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根据福建省境内１９７２年以来两次精密水准复测资料，利用速率面拟合法研究福建省现今地壳垂直运动的特征，并结合本区地质构造和地震活动性探讨这种运动的地球物理意义。资料分析表明，本区内新华夏系构造带是强震活动的主要场所，强震活动地点则又受到与这些新华夏系构造交汇的次一级的东西向构造、北西向构造和环状构造活动的制约；在主要构造断块的交接带上则表现为较显著的地壳垂直运动的差异性，差异活动较强烈的地区与本区地震活动的分布特征有着良好的一致性，且地震均落在地壳垂直运动速率变化较大的地区或其邻近海域
According to the data of two precision leveling rehearsal tests since 1972 in Fujian province, the velocity face fitting method is used to study the current crustal vertical movement in Fujian Province. The geophysical significance of this movement is discussed based on the geological structure and seismicity in this area. Data analysis shows that the Xinhuaxia tectonic belt in this area is the main site of strong earthquake activity and the strong earthquake activity sites are sub-level east-west tectonics and NW-trending and ring structures The difference of vertical movement of the crust on the transition zone of the main tectonic fault blocks shows a significant difference in the vertical movement of the crust. There is a good consistency between the distribution of seismic activity in the regions with strong differential activity and the distribution of the seismic activity in this area, In the area where the rate of vertical crustal movement changes greatly or in the adjacent sea area