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研究表明,通过对花岗质岩石中的镁铁质暗色包体的成因进行研究,对于深入认识岩浆源区性质、地球动力学背景以及壳、幔岩浆混合作用具有重要意义。含暗色镁铁质包体的中、晚三叠世花岗质岩石在青海祁漫塔格地区广泛分布(丰成友等,2012)。这些花岗质岩石与该区矽卡岩—斑岩型多金属矿
The study shows that the study of the genesis of mafic dark inclusions in granitic rocks is of great significance for understanding the properties of magma source areas, the geodynamic background and the mixing of crust and mantle magma. Mid- and late-Triassic granitic rocks with dark mafic inclusions are widely distributed in Qimantag area, Qinghai (Feng et al., 2012). These granitic rocks and skarn-porphyry-type polymetallic deposits in this area