Royal Society of Chemistry, Dalton Transactions, 14(53), p. 6224-6233, 2024
DOI: 10.1039/d4dt00179f
Full text: Unavailable
We used DFT+U to explore high-P structures and energetics of CeSiO4, and found the stetindite → scheelite transition at ∼15 GPa (>8.4 GPa predicted by enthalpy) is driven by lattice instability, due to softening and imaginary state of the Eg1 mode.