位置:成果数据库 > 期刊 > 期刊详情页
位场曲化平的插值-迭代法
  • 期刊名称:地球物理学报
  • 时间:0
  • 页码:1811-1815
  • 语言:中文
  • 分类:P631[天文地球—地质矿产勘探;天文地球—地质学]
  • 作者机构:[1]浙江大学地球科学系,杭州310027
  • 相关基金: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(2006AA062107)资助.本文图3a,3b的资料.由中国国土资源航空物探遥感中心提供,特此致谢!
  • 相关项目:位场曲面延拓和大深度向下延拓的迭代法
中文摘要:

将起伏曲面B上的位场向下延拓至曲面最低点的平面A的插值一迭代法步骤是: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.这种插值一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.

英文摘要:

The interpolation-iteration procedure of downward continuation from the undulating surtace B to me 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.

同期刊论文项目
同项目期刊论文