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某顺层岩质斜坡倾倒的成因机制研究

Study on formation mechanism of toppling of a consequent rock slope

中文摘要英文摘要

顺层岩质斜坡是常见的斜坡结构类型之一,一般认为顺层岩质斜坡的变形破坏以缓倾斜坡中发生整体顺层下滑和中-陡倾斜坡中发生溃屈破坏为主,对此类变形破坏特征和形成机理研究已较深入。通过现场调查和查阅国内外文献发现,顺层岩质斜坡中也存在一种倾倒变形破坏方式。以黄河上游某水电站库区顺层岩质斜坡坡脚处倾倒变形破坏为实例,结合该斜坡所处的地质环境及其变形破坏特征,分析其形成条件和演化过程。

onsequent rock slope is one of common type of slope structure. In place to reduce the overall tilt of bedding down and buckling failure of in steep slope are regarded as the main features of deformation and failure of consequent rock slope. Deformation and failure of such features and formation mechanism has been studied more in-depth. A number of field surveys and many literatures from domestic and abroad indicate that there is also a way of dumping deformation in consequent rock slope. According to the toppling of deformation and failure characteristics of the foot of a bedded rock slope, which is located in the reservoir region of a hydropower station on upper reaches of the yellow river, combining the geological conditions and the characteristics of the formation and failure, formation condition and evolutionary process of the slope are analyzed in this paper.

刘高、石瑞红、李高勇

地质学灾害、灾害防治

顺层岩质斜坡倾倒形成条件演化过程

Bedded rock slopeMulti-level bucklingMechanismMechanics analysis

刘高,石瑞红,李高勇.某顺层岩质斜坡倾倒的成因机制研究[EB/OL].(2012-05-16)[2025-08-11].http://www.paper.edu.cn/releasepaper/content/201205-275.点此复制

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