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时间:2019-03-19
《浅论贵州典型岩层组合层状边坡失稳机理及稳定性评价理论研究——以牟珠洞滑坡为例》由会员上传分享,免费在线阅读,更多相关内容在学术论文-天天文库。
1、分类号:TU457密级:公开论文编号:2006090583贵州大学2009届硕士研究生学位论文贵州典型岩层组合层状边坡失稳机理及稳定性评价理论研究—以牟珠洞滑坡为例学科专业:岩土工程研究方向:边坡工程导师:宋建波教授研究生:闫建中国·贵州·贵阳2009年5月目录目录····················································································································I摘要········
2、··········································································································IIIAbstract·················································································································IV1绪论·························
3、························································································11.1选题依据及研究意义·························································································11.2国内外研究现状···························································
4、····································21.2.1层状岩质边坡失稳机理··············································································21.2.2层状岩质边坡稳定性评价···········································································41.2.3层状岩质边坡数值模拟技术····················
5、····················································61.3研究思路与方法·······························································································61.3.1研究思路····························································································
6、····61.3.2研究方法································································································82贵州典型岩层特征··································································································92.1概述····································
7、·······································································92.2层状岩体形成条件及成岩作用·············································································92.2.1层状岩体形成条件特征············································································102
8、.2.2层状岩体成岩作用··················································································102.3层状岩体结构及力学特征······································································
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