In the middle of the research area, the ductile shear zone was developed; it was possibly the identical structural system root belt with Xuniwusu fault, which belonged to the deeper tectonic level.
3.研究区中部发育的韧性剪切带,与徐尼乌苏逆冲断层可能是同一构造体系的根带,属于较深构造层次。
参考来源 - 内蒙古中部白音希勒地区构造特征及其演化·2,447,543篇论文数据,部分数据来源于NoteExpress
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