Uniform, ultrafine, microcrystalline, hard, pyroxenic glass-ceramic materia
ls have been obtained successfully from basalt rock; instead of adding nucl
eation catalysts, the FeO:Fe2O3, CaO:Na2O, and CaO:MgO ratios have been rec
tified. This process has been accomplished by deliberately adding the small
est permissible amounts of oxidizers, limestone, dolomite, and soda ash (as
additives) that are necessary to fulfill the monominerality requirements;
these requirements affect the melting, workability, crystallization, and mi
crostructure of the glass-ceramics, The melting temperature decreases as th
e ratios decrease (beyond certain limits); in addition, the workability, cr
ystallization, and microstructure also improve as the ratios decrease. An a
lmost-stable solid solution of augite or aegirine-augite composition is the
only crystalline phase that is formed. The minimal FeO:Pe(2)O(3) ratio and
the likelihood of a greater affinity of the Na+ cation for the Fe3+ cation
, rather than the Al3+ cation, may be responsible for increasing the stabil
ity and widening of the crystallization field of the complex aluminum-beari
ng pyroxene solid solution.