影响黄土地区地震崩滑敏感性的宏观因素包括活动地质构造、地震断层、地层、地形、水文条件、地震强度等。
The macroscopic factors influencing sensitivity of seismic loess landslides include geological structure, seismic fault, stratum, topography, hydrological condition, seismic intensity etc.
现代地形资料可资鉴定断层活动性。
Recent topographic data are useful for identification of fault activity.
结果显示，隧址区的最大主压应力及最大剪应力分布主要受地形和断层的控制。
The results show that the distributing of the maximum principal stress and maximum shear stress are mainly under the control of the landform and fault.
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