89-91 |
Number of pages | 3 |
Journal | Acta Crystallographica Section A |
Volume | 28 |
Issue number | 1 |
DOIs | |
Publication status | Published - 1972 |
Externally published | Yes |