摘要
利用福清、泉州综合场地的水准复测资料,对该地区的重力复测资料进行地形变模型校正,得到大部分测点地形变影响量级≤10×10-8ms-2;GPS资料的处理结果表明,跨综合场地的三组断层由东向西运动逐渐减弱,其运动速率与华南块体的整体运动速率一致。
Using the leveling repetition data of Fuqing and Quanzhou comprehensive sites, the crustal deforma- tion of the regional repetition gravity data was corrected, the magnitude order of that effect is less than 10×10-8ms-2 . The processing results of GPS data show that the movement of three groups of faults across the comprehensive site decreased gradually from east to west, the movement velocity is the same as the southern China block.
出处
《大地测量与地球动力学》
CSCD
北大核心
2013年第A02期5-8,共4页
Journal of Geodesy and Geodynamics
基金
厦门地震勘测研究中心基金(2011)
关键词
综合场地
流动重力测量
水准
地形变
GPS
comprehensive site
repeated gravity measurements
leveling
crustal deformation
GPS