silicate minerals

基本解释

Silicates are the most important forming-rock minerals of earth crust rock and in exogenous environments, and the dissolution of silicate minerals is universal.
矽酸鹽是地殼巖石最主要的造巖鑛物，表生條件下矽酸鹽鑛物的溶解是普遍的。
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The dry land of the continents consists mostly of granite and other light silicate minerals, while the ocean floors are made up mostly of a dark, dense volcanic rock called basalt.
陸地地殼主要由花崗巖和其它輕質矽酸鹽鑛物搆成，而海底則主要由黑色的高密度火山巖——玄武巖搆成。
It is inferred that, before explosion, the primary mantle minerals were hydrous magnesium silicate or magnesium-aluminium silicates.
推斷爆炸前的原生鑛物是含水的鎂矽酸鹽和鎂鋁矽酸鹽鑛物。