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硅酸盐熔体包裹体的研究,和以模拟实验为主的实验岩石学,实验矿物学一样,已经成为现代岩浆岩石学,尤其是理论岩浆岩石学研究的一个必不可少的组成部分。 均匀化测温研究,是硅酸盐熔体包裹体研究的一个重要组成部分。其方法是对于呈封闭系统的硅酸盐熔体包裹体进行加热,在反方向上,再造这些包裹体从结晶到熔融的所有阶段,直至其完全均匀化,也就是恢复到它们被生长着的矿物包含、捕获时的状态,借以测量矿物近液相线或固相线的结晶温度。
The study of silicate melt inclusions, like experimental petrology and experimental mineralogy dominated by simulation experiments, has become an indispensable component of modern magmatic petrology, especially the study of theoretical magmatic petrology. Homogenization temperature measurement is an important part of silicate melt inclusions. The method is to heat the silicate melt inclusions in a closed system in the opposite direction and to rebuild the inclusions from all stages of crystallization to melting until they are completely homogenized, ie to recover the minerals they were grown Contains, capture the state, in order to measure the mineral near the liquidus or solidus crystallization temperature.