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Addressing the Difficulties of Differentiating Members of the Feldspar Solid Solution Series via Electron Backscatter Diffraction

Many minerals in the geological realm behave as solid solutions with one of the most common of these being the Feldspar series. Combine this with lower symmetries and it can be difficult to both index and differentiate these minerals. One final complication is that the phase files available for these phases may be for chemical compositions that are much different from the actual sample. This presents many difficulties in indexing the EBSD patterns. Understanding the differences in the patterns with small changes in chemistry and atomic positions can help the analyst get more correct orientations and less noise in geological EBSD data. Using dynamically simulated EBSD patterns, it is possible to model the differences between the members of the solid solutions to come up with strategies to increase the precision and accuracy of indexing routines.