“…The best known are the following: the RE 2 SiO 5 orthosilicates, the RE 2 Si 2 O 7 disilicates also called pyrosilicates, and the RE silicates related to apatite structures: RE 9.33 (SiO 4 ) 6 O 2 , and RE 10 (SiO 4 ) 6 O 3 . , Disilicates are able to exhibit various polymorphs, which depend on the synthesis temperature, on the pressure, and on the chosen RE element. − At least 11 forms are known and reported with a specific nomenclature (A to I, ,, K, and X types). The apatite-type RE silicates were greatly studied in particular since cationic vacancies on one site induce free oxygen atoms leading to ionic conduction − and curiously all of them are reported with the P 6 3 / m space group, in opposite to the disilicates for which a symmetry change is observed depending on the RE element. ,− This paper follows the preliminary works of Davesnne et al , and Guillaume and deals with advanced TEM studies of annealed Eu-/Tb-codoped ZnO thin films at high temperatures typically 1100 °C to complete the nanoscale structure characterization, to identify more precisely the microstructure of the detected RE silicate inclusions, and eventually to understand the observed major changes in the luminescence properties at this extreme temperature. Especially, a crystallographic approach from precession electron diffraction tomographic (PEDT) data coupled with atomic scanning TEM (STEM)-high-angle annular dark-field (HAADF) imaging has been carried out.…”