Because of plagioclase fractionation, the magma became richer in mafic components and were then emplaced to form Fe-Ti-rich norites.

 
  • 大廟斜長(cháng)巖雜巖體的演化過(guò)程是:硅酸鹽母巖漿首先晶出大量的斜長(cháng)石晶體堆積形成斜長(cháng)巖。
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