at high temperature have been investigated by means of in situ high temperature powder XRD measurements. The monoclinic P2 1 /n phase of Li 2 MgSiO 4 shows a reversible phase transition to high temperature orthorhombic Pmnb phase due to the order-disorder of Mg and Li atoms at 590 °C. By slow cooling from 1000°C to room temperature, the monoclinic Pn phase of Li 2 MgGeO 4 was obtained. Lattice parameters are a = 6.389(1), b = 5.475(1), c = 4.995(1) Å, and β = 90.18(1). The monoclinic Pn phase of Li 2 MgGeO 4 shows a reversible transformation to the orthorhombic Pmn2 1 phase at 540 °C, accompanied with the abrupt contraction along c-axis and elongation along b-axis on heating.Key words: orthosilicates, wurzite-type structure, cationic ordering, powder XRD, DTA 4,5) , structural details of the phase transitions are not clear. We will report the revisited high temperature powder XRD study on the structural phase transitions of Li 2 MgSiO 4 and Li 2 MgGeO 4 .Li 2 MgSiO 4 and Li 2 MgGeO 4 were reported by P. Tart and T. Cahay in 1970 for the first time as members of series of compounds Li 2 MXO 4 (M: Mg, Zn, Cd, Mn, Fe, Co; X: Si, Ge) with the crystal structures analogous to those of Li 3 PO 4 6) . In these compounds, oxide ions form a pseudo-hexagonal closed packed (hcp) structure. The cations occupy a half of its tetrahedral sites and show some ordered arrangements, depending on the metal species and the heat treatments during the sample preparation. . Also their mutual relationships or phase transitions among polymorphs have been summarized.