Earlier crystallization of felsic minerals than biotite and garnet is related with much lower crystallization pressure.
长英质矿物早于黑云母和石榴子石结晶与岩浆侵位浅（结晶压力低）相关。
These reactions involving melt are not only controlled by PT conditions, but also genetically associated with dehydration melting, partial melting of felsic minerals in host rocks.
这类熔体参与变质反应不仅受控于温压条件，而且与寄主岩石脱水熔融、长英质矿物部分熔融存在密切成因关系。
The presence of these minerals gives felsic rock its characteristic light gray color.
这些矿物的存在使这种岩石呈特有的浅灰色。
The presence of these minerals gives felsic rock its characteristic light gray color.
这些矿物的存在使这种岩石呈特有的浅灰色。
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