摘要
设计了位移形变模拟试验场并进行位移形变模拟试验,利用Bernese 5.0软件的单历元单点定位功能,处理并分析了位移模拟形变试验获取的1 Hz GPS数据。并以2008年5月12日汶川地震为例,获取了震中附近3个GPS站(成都、简阳和郫县)震前的短临位移过程及震后短时间的动态时变序列,结果显示各站的形变结果在时间上具有很好的一致性。利用动态时序的地震波到时和震中距离估计地震波地壳平均速度为3.17 km/s。
The experimental base for surface deformation simulation is designed and simulation test is carried out, and 1 Hz GPS data obtained from the simulation test is processed and analyzed with the single epoch single point positioning of the Bernese 5.0 software. Taking the Wenchuan earthquake on May 12,2008 as an example, we obtain the time series of the shortmpending displacement before the earthquake and shortly after the earthquake at 3 GPS stations：CHDU ,JYAN, PIXI. The results after data processing show good consistency among the deformation results at all stations in time. On the basis of arrival time of seismic wave recorded in kinematic time series and the distance between 1 Hz GPS stations and the epicenter, the estimated average velocity of seismic wave in the crust is 3.17 km/s.
出处
《大地测量与地球动力学》
CSCD
北大核心
2012年第B08期109-112,116,共5页
Journal of Geodesy and Geodynamics
基金
中国地震局地震行业专项(201101014)
关键词
高频GPS
地表形变
动态监测
单点定位
单历元解
high-rate GPS
surface deformation
dynamic monitor
single point positioning
single epoch positioning solution
