Pw. Trimby et al., Misorientations across etched boundaries in deformed rocksalt: a study using electron backscatter diffraction, J STRUC GEO, 22(1), 2000, pp. 81-89
Automated electron backscatter diffraction (EBSD) in the scanning electron
microscope has been used to collect crystallographic orientation and misori
entation data from etched surfaces of deformed synthetic rocksalt. By compa
ring the misorientation across individual boundaries to the intensity of et
ching, we have assessed the effectiveness of the etching procedure. High an
gle (>10 degrees) grain boundaries are typically etched significantly more
than low angle subgrain boundaries, and thus they can be easily identified
using reflected light microscopy. However, there exists considerable variat
ion in the intensity of etching of subgrain boundaries, independent of thei
r misorientation. The intensity of intragranular boundary etching is contro
lled by the crystallographic orientation of the etched surface: surfaces cl
ose to {100} faces are only lightly etched, while surfaces close to {111} f
aces are heavily etched. Therefore, whilst reflected light microscopy of et
ched surfaces of deformed rocksalt remains extremely useful for general mic
rostructural characterisation, fully quantitative techniques such as EBSD a
re ideal for more detailed microstructural analyses. (C) 1999 Elsevier Scie
nce Ltd. All rights reserved.