通过对跨断层测量特点的分析，提出断层运动中趋势性成分具有反映区域地壳形变及应变能累积程度的意义。
By analyzing features of across fault measurement, the trend components of deformation can reflect the strength of strain energy accumulation in regional area.
基于连续介质力学理论，提出了直接利用GPS测量资料建立地壳运动与形变模型的方法。
Based on the theory of continuous medium mechanics, a method of establishing the model of crustal movement and deformation is presented completely with GPS data in this paper.
断层位错运动是地壳形变与密度变化耦合运动的特殊形式。
The fault dislocation and movement is a special form of the coupling movement between the crustal deformation and density change.
而地壳垂直形变场的时间权系数能够表示区域地壳运动的相对强弱，它可以作为区域地震危险性判定的时间判据。
The weight coefficients can indicate severity of crustal related movement in an area. It is one of the time criterion of earthquake region.
而地壳垂直形变场的时间权系数能够表示区域地壳运动的相对强弱，它可以作为区域地震危险性判定的时间判据。
The weight coefficients can indicate severity of crustal related movement in an area. It is one of the time criterion of earthquake region.
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