摘要
大地电磁测深法中的静位移是国内外专家十分关注的问题,虽然提出了多种解决方案,但各种方法都有其效果与弊端.从大地电磁场基本理论出发,讨论了大地电磁测深法及其衍生方法的静位移问题,并提出了一种改进的大地电磁场静位移校正方法,利用最优估计和迭代的思路将平面聚类法和首枝重合法结合起来,解决不同成因产生的静位移效应,并使其完善为能够实现大规模资料处理的方法.使用理论模型响应验证了该方法的正确性,并且通过实测数据的应用结果与已知信息的对比分析,验证了方法的有效性.
The static shift of MT exploration is the issue concerned by domestic and foreign experts,and many correction methods were proposed.But each method has its advantages and disadvantages.In this paper,the static shift of MT and its derivative methods is discussed from the basic theory,and a joint correction method is proposed using the improved plane Hanning window weighting and the first branch coincidence methods.The optimal estimation and iterative methods are used to combine the correction methods for static shift problems with different formations,and the correction method is consummated for realizing large-scale data processing.The correctness of the correction method is verified using the synthetic sounding.And the effectiveness is verified by the comparison of the application results with real data and priori information.
出处
《地球科学（中国地质大学学报）》
EI
CSCD
北大核心
2016年第5期864-872,共9页
Earth Science-Journal of China University of Geosciences
基金
中国地质科学院矿产资源研究所2013年度基本科研业务费专项资金项目(No.K1318)
中国地质调查局地质调查项目(No.12120114053301)
关键词
静位移校正
大地电磁场
首枝重合
平面聚类
最优估计
地球物理
static shift correction
magnetotelluric
coincidence first branch
plane clustering
optimal estimation
geophysicals
