摘要
在利用普通克里金方法外推的基础上,通过频域径向平均功率谱估算噪声方差,采用迭代维纳滤波法获取较为稳定的重力场向下延拓结果,并分别利用模拟算例和实际数据进行实验。对于模拟算例,外推后的均方根误差由6.72μGal下降到1.89μGal,相对误差由9.26%下降到4.44%。对于实际数据,外推后延拓结果不仅可避免边缘失真现象,而且能更好地反映浅源高频异常特征信息。
Based on ordinary Kriging extrapolation method,the noise variance is estimated by frequency radially averaged power spectrum,and then the downward continuation of stable gravity field is calculated by the iterative Wiener filter.The simulation example and actual data are separately used to do experiments.The accuracy of simulation example is significantly improved after extrapolation,the mean square error decreases from 6.72μGal to 1.89μGal,and the relative error decreases from 9.26%to 4.44%.The continuation result of actual data after extrapolation reflects the shallower anomaly information with high frequency better and avoids obtaining false values in the boundary.
作者
朱文武
彭军还
罗三明
陈敏
申成锋
李永昆
ZHU Wenwu;PENG Junhuan;LUO Sanming;CHEN Min;SHEN Chengfeng;LI Yongkun(School of Land Science and Technology,China University of Geosciences,29 Xueyuan Road,Beijing 100083,China;The First Monitoring and Application Center,CEA,7 Naihuo Road,Tianjin 300180,China;Qinghai Natural Resources Remote Sensing Center,13 Huanghe Road,Xining 810001,China;Qinghai Nonferrous First Geological Survey Institute,36 Jinhe Road,Xining 810007,China)
出处
《大地测量与地球动力学》
CSCD
北大核心
2020年第7期704-707,共4页
Journal of Geodesy and Geodynamics
基金
国家重点研发计划(2018YFC1503606)
中国地震局震情跟踪课题(2019010205)。
关键词
重磁位场
解析延拓
普通克里金
径向平均功率谱
维纳滤波
快速傅里叶变换
gravity and magnetic field
analytic continuation
ordinary Kriging
radially averaged power spectrum
Wiener filter
fast Fourier transformation