小兴安岭晚石炭世花岗岩具有明显的岩浆混合特征。
Late Carboniferous granite in the Xiao Hinggan Mountains shows magma-mixing characteristics.
第一期为辉长质与花岗质岩浆混合，并生成闪长质岩石；
The first stage was mixing of gabbroic and granitic magmas, which formed dioritic rock;
同时，俯冲板块上深海沉积物与基性岩浆混合作用也是不容忽视的因素。
In addition, mixing between abyssal sediments on the subducted plate and basic magma is also a factor that can not be negligible.
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