石碑塬滑坡成因机制及数值模拟初步分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
通过对1920年海原大地震造成的石碑塬滑坡区域地质条件和基本特征的现场调查,推测出石碑塬滑坡的边界、形成原因及破坏过程,并通过数值模拟分析其原始斜坡在地震作用时的位移、应变等特征。
In this paper,an on-site investigation on the geological conditions and basic characteristics to Shibeiyuan landslide area impacted by Haiyuan earthquake in 1920 has been made.We infer the boundary,formation causes,and failure process of Shibeiyuan landslide,and analyze its original slope displacement,strain and other characteristics by the action of earthquake through numerical simulation.
引文
[1]王家鼎,白学铭,肖树芳.强震作用下低角度黄土斜坡滑移的复合机理研究[J].岩土工程学报,2001,23(4):445-448.
    [2]白学铭.高烈度地震时黄土层的液化移动[J].工程勘察,1990(6):1-5.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心