摘要
由于以洒勒山滑坡为代表的高速远程型滑坡造成的巨大灾害及其形成机制的“神秘莫测”,引起了国内外不少学者对其形成机制进行研究的兴趣,陆续有若干论文见诸于世。作者发现,在部分论文中有将高速滑坡“扩大化”或将几种不同的地质现象混淆的情况,这将对研究工作的深入进展产生不利影响。为此,作者撰写本文阐述对这一问题的看法,提出将高速远程型坡体运动分成高速远程碎屑流、高速远程泥石流、高速远程滑坡三类,并提出了高速远程滑坡的判别指标和途径。
On behalf of the high speed and long distance landslide, Saleshan landslide aroused a large disaster and its formation mechanism was secret and unpredictable, so many scholars at home and abroad were interested in the research on the formation mechanism, and a number of pa-pers were presented one after another. The present author found that there were the expansion of high speed landslide or the confusion of various geological phenomena in some of them, which would exercise an unfavourable influence on the deepgoing research. For that, the present author wrote this paper in which an opinion was presented about this problem, and presented that the slope movement with high speed and long distance can be divided into three types as high speed and long distance sturzstrom, high speed and long distance debris flow, high speed and long distance landslide, as well as, a special method and way was presented for distinguishing high speed and long distance landslide
出处
《中国地质灾害与防治学报》
CSCD
1993年第4期3-8,共6页
The Chinese Journal of Geological Hazard and Control
关键词
滑坡
崩塌
泥石流
(干)碎屑流
高速
远程
landslide, rockfall, debris flow, sturzstrom, high speed, long distance
