“…Therrnodynarnic data can often be used quite effectively in discussing the structures of molten salts and ceraITlic oxides (18,45,133). The inforITlation derived froITl such "phase diagraITl ITlethods " is not of the saITle precise nature as that flowing froITl the experiITlental techniques described in the preceding chapters; bond angles, bond lengths, and other geoITletric factors, for exaITlple, cannot be deterITlined.…”