实验结果还表明，中性-中酸性硅酸盐熔体的不混溶性普遍存在。
The results also show that the immiscibility of the intermediate and intermediate-acid silicate melts exists widespreadly.
随着温度的升高同一体系内的熔体成分均向酸性方向演化。
And at the same localized melting system, compositions of melts run to acid along with the increase of temperature.
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