[1]陈自生.高位滑坡的运动转化形式[J].山地学报,1992,(04):225.
点击复制

高位滑坡的运动转化形式()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
1992年04期
页码:
225
栏目:
山地学报
出版日期:
1992-12-30

文章信息/Info

作者:
陈自生
中国科学院、水利部成都山地灾害与环境研究所
关键词:
高位滑坡崩塌碎屑流动碎屑滑动泥石流
文献标志码:
A
摘要:
高位滑坡剪出口高于坡脚,它一旦滑离滑坡发生区,运动可能转化成四种形式:1.崩塌:由滑体经分级解体滑过剪出口处依次向前倾倒而成;2.碎屑流动或3.碎屑滑动:由滑动块体经碎屑化而成;4.泥石流:在适当的细粒物质量和水体条件下生成的碎屑流动。

相似文献/References:

[1]罗永忠.“4·20”芦山地震震中龙门乡地质灾害特征[J].山地学报,2014,(01):124.
 LUO Yongzhong.Characteristics of Geological Hazards in Longmen Township by “4·20” Lushan Earthquake,China[J].Mountain Research,2014,(04):124.
[2]王东坡,何思明,葛胜锦,等.“9?07”彝良地震诱发次生山地灾害调查及减灾建议[J].山地学报,2013,(01):101.
 WANG Dongpo,HE Siming,GE Shengjin,et al.Mountain Hazards Induced by the Earthquake of Sep 07,2012 in Yiliang and the Suggestions of Disaster Reduction[J].Mountain Research,2013,(04):101.
[3]崔鹏,陈晓清,张建强,等.“4·20”芦山7.0级地震次生山地灾害活动特征与趋势[J].山地学报,2013,(03):257.
 CUI Peng,CHEN Xiaoqing,ZHANG Jianqiang,et al.Activities and Tendency of Mountain Hazards Induced by the Ms7.0 Lushan Earthquake,April 20,2013[J].Mountain Research,2013,(04):257.
[4]高延超,陈宁生,徐如阁,等.芦山地震中G318线天全段崩塌发育规律[J].山地学报,2013,(05):632.
 GAO Yanchao,CHEN Ningsheng,XU Ruge,et al.Development and Distribution of Collapses Induced by“4?20”Lushan Earthquake:Taking Tianquan Section of China National Highway 318 as a Sample[J].Mountain Research,2013,(04):632.
[5]常鸣,唐川,李为乐,等.汶川地震区绵远河流域泥石流形成区的崩塌滑坡特征[J].山地学报,2012,(05):561.
 River Basin,ChinaCHANG Ming,TANG Chuan,et al.The Characteristic of Collapse and Landslide by Wenchuan Earthquake in Debris Flow for Mative Region along the Mianyuan[J].Mountain Research,2012,(04):561.
[6]陈自生,张晓刚.1994-04-30四川省武隆县鸡冠岭滑坡→崩塌→碎屑流→堵江灾害链[J].山地学报,1994,(04):225.
[7]唐邦兴,柳素清,刘世建.我国山地灾害及其防治[J].山地学报,1996,(02):103.
[8]胡卸文,陈明东,刘汉超,等.金沙江向家坝库区崩滑灾害的环境效应[J].山地学报,1996,(03):205.
[9]柴宗新.山地灾害概念之我见[J].山地学报,1999,(01):92.
[10]李锦育.台湾崩塌地的分类与防治工法[J].山地学报,2001,(05):425.

更新日期/Last Update: 1992-12-30