| 贵阳市乌当地区逆冲推覆构造的特征分析 |
| |
| 引用本文： | 范晓华 杜定全. 贵阳市乌当地区逆冲推覆构造的特征分析[J]. 贵州工业大学学报(自然科学版), 1997, 26(2): 23-26 |
| |
| 作者姓名： | 范晓华 杜定全 |
| |
| 作者单位： | 贵州工业大学资源工程系 |
| |
| 摘 要： | 乌当地区平面呈东西向展布的五条断层，其断层性质均同南倾斜的逆冲断层，五条逆冲断层的扩展方式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。
|
| 关 键 词： | 逆冲断层 迭瓦状构造 形成时代 推覆构造 |
CHARACTERISTIC ANALYSIS OF THRUST AND NAPPE TECTONICS IN WUDANG,GUIYANG |
| |
| Fan Xiaohua Du Dingquan Zhou Hongqing He Fengsheng Mao Jiaren. CHARACTERISTIC ANALYSIS OF THRUST AND NAPPE TECTONICS IN WUDANG,GUIYANG[J]. Journal of Guizhou University of Technology(Natural Science Edition), 1997, 26(2): 23-26 |
| |
| Authors: | Fan Xiaohua Du Dingquan Zhou Hongqing He Fengsheng Mao Jiaren |
| |
| Abstract: | 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. |
| |
| Keywords: | thrust imbricate structure overstep propagation forming time of fault |
| 本文献已被 CNKI 维普 等数据库收录！ |
