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在 1∶2 5万马鬃山幅区调填图和方法研究工作中 ,通过观察到的一些与岩浆混合模式相关的现象 ,指出暗色微粒镁铁质包体是岩浆混合作用的有利证据 ,讨论了与花岗岩侵入体相关的镁铁质小岩体混合成因的可能性 ,认为岩浆混合作用在造山带岩浆活动中是一种极为普遍的现象。
In the study of 1: 25000 Mazongshan amplitude maps and methods, it is pointed out that the dark-colored mafic inclusions are favorable evidences for magma mixing through the observation of some phenomena related to magma mixing patterns. The possibility of mixed mafic small rock mass associated with granite intrusions suggests that magmatic mixing is an extremely common phenomenon in orogenic magmatism.