It is shown that current landslide mass of Yanzipin is still active.

分析结果表明，目前滑坡体仍在活动。

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By analyzing the geological condition in the area of the potential landslide, the contributing factor of potential landslide mass is put forward and its stability is checked.

通过对潜滑体区域地质情况的分析，指出了潜滑体的成因，并对其稳定性进行了验算，根据分析结果提出了相应的防治措。

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The loess landslide movement is a non stationary complex one combined with earth microtremors, the hydraulic gradient of high osmosis and strong shear force of landslide mass.

分析认为这种振荡曲线与地球自身的脉动有关，它是由地球脉动、高渗透水力坡降和大的滑体剪切作用叠加而成的一种呈非平衡态的复杂运动。

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