[1]陈自生,李沛,任连城.金龙山地区滑坡研究[J].山地学报,1991,(04):210.
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金龙山地区滑坡研究()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
1991年04期
页码:
210
栏目:
山地学报
出版日期:
1991-12-31

文章信息/Info

作者:
陈自生;李沛;任连城
中国科学院、水利部成都山地灾害与环境研究所 ;中国科学院、水利部成都山地灾害与环境研究所 ;二滩水电开发公司
关键词:
金龙山; 滑坡; 蠕滑; 滑面
文献标志码:
A
摘要:
金龙山地区位于四川省雅砻江二滩水电站库首左岸。区内海拔1000—2700米;重点研究区海拔<1730米,面积近1.3平方公里。本区滑坡顺层发育,以蠕滑方式为主,成条成群分布,新老俱全,厚度各异(巨厚—表层),规模不一。控制坡体蠕滑和滑动的主要是层面(或似层面)、层间错动带和中缓倾角裂隙。据滑坡活动状况的不同,将全区分为三个滑坡区:Ⅰ区是多级古滑坡区(方量约200万立方米);Ⅱ区是蠕滑区(方量约2000万立方米);Ⅲ区是浅-表层残坡积层滑坡区。

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[11]李沛,陈自生.金龙山地区滑坡综合观测方案概述[J].山地学报,1991,(04):244.

更新日期/Last Update: 1991-12-31