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.
该文提出利用断层位移模式从观测的断层位移数据中分析断层发育史。
By utilizing the model of fault displacements, a method to study the history of faults based on observed data of fault displacement was proposed.
本文采用观测值曲线的分段拟合方法，对北京地区部分断层位移测量资料进行处理。
Using separation stage for fitting of observational curves in this paper, the surveying data of fault displacements of Beijing area has been analyzed.
一般说来，地壳介质是不均一的，因而温度对跨断层位移测量的干扰是不容忽视的。
However crustal media, in general, are inhomogenous, therefore temperature influence on displacement measurements across faults, should not be ignored.
跨断层测量的复测周期主要由观测精度和断层位移速度决定，二者合理匹配的周期就是最佳周期。
A repeated period of measurement across the fault is mainly determined by observation accuracy and rate of deformation. It is the best period for they to match reasonably.
跨断层测量的复测周期主要由观测精度和断层位移速度决定，二者合理匹配的周期就是最佳周期。
A repeated period of measurement across the fault is mainly determined by observation accuracy and rate of deformation. It is the best period for they to match reasonably.
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