EBSD is a very powerful earth science technology, it can be used for the analysis of the microstructure and phase identification.By measuring the lattice orientation of the particles and the distribution of the facies, EBSD can be used to determine the mineral crystallography preferred direction of the texture (CPO), and understand that the mineral deformation and phase transformation mechanism.
Mineralogy samples is one of the challenges, the sample is more heavy, the main content and vice phase grain size may be considerable differences, when setting up the measurement parameters is easy to miss these vice.However, EBSD can distinguish with similar chemical composition but different crystal structure phase, and EDS can distinguish between a similar crystal structure but different phase chemical composition.EDS and EBSD combination can be measured include multiphase mineralogy of the samples, to overcome these limitations.
In this case, through the collection of EBSD and EDS signal of Oceanic Gabbro samples of 304/305 U1309D (ODP) is analyzed.10 in the samples with 5 different symmetry phase was successful identification and calibration.It is important to note that the phase identification and distinguish can be semi-automatic execution.Both to the SEM test phase to identify and distinguish to sample directly, also can use the saved at the end of the test data offline.For users, the correct analysis, the need to measure.EBSD phase diagram and orientation distribution (figures 3 and 4) shows the software calibration of low and high crystal symmetry phase at the same time.