断层的真位移矢量可以分解为走向滑距和倾向滑距两个分量，前者简称走滑，后者简称倾滑。大多数断层兼有走滑和倾滑组分，即斜向滑动。
断层位移可能是垂直的、平行的、或者是两者的综合。
The fault displacement may be vertical, horizontal, or any combination of these.
本文首先给出了北京地区若干跨断层位移测量结果的年周期变化。
This paper gives first the annual periodic variations in the geodetic data obtained from several observation stations for fault displacements in the Beijing region.
为了计算方便，我们简化了曼辛哈和斯迈里断层位移场的解析表达式。
For convenience of calculations, We simplify the mansinha and smylie analytic expressions for the fault displacement field.
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