High-Quartz Solid Solution Phases from Thermally Crystallized Glasses of Compositions Li2O2,MgO).Al2O3,nSiO2

Thermally crystallized glasses of compositions (Li₂,O₂, MgO).Al₂O₃.nSiO₂ were studied by X-ray powder diffraction methods. High-quartz solid solution phases developed at relatively low temperatures and, for n 3.5, transformed at higher temperatures to keatite solid solution phases. Associated phases, if present, were Mg spinel and/or cordierite, or a few other trace phases. The a crystallographic axis (a₀) of high-quartz solid solutions decreased with increase of MgO and/or SiO₂. The c crystallographic axis (c₀) decreased with increasing MgO; it also decreased with increasing SiO₂, but only when MgO content was low. X-ray diffraction photographs of single crystals of high-quartz solid solutions of compositions LiaO.Al₂O₃.nSiO₃ demonstrated that the maintenance of a basic high-quartz structure is the basis of the solid solution relation. Three modifications of the high-quartz structure were recognized in the Li₂O-Al₂O₃−SiO₃ system. These modifications were based on the occurrence and positions of superlattice reflections. The high-quartz solid solution from Li₂O Al₂O₃−2SiO₂, showing streaky reflections in its precession photographs, suggested a defective structure. The term "high-quartz solid solution," with or without additional prefixes specifying the compositional series and modification, was considered the preferred nomenclature for these solid solution phases.