摘要
乌当地区平面上呈东西向展布的五条断层，其断层性质均为向南倾斜的逆冲断层，五条逆冲断层的扩展方式为由北向南依次形成的后展式，逆冲推覆构造的形成时间为三迭纪之后，白垩纪之前。
Five faults extenal in east-west direction of Wudang.They are characteri zed by thrust and southward dip.These thrusts consist in southward overstep propagation.The forming time of the thrust and nappe tectonics was somewhere between Triassic Period and Cretaceous Period.
出处
《贵州工业大学学报（自然科学版）》
CAS
1997年第2期23-26,共4页
Journal of Guizhou University of Technology(Natural Science Edition)
关键词
逆冲断层
迭瓦状构造
形成时代
推覆构造
thrust
imbricate structure
overstep propagation
forming time of fault
