中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
狮子山滑坡群和宝鸡峡塬边渠道滑坡成因机制初探——易滑地层与有效临空面研究的实际意义例证

文献类型:会议论文

作者卢螽槱
出版日期1984-05
会议名称四川省滑坡研究及防治经验交流会
会议日期1983-1
会议地点四川成都
关键词滑坡 成因 狮子山滑坡群 宝鸡峡塬边渠道滑坡
页码130-134
其他题名A Preliminary research on the Forming Mechanisms of Shizishan Landsilde Group and Landslides Along the Irrigation Ditch on the Edge of the Loess Piateau Near Baojixiao——Expamples Showing the Actual Effect of the Research on Slide Favourable Strata and Effective Slopes Facing the Air
通讯作者卢螽槱
中文摘要本文旨在通过对成都狮子山滑坡群和宝鸡峡引滑工程塬边渠道滑坡成因机制分析,以检验对于易滑地层和有效临空研究所形成的认识。
英文摘要The paper puts forward new understanding of the forming mechanem of Shizishan Landslide Group along Chengdu-Kunming Railay and landslides along the Irrigation Ditch on the Edge of Loess Plateau near Baojixia through analiysing the data about them. The author considers that those landslides are controlled by the slide-favourable strata and effective slopes facing the air. It means the slpoes are high up in the air. There are two kinds of slide-favourable strata which have different characteristics——Chengdu Clay (Q3) and liading Res Shale (K2) in Shizishan Region, Chengdu. So, two kinds of strata in the region along the Irrigation Dich on the Edge of the Loess Plateau near Baojixia, landslides are controlled by two kinds of them——Yellow Alluvial Mild Clay (Q1) and Red Clay (N2). So, the characteristics of the two kinds of landslides are different from each other. It is pointed out that the effective slopes facting the air in Shizishan Region are provided by cutting. The effective slopes facting the air for the landslides along the Irrigation Ditch on the Edge of the Loess Plateau are provided by rayer erosion.
会议主办者四川省地理学会滑坡专业委员会;中国科学院成都地理研究所
会议录滑坡分析与防治
会议录出版者科学技术文献出版社重庆分社 ; 重庆
会议录出版地重庆
语种英语
ISBN号12176·32
源URL[http://ir.imde.ac.cn/handle/131551/17457]  
专题成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前)
作者单位中国科学院成都地理研究所
推荐引用方式
GB/T 7714
卢螽槱. 狮子山滑坡群和宝鸡峡塬边渠道滑坡成因机制初探——易滑地层与有效临空面研究的实际意义例证[C]. 见:四川省滑坡研究及防治经验交流会. 四川成都. 1983-1.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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