岩相学及岩石化学研究表明，岩浆演化机制是矿物分离结晶作用。
The petrologic and petrochemical study has shown that the main mechanism controlling the magmatic evolution is fractional crystallization of minerals.
但在高位岩浆房中，随着分离结晶作用的进行，岩浆的温度和氧逸度逐渐降低。
However, the temperatures and oxygen fugacity of magmas at high level magma chamber decreased along with fractional crystallization.
采用乳化结晶法，研究了粗蒽精制过程中溶剂、温度、助剂及分离时间的作用。
The effects of solvent, temperature, additive and separation time on the refinement process of crude anthracene by using emulsion-crystallization were reported.
成岩作用是分离结晶和同化混染联合作用。
成岩作用是分离结晶和同化混染联合作用。
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