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位场曲化平的插值-迭代法
引用本文:徐世浙,余海龙.位场曲化平的插值-迭代法[J].地球物理学报,2007,50(6):1811-1815.
作者姓名:徐世浙  余海龙
作者单位:浙江大学地球科学系,杭州,310027;浙江大学地球科学系,杭州,310027
基金项目:教育部博士点基金项目(20050335090),国家自然科学基金项目(40774059),国家863计划项目(2006AA06Z107)资助
摘    要:将起伏曲面B上的位场向下延拓至曲面最低点的平面A的插值-迭代法步骤是:1)将曲面B上的场值放置在水平面A上具有相同水平坐标的点上,作为A上的初值;2)用若干水平面切割B,从A的初值,用快速傅里叶变换法(FFT)向上延拓出这些平面的场值,用插值的方法从这些平面的场值计算曲面B的场值;3)根据B上的实测值与计算值的差值,对A上的值进行加权改正;4)重复步骤2)和3),直到B上的差值小到可以忽略.这种插值-迭代法具有高的计算速度,比通常的FFT法延拓得更深,可以超过10倍点距.文中给出计算实例.

关 键 词:位场  向下延拓  插值  迭代  FFT  磁异常
文章编号:0001-5733(2007)06-1811-05
收稿时间:2007-2-9
修稿时间:2007-02-09

The interpolation-iteration method for potential field continuation from undulating surface to plane
XU Shi-Zhe,YU Hai-Long.The interpolation-iteration method for potential field continuation from undulating surface to plane[J].Chinese Journal of Geophysics,2007,50(6):1811-1815.
Authors:XU Shi-Zhe  YU Hai-Long
Institution:Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
Abstract:The interpolation-iteration procedure of downward continuation from the undulating surface B to the horizontal plane A that below the lowest point of B is:(1) choose the initial potential field value at each point on the plane A as the observed one on the surface B at the point with the same horizontal coordinates;(2) intersect the surface B with several planes and obtain the field values on these planes by upward continuing the fields on A using the FFT technique,then the fields on the surface B can be interpolated from the fields on these planes;(3) the new field values on A are then obtained by adding the initial values and the weighted difference between the observed and the calculated field values on B;(4) repeat steps(2) and(3) until the difference becomes negligible.The interpolation-iterative continuation method possesses a higher computation speed and can stably downward continue data to a much deeper depth than using standard FFT techniques,up a depth equal to more than 10 times the grid interval.A test example for real survey data is given.
Keywords:Potential field  Downward continuation  Interpolation  Iteration  FFT  Magnetic anomaly
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