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地震地表破裂特征及其对应的分析方法
Characteristics of earthquake surface ruptures and related analytical methods
【摘要】 介绍了Kocaeli地震和集集地震的板块构造和区域地震的活动特性,及地震引起的地表破裂,提出了一种基于动力学和界面系统的、局部宏观尺寸的震源动力破裂过程分析方法。归纳出基于材料破坏分析基础的地震地表破裂的5种主要特征,应用材料和界面本构描述的控制方程稳定性讨论,阐明了地表破坏类型对应的力学机制,提出了相应的分析方法。
【Abstract】 Surface ruptures caused by strong earthquakes of Kocaeli and Chi-Chi,and local continental tectonics,earthquake activity are introduced here.A general method of source rupture progress is proposed based on a macroscopical dynamic system of discontinuous earth media and interfaces.For existent surface ruptures,5 main types are classified by in-situ survey and in general sense,which are shear strain localization,tensional break, shear fragmentized belt,plastic deformation zone,and liquefaction/lateral movement divisions.And related methods of those kinds of geomaterial failure of onset and evolution are proposed based on stability of governing equations with specified constitutive models.
【Key words】 surface failure; the stability of governing equations; shear strain localization; tensional failure; shear fragmentized belt; and liquefaction and lateral movement;
- 【文献出处】 世界地震工程 ,World Earthquake Engineering , 编辑部邮箱 ,2007年03期
- 【分类号】P315.2
- 【被引频次】8
- 【下载频次】157