摘要
六盘山盆地位于鄂尔多斯西南缘,文中通过六盘山盆地南部断裂变形及滑动矢量的详细观测,结合已有的资料,反演了六盘山盆地白垩纪变形历史。
The Liupanshan basin locates in the west southern erduosi, this text based on the observation of the south fault and slip vectors of Liupanshan basin joining with the data which hove got, makes the Liupanshan basin cretaceous period transform.
出处
《煤炭技术》
CAS
2007年第11期101-104,共4页
Coal Technology
关键词
六盘山盆地
早白垩纪
构造变形分析
Liupanshan basin
early cretaceous peoriod
structural deformation analysis
