然而,有时观察到硅酸盐包裹体的晶体形态比其他硅酸盐矿物更接近金刚石的内部结构。
Sometimes, however, the crystal form of the silicate inclusions is observed to resemble more closely the internal structure of diamond than that of other silicate minerals.
所有的岩浆基本上地包括多种多样的硅酸盐矿物,高硅氧化合物;但任何给定的(岩浆)流的化学成分都可能与其他岩浆流有完全不同地化学成分。
All magma consists basically of a variety of silicate minerals, high in silicon-oxygen compounds, but the chemical composition of any given flow may differ radically from that of any other.
给出金属、高聚物和硅酸盐等材料典型的实验结果,它们与其他一些研究者的结果十分一致。
Typical experimental results for metals, polymers and ceramic materials are given and a good agreement with other investigater's results is shown.
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