壳源组分的加入是促进岩浆熔离作用的重要因素。
The addition of the crustal materials into the magma played an important role in promoting the liquation processes.
岩浆起源于上地幔，属于拉斑玄武岩系列，发生过金属硫化物的熔离作用。
The magma originated from the upper mantle and belongs to the tholeiitic series which has undergone immiscible separation of metal sulfide.
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