一个多世纪以来,对矿物中气—液包体已进行了系统的研究工作。因而,已经积累了有关热液成矿作用过程中的大量资料。众所周知,测定均一化温度的方法是现代测定矿物温度的一种最重要方法,根据异常包体及三相(液-液-气)包体的研究,常常为计算矿物结晶时的压力打下了基础。 For more than a century, the gas-liquid inclusions in minerals have been studied systematically. Thus, a great deal of information has been accumulated on hydrothermal mineralization. It is well-known that the method of determining the homogenization temperature is one of the most important modern methods for determining the temperature of minerals. Based on the study of the abnormal inclusions and the three-phase (liquid-liquid-gas) inclusions, it is often the basis for calculating the pressure at the time of mineral crystallization .