Abstract
A top-bottom effect in double diffraction has been observed in selected-area diffraction (SAD) patterns recorded from epitactic overgrowths. In SAD patterns recorded from epitactic α-Fe2O3 islands grown on an (0001) Al2O3 substrate, the double-diffraction reflections were found always to surround the primary reflections associated with the bottom crystal. This observation is explained using simple geometric constructions and the concepts of kinematical diffraction in a deformed crystal. The effect may be useful as a simple method for determining on which side of a TEM specimen a particular epitactic feature lies. © 1995.
| Original language | English |
|---|---|
| Pages (from-to) | 241-246 |
| Number of pages | 6 |
| Journal | Ultramicroscopy |
| Volume | 60 |
| Issue number | 2 |
| DOIs | |
| State | Published - Jan 1 1995 |
| Externally published | Yes |
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