0 any of a large number of common minerals formed of silica, oxygen, and one or more other elements -- 矽酸鹽
A method for determining the solubility of water in silicate melts.
Particles of order 10m in size are generally single spheres or conglomerates or lattice silicates.
Concomitant separation of strontium and samarium- neodymium for isotope analyses in silicate samples, based on specific extraction chromatography.
Since actual observed vesicle fillings are silicate minerals, chemical element transfers from basalt to geodes must have taken place.
Chapter 4 examines the role of silicate melts and volatile fluids in magma systems.
The next group of papers is concerned with the genesis of carbonatites and their spatial and temporal association with silicate magmas.
The outgassing is independent of the surface temperature while the silicate weathering rate is strongly dependent on temperature.
By design, elements bound in silicate structures were not normally dissolved by the procedures used.
