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在研究和测试包裹体(以下简称包体)的物理化学性质时,通常假设包体从矿物结晶被捕获时起,其容积和内部成分总量不再与外界交换。若在室内对矿物重新加热,其中包体溶液在某一温度下又恢复均匀充满整个包体容积的状态。设包体容积不随温度和压力而变,则温度继续增高时,包体溶液始终保持等容均一态,直至在某一温度压力下破裂。
In studying and testing the physicochemical properties of inclusions (hereinafter referred to as inclusions), it is generally assumed that the volume of the inclusions and the total amount of internal components are no longer exchanged with the outside world since the time when the inclusions were captured. If the indoor re-heating of minerals, including the inclusion solution at a certain temperature and restore the volume of the entire state of the pack. Suppose the volume of the inclusion body does not change with the temperature and pressure, then the temperature continues to increase, the inclusion body solution is always kept in uniform state until ruptured at a certain temperature and pressure.