[1]樊晓一,王成华,乔建平.两龙滑坡特征及转化泥石流机制分析[J].水土保持研究,2005,12(06):156-158.
　FAN Xiao-yi,WANG Cheng-hua,QIAO Jian-ping.Feature of Lianglong Landslide and the Mechanism Analysis of Landslide-induced Debris Flow[J].Research of Soil and Water Conservation,2005,12(06):156-158.
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两龙滑坡特征及转化泥石流机制分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 12 期数: 2005年06期 页码: 156-158 栏目: 出版日期: 1900-01-01
Title:
Feature of Lianglong Landslide and the Mechanism Analysis of Landslide-induced Debris Flow
作者:
樊晓一1,2, 王成华1, 乔建平1
1. 中国科学院水利部成都山地灾害与环境研究所, 成都, 610041;
2. 中国科学院研究生院地球科学学院, 北京, 100039
Author(s):
FAN Xiao-yi1,2, WANG Cheng-hua1, QIAO Jian-ping1
1. Institute of Mountain Hazards & Environment, Chinese Academy of Science and Ministry of Water Conservancy, Chengdu, 610041, China;
2. School of Earth Science, Graduate School of Chinese Academy of Science, Beijing, 100039, China
关键词:
两龙滑坡; 运动特征; 形成机理
Keywords:
Lianglong landslide; movement feature; formative mechanism
分类号:
P642.24;P642.2
摘要:
从两龙滑坡发育的阶段性特征出发,根据滑坡在滑动过程的特征,将滑坡的运动特征划分为主滑区、流化区和流动区.分析了滑坡转化为泥石流的形成机理.并对四川盆地盆周山区地质灾害提出减灾防灾措施和建议.
Abstract:
From Lianglong landslide growth stage feature,and according to characteristic of the sliding process,the movement feature was divided into main sliding zone,liquid state zone and flowing zone.It analyzed the formative mechanism of landslide-induced debris flow,and brought forward the measure and advice about the geologic hazard around Sichuan basin.

参考文献/References:

[1] 乔建平.滑坡减灾理论与实践[M].北京:科学出版社,1997.28-41.
[2] 谢洪,王成华,林立相.标水岩沟滑坡型泥石流灾害及特征[J].中国地质灾害与防治学报,2000,11(3):20-22.
[3] 徐永年,等.崩塌土流动化机理的实验研究[J].水利学报,2002,(10):87-90.

相似文献/References:

[1]胡桂胜,陈宁生,李俊,等.金沙江白鹤滩水电站坝址近场区泥石流运动特征与发展趋势分析[J].水土保持研究,2014,21(02):238.
　HU Gui-sheng,CHEN Ning-sheng,LI Jun,et al.Research on Dynamic Characteristics and Development Tendency of Debris Flow Near Field Region in Baihetan Hydropower Station, Jinshajiang River[J].Research of Soil and Water Conservation,2014,21(06):238.

备注/Memo

收稿日期:2005-1-6。
基金项目:中国科学院水利部成都山地灾害与环境研究所应急基金
作者简介:樊晓一(1974- ),男,四川双流人,博士研究生,从事滑坡预测预报及危险度评价研究.

更新日期/Last Update: 1900-01-01