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作者对岩石中的熔融包裹体及其测温方法进行了实验,在淬火法测温方面取得了新的进展,对熔融包裹体的特征进行了较系统的总结。 一、熔融包裹体的鉴别特征 熔融包裹体是硅酸盐岩浆结晶过程中某些矿物捕获了硅酸盐熔浆而形成的。包裹体中的熔浆随着温度的下降形成了固化的玻璃质和气泡,当它缓慢结晶或通过脱玻结晶作用,也可形成结晶质和气泡,前者为玻璃包裹体,后者为结晶包裹体。
The authors have carried out experiments on the melt inclusions in rocks and their temperature measurement methods. New progress has been made in the temperature measurement by quenching methods. The characteristics of melt inclusions have been systematically summarized. First, the identification of melt inclusions Molten inclusions in the silicate magma crystallization process of certain minerals captured silicate melt formed. The inclusions in the melt with the temperature dropped to form a solidified glassy and bubbles, when it slowly crystallizes or through de-crystallization crystallization can also form crystals and bubbles, the former for the glass inclusions, the latter for the crystal package body.