摘要
运用大陆造山带填图方法 ,首次对雪山断裂带进行了系统研究 ,认为雪山断裂带为构造混杂岩带 ,其南北边界清楚 ,内部由 14个大小不同的构造岩片 (或岩块 )混杂堆积组成 ,其微观及变形特征清楚。
Application of continental orogenic zone mapping method to firstly systematical study of the Xueshan fracture zone. The study indicates that the Xueshan fracture zone is a boundary-definite tectonic melange zone consisting of 14 various tectonic melange sheets (blocks) in size characterized by obvious deformation.
出处
《四川地质学报》
2001年第4期199-204,共6页
Acta Geologica Sichuan
