0 any of a large number of common minerals formed of silica, oxygen, and one or more other elements -- 矽酸鹽
Magnetic fabrics show an evolution similar to the silicate mineral fabrics.
Magnetic fabrics show an evolution similar to the silicate mineral fabrics in general.
Densities of liquid silicate systems calculated from residual molar volumes of oxide components.
The hollow spaces left when the creatures dissolved were filled with silicate in solution.
Present clues on the composition of organic refractories and silicates will be given.
By design, elements bound in silicate structures were not normally dissolved by the procedures used.
The outgassing is independent of the surface temperature while the silicate weathering rate is strongly dependent on temperature.
The next group of papers is concerned with the genesis of carbonatites and their spatial and temporal association with silicate magmas.
