Hi everyone,
I'm having problems in processing coupled EBSD and EDS measurements on experimental mixed calcite-dolomite gouges. The quality of the EBSD data is good, despite a hit rate ranging between 50-65%, mostly due to porosity and very fine grained material of the samples ( grain size <1 um). The dolomite grains are incorrectly characterised by a more or less thick rim of calcite (and spurious pixels inside). This error is mostly due to the activation volume of the EDS, which on the borders collects data both from the dolomite grain and the surrounding matrix (calcite rich) resulting in an incorrect phase recognition in these areas.
This is a problem for the interpretation of the orientation of the calcite within the maps, since data include the "fake"-calcite too.
I'd like to know if someone knows some ways either to get rid of these misindexed points or change them into dolomite (still maintaining the orientation though).
Moreover, in the analysis I'd like to maintain the non-indexed areas, limit the grain to the minimum necessary.
I have attached a band contrast image of one small map and the phase map. In the latter you can see how the dolomite grains are surrounded by a rim of calcite (thicker as smaller the dolomite grains are) and some pixels within the grains too.
Any suggestion and help is welcome.
Cheers,
Matteo