方荣新, 施闯, 陈克杰, 徐培亮. GPS地震仪:PANDA软件测试结果与验证[J]. 武汉大学学报 ( 信息科学版), 2011, 36(4): 453-456.
引用本文: 方荣新, 施闯, 陈克杰, 徐培亮. GPS地震仪:PANDA软件测试结果与验证[J]. 武汉大学学报 ( 信息科学版), 2011, 36(4): 453-456.
FANG Rongxin, SHI Chuang, CHEN Kejie, XU Peiliang. GPS Seismometer:PANDA Software Testing Results and Validation[J]. Geomatics and Information Science of Wuhan University, 2011, 36(4): 453-456.
Citation: FANG Rongxin, SHI Chuang, CHEN Kejie, XU Peiliang. GPS Seismometer:PANDA Software Testing Results and Validation[J]. Geomatics and Information Science of Wuhan University, 2011, 36(4): 453-456.

GPS地震仪:PANDA软件测试结果与验证

GPS Seismometer:PANDA Software Testing Results and Validation

  • 摘要: 介绍了基于PANDA软件的高采样率GPS数据非差精密定位方法,为了验证高采样GPS技术与地震仪观测结果的一致性,进行了震动平台模拟数据试验。试验结果表明,高采样GPS和地震仪均能有效地恢复平台震动位移和震动主频率。对2010年Baja地震实际观测的GPS和强震仪进行分析,结果表明,利用高采样GPS技术不仅能成功获取地震波信号;而且能同时获得地表永久形变信息;而地震仪只能获取地震波信息,而不能直接获得地表永久形变信息。

     

    Abstract: In this paper,high-rate GPS data are processed using the non-difference precise positioning technique in PANDA package.It has shown that the high-rate GPS processed results are consistent with seismometer observations.Furthermore,the simulated vibration data and real observing seismic data during the Baja earthquake on 4 April,2010 are employed to test its validation.The high-rate GPS data could successfully capture the consistent seismic wave signal and permanent offset of ground deformation,while seismometer could only obtain the seismic wave.

     

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