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近现代对于熔体包裹体(melt inclusion)的研究已经有50余年,但它们在反映岩浆系统特征方面的价值是直至最近10~15年间才逐渐被火山学家,岩石学家和包裹体学者所意识到。熔体包裹体的研究结果之所以难以被接受主要有以下几个因素:(1)缺乏可靠的分析技术;(2)熔体包裹体捕获后会发生一系列的变化;(3)有的包裹体中熔体存在不均匀的现象;(4)较高的均一温度,很难测定。但随着分析方法的改进和熔体包裹体的系统研究的进展,学者们逐渐确定了熔体包裹体在解开岩浆系统
Modern research on melt inclusions has been in existence for more than 50 years, but their value in reflecting the characteristics of magmatic systems was not gradually recognized by volcanologists, petrologists, and inclusion scholars until the last 10-15 years Realize. The reason why the results of melt inclusions are hard to be accepted is that: (1) there is a lack of reliable analytical techniques; (2) a series of changes occur after the melt inclusions are captured; (3) some packages The body of the melt there is uneven phenomenon; (4) a higher uniform temperature, it is difficult to determine. However, with the improvement of analytical methods and the systematic study of melt inclusions, scholars have gradually established that the melt inclusions have great potential in unlocking the magmatic system