摘要
<正>组成复式岩基的有镁铁质暗色岩浆包体(mafic magmatic enclaves,MME)发育的钙碱性(I型)花岗岩,及其伴生的少量块状镁铁质侵入体的成因,以及复式岩基中该岩石组合的意义和其形成地球动力学模型的认识,仍然是国际学术界争议的热点,如复式岩基中I型花岗岩混合成因问题,岩石成因模型对应的大陆地壳生长方式等。阿拉善地块北部雅布赖-诺尔公-红古尔玉林构造带广泛出露二叠纪的I型花岗岩(其中广泛发育MME)和伴生的少量辉长岩侵入体组成的复式岩基,是研究复式岩基
引文
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