Many mineralogical phases, as well as new developed synthetic compounds, occur only in form of nano-crystalline materials. The structure characterization of these phases results often impossible with conventional X-ray techniques, as X-ray single crystal diffraction is not possible for crystals smaller than 10 µm and powder X-ray is limited to one-dimensional information, resulting inadequate in presence of low symmetry structures, super-structured phases and multiphase systems. Conversely, an electron beam can be focused on a spot of few nanometres, allowing single nano-crystal analysis. Well known problems related with electron diffraction are the strong dynamical effects due multiple scattering, the reduced number of reflections achievab...