白龙江流域滑坡与泥石流研究进展与展望

Xing-min Meng, Guan Chen, P. Guo, Muqi Xiong, Wasowski Janusz
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引用次数: 13

摘要

白龙江流域位于青藏高原、黄土高原和四川盆地的交汇处。它也是东西地震带和南北地震带的交叉点。由于地质构造复杂,该地区以陡坡、高相对起伏和深切割山谷为特征。分布广泛的弱岩和强降雨使该地区成为中国四大滑坡和泥石流灾害最严重的地区之一。本文根据现场调查资料和正在进行的研究项目,探讨了滑坡和泥石流的特征及其形成机制。还讨论了该地区监测和预警系统的管理以及灾害预防,目的是鼓励进一步研究该地区的地质灾害和减灾措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research of Landslides and Debris Flows in Bailong River BASIN:PROGRSS and Prospect
The Bailong River catchment is located in the intersection of Tibetan Plateau,Loess Plateau and Sichuan Basin.It is also the cross point of the east-west and north-south seismic zones.Due to complex geological structures,the region is characterized by steep slopes,high relative reliefs and deep incised valleys.Weak rocks,which are widely distributed,and heavy rainfalls made the region one of the four areas in China most severely affected by landslide and debris flow disasters.Based on the data from field investigation and on-going research projects,this paper deals with the characteristics of landslides and debris flows,and their genetic mechanisms.The management of monitoring and early-warning systems and hazard prevention in this region are also discussed,with the purpose to encourage further researches on geohazards and mitigation measures in the region.
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