摘要
大青山逆冲推覆构造发育在石拐断陷盆地南侧，由一系列规模大小不等向南倾的叠瓦状逆冲推覆断层构成，由南南西向北北东方向推覆，是单冲型逆冲推覆构造。由北向南分为前缘挤压滑脱构造带、斜歪倒转褶皱—逆冲断层带和逆冲推覆岩席及叠瓦状逆冲断层带。
The Daqingshan thrust is develop on the southern margin of Shiguai fault basin. As a solely thrusting type,the thrust belt consists of a set of south dipping reverse faults.From north to south,several tectonic belts can be distinguished:front compressive detachment belt,overturned thrusting belt,sheeted thrusting belt and imbricate thrusting belt.
出处
《中国区域地质》
CSCD
1999年第4期366-372,共7页
Regional Geology of China
基金
原地质矿产部内蒙古大青山地区6 幅1:5 万区调项目
