这些界面反应物主要来自挤压铸造时粘结剂与熔融的镁反应。
These interfacial reaction products are mainly from the reaction between the binder and the melted magnesium.
所以我去了趟图书馆，查阅了，第六版的《高级熔融态盐化学》，因为那里面有一篇关于生产镁的，化学和电化学的文章。
So, I went to the library and I looked up Advances in Molten Salt chemistry volume six because there's an article in there about the chemistry and electrochemistry of magnesium production.
因此，岩浆起源于加厚地壳底部榴辉岩相镁铁质岩石的低度部分熔融，且岩浆源区受到了流体的影响。
Therefore, the magmas were the product of low partial melting of mafic eclogite at the base of the thickened crust, and their magma sources were affected by fluids.
综合地球化学证据表明岩浆起源不受古俯冲体系的影响，而是幔源岩浆与榴辉岩相镁铁质岩石部分熔融岩浆混和的产物。
The deeply studies show the GD intrusions was mixed by magmas from mantle and from lower crust, without the effect of subduction system.
综合地球化学证据表明岩浆起源不受古俯冲体系的影响，而是幔源岩浆与榴辉岩相镁铁质岩石部分熔融岩浆混和的产物。
The deeply studies show the GD intrusions was mixed by magmas from mantle and from lower crust, without the effect of subduction system.
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