在显微镜中可以清楚看到，赤铁矿中有不少磁铁矿的残晶。
Some relict crystals of magnetite in hematite are clearly discovered under the mineragraphic microscope.
经过分凝作用之后，岩浆的成分发生了变化，岩浆中依然存在小颗粒的耐熔残晶。
The segregation caused the component variation of the magma and the small crystals still existed in the magma.
经过分凝作用之后，岩浆的成分发生了变化，岩浆中依然存在小颗粒的耐熔残晶。
The segregation caused the component variation of the magma and the small crystals still existed in the magma.
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