研究结果表明：各类榴辉岩相岩石的流体包裹体均程度不同地发生了次生变化。未发现原生包裹体。
The studied results show that different secondary changes occurred in fluid inclusions of various rocks and no primary inclusion has been found.
矿物流体包裹体的研究表明：（1）以气液两相包裹体为主，由孤立的原生包裹体和沿裂隙成串分布的次生包裹体构成；
The study of the fluid inclusions from the deposit reveals that:(1) most of them are two-phase isolated primary inclusions and chained secondary inclusions along fractures in minerals;
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