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前人对热液矿物中的包裹体研究比较多,也比较详细,并利用包裹体的测温和成分分析等资料,解决了一些岩石矿床的成因问题。但是,对常温常压下从地表水中形成的沉积矿物,特别是盐类矿物中的包裹体则研究较少。近几年来,我们对几种盐类矿物的包裹体进行加热研究,发现这种包裹体当加热到一定温度时会产生汽化现象。这一现象,对区分不同成因的气液包裹体和正确进行包裹体测温,具有较重要的意义。
Previous studies on the inclusions in hydrothermal minerals have been more detailed and more detailed. The temperature and composition analysis of the inclusions are used to solve the genesis problems of some rock deposits. However, there is less research on the inclusions of sedimentary minerals formed from surface water at normal temperature and pressure, especially in salt minerals. In recent years, we have studied the heating of inclusions of several salt minerals and found that the inclusions vaporize when heated to a certain temperature. This phenomenon is of great significance in distinguishing the gas-liquid inclusions of different origin from the correct inclusion temperature measurement.