摘要
与地震勘探一样,大地电磁勘探也存在着多次波与透过波干扰,研究这一问题对于大地电磁勘探资料的地质解释非常重要。本文从理论上分析了大地电磁拟地震解释中多次波的存在,指出了大地电磁测深电磁波反射函数中不存在多次波干扰而仅有上透过波干扰,导出了电磁波反射函数与上透过波干扰的数学关系,指出了压制上透过波干扰的选频办法。最后,用大地电磁拟地震解释法和电磁波反射函数延拓成像法对理论模型进行了计算,证实了前面的理论。
Similar with seismic prospecting,there exist multiple and proximity disturbances in magneto-electrotel-luric exploration(MTE).To study this problem is an important in geologic interpretation of MTE data.Theoretically,this study analyzed existence of multiple wave in pseudo seismic interpretation of MT,pointed out that no multiple interfer-ence appears in the magneto-electrotelluric sounding reflectance functions,and derived mathematical relations between the reflectance function and top proximity interference,giving the way of frequency-selecting for rejection of top proxim-ity interference.Finally,the theoretical model was estimated by using pseudo seismic interpretation of MT and electro-magnetic reflectance function continuation imaging methods for indicating effect of the theory.
出处
《新疆石油地质》
CAS
CSCD
2002年第2期117-120,共4页
Xinjiang Petroleum Geology
关键词
多次波
透过滤
压制方法
大地电磁测深
地震解释
成像
电磁波反射函数
上界面
下界面
magneto-electrotelluric sounding
seismic interpretation
continuation
imaging
electromagnetic reflectance function
upper interfacial effect
lower interfacial effect