首页 | 本学科首页   官方微博 | 高级检索  
     

长白山旅游区泥石流灾害研究
引用本文:孙平,王钢城,曹炳兰. 长白山旅游区泥石流灾害研究[J]. 世界地质, 2002, 21(2): 167-171,188
作者姓名:孙平  王钢城  曹炳兰
作者单位:吉林大学,建设工程学院,吉林,长春,130026
摘    要:长白山旅游区为泥石流灾害频发地段,从地貌形态来看,其主要类型为山坡型泥充,其形成条件主要包括三个方面:区内广泛分布的倒石堆为泥石流的形成提供了主要物质来源,陡峭的地形提供了动力条件,丰富集中的降雨是诱发因素,这三个条件相互影响,缺一不可。分析表明,本区泥石流的空间分布规律与倒石堆的发育状况密切相关。

关 键 词:泥石流 长白山 倒石堆 形成条件 发育特征
文章编号:1004-5589(2002)02-0167-05

Research On the Debris Flows Hazard in the Tourist Area of Changbai Mountain
SUN Ping,WANG Gang cheng,CAO Bing lan. Research On the Debris Flows Hazard in the Tourist Area of Changbai Mountain[J]. Global Geology, 2002, 21(2): 167-171,188
Authors:SUN Ping  WANG Gang cheng  CAO Bing lan
Abstract:The tourist area of Changbai Montain is a place where debris flows happen frequently. According to the geomorphologic conditions of debris flow activity, the principal type is hillslope type of debris flows. Its forming conditions are mainly as follows: wide range distributing talus is the material source, and the steep topography and plenty of rainfall are respectively the dynamic and inductive factors. Not a single one of these conditions can be dispensed with. Finally, it can be concluded that the spatial distribution of debris flow is interrelated with the developing condition of talus.
Keywords:debris flow  Changbai Mountain  talus  developing condition  formative characteristic
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号