Abstract
Electron diffraction and imaging techniques have been used to examine the structure and thickness of low-angle grain boundaries in olivine. For edge-on grain boundaries, a periodic array of dislocations in a boundary gives rise to sets of periodic rods of diffracted intensity that are recorded as streaks in the diffraction pattern. The length of these streaks provides a measure of the structural width of a boundary. For olivine, the structural width of a boundary with a given dislocation spacing is three to four times smaller than that in metals where the boundary width is approximately equal to the spacing between dislocations in the boundary.
Original language | English (US) |
---|---|
Pages (from-to) | 133-138 |
Number of pages | 6 |
Journal | Physics and Chemistry of Minerals |
Volume | 9 |
Issue number | 3-4 |
DOIs | |
State | Published - Mar 1983 |