Rare-earth cation (Nd 3+ ) are incorporated into the interlayer spaces between the silicate layers of synthetic fluorine mica, Na 0.665 Mg 2.68 (Si 3.98 Al 0.02 )O 10.02 F 1.98 , by conventional ion exchange reaction. Subsequent migration of the interlayer cations upon calcination into the vacant octahedra of 2:1 layers is followed by powder X-ray diffraction, diffuse-reflectance UV spectroscopy, and X-ray absorption spectroscopy as a function of calcination temperature. It is found from the spectroscopic analyses that the interlayer cations start to migrate into the octahedral vacant sites from 400 o C through the hexagonal siloxane ring of the tetrahedral silicate layers. According to the Nd L III -edge XANES spectra, the normalized absorption intensity gradually decreases while the FWHM increases with temperature, suggesting that the bonding character of rare-earth cations and silicate lattices evolves from ionic to covalent as the calcination temperature increases.