| 6.16龙潭泥石流成因 |
| |
| 引用本文： | 卫宏. 6.16龙潭泥石流成因[J]. 太原理工大学学报, 2000, 31(3): 294-296,299 |
| |
| 作者姓名： | 卫宏 |
| |
| 作者单位： | 太原理工大学矿业工程学院 |
| |
| 摘 要： | ６．１６松潘龙潭泥石流是一种典型的雨后饱和松散坡只物没坡堰塞泥石流。对该泥石流的形成条件、成灾情况及动力学、运动学特征进行了研究，提出了防治对策。
|
| 关 键 词： | 泥石流 滑坡 崩积物 成因 龙潭泥石流 |
| 文章编号： | 1007-9432(2000)03-0294-03 |
The Cause of Longtan Debris Flow on June 16 1999 |
| |
| Wei Hong. The Cause of Longtan Debris Flow on June 16 1999[J]. Journal of Taiyuan University of Technology, 2000, 31(3): 294-296,299 |
| |
| Authors: | Wei Hong |
| |
| Affiliation: | College of Mining Engineering of TUT |
| |
| Abstract: | The 6 16 debris flow of Longtan on June 16, 1999 is a kind of typical landslide dammed debris flow formed by the loose slop washing and colluvium after rain,its forming conditions and dynamic and kinematic characteristics are studied,some protection measures of debris flow are pointed out. |
| |
| Keywords: | debris flow landslide dammed rocks |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
