Lanthanide disilicates and oxyapatites have potential roles in high temperature applications as thermal (TBC) and environmental barrier coatings (EBC), or possible alteration phases in geological nuclear waste respositories. However, those Ce 3+-bearing silicates have only been limitedly studied. In this work we performed detailed structural and thermodynamic investigations on ACe 2 Si 2 O 7 (tetragonal, P4 1) and Ce 4.67 (SiO 4) 3 O (hexagonal, P6 3 /m). The high temperature structural behaviors and coefficients of thermal expansion were determined by in situ high temperature synchrotron X-ray diffraction (HT-XRD) implemented with Rietveld analysis and thermogravimetric analysis coupled with differential scanning calorimetry (TGA-DSC). ACe 2 Si 2 O 7 was found to be stable in N 2 and air up to ~1483 K with an isotropic thermal expansion (α a = 12.3 × 10-6 K-1 and α c = 12.4 × 10-6 K-1). Ce 4.67 (SiO 4) 3 O had a slow partial oxidation between 533 K and 873 K to a new nonstoichemitric phase Ce 3+ 1.67-x Ce 4+ x Ce 3+ 3 (SiO 4) 3 O 1+0.5x , followed by a thermal decomposition to CeO 2 and SiO 2 at ~1000 K. By using high temperature oxide melt solution calorimetry at 973 K with lead borate as solvent, we determined, for the first time, the standard enthalpy of formation of ACe 2 Si 2 O 7 (-3825.1 ± 6.0 kJ/mol) and Ce 4.67 (SiO 4) 3 O (-7391.3 ± 9.5 kJ/mol). These thermodynamic paramters were compared with those of CeO 2 , CeSiO 4 , and other silicate oxyapatites for examining their chemical stability in high temperature environments relevent for aeronautical applications, mineral formation, and nuclear fuel cycle.