稳定同位素特征表明其成岩流体为海水、大气成因水或原生水。
The stable isotope composition indicates that their rock-forming fluid is the seawater, meteoric water or primary water.
已有文用流体运动学的观点，提出原生应力——冷缩假说。
Some geologists have developed the "primary stress-cooling hypothesis" based on the viewpoint of the fluid kinematics.
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.
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