论文部分内容阅读
产于新疆东准噶尔红柳峡南扎曼苏-鲍尔先吉变形带中的鲍尔羌吉超单元以强烈塑性变形为特征，形成于加里东早期造山运动大陆孤环境，属壳幔混熔的I型花岗岩。
The Bauerqiang Jikun unit, which is produced in the southern Zhamansu-Bauer-Xianji deformation zone of Hongliuxia, eastern Junggar, Xinjiang, is characterized by strong plastic deformation. It was formed in the isolated orogeny of the Caledonian orogeny in continental China, Granite.