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矿物的形成与分布主要受温度、压力、介质性质等物理化学条件所制约。研究者们为了了解这些物理化学参数曾多方面进行探索。应用矿物中包裹体所包含的原始成岩成矿介质来探讨矿物形成的温度、压力、介质浓度及成分,矿物共生组合及空间分布规律、成矿物质来源等问题有着指导意义。目前地质研究者广泛应用这一手段解决成岩、
The formation and distribution of minerals are mainly controlled by the physical and chemical conditions such as temperature, pressure and medium nature. Researchers have explored many aspects of these physicochemical parameters. The application of the primitive diagenetic ore-forming media contained in inclusions of minerals to study the formation, temperature and pressure of minerals, the concentration and composition of minerals, the symbiosis of minerals and their spatial distribution, and the origin of ore-forming materials are of guiding significance. At present, geologists have widely used this method to solve diagenesis,