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加权平滑边界元法重力反演
引用本文:毛小平 吴蓉元. 加权平滑边界元法重力反演[J]. 石油地球物理勘探, 1995, 30(4): 523-532
作者姓名:毛小平 吴蓉元
作者单位:中国地质大学(武汉)物探系
摘    要:对于三度界面的重力反演,应用边界元法(代数重建法ART解反演方程)求解时会出现边界振荡现象.本文分析了产生这一现象的原因,提出用加权平滑方法来克服边界振荡现象,并可加快迭代反演的收敛速度.理论和实测重力场的界面反演结果表明:加权平滑边界元反演方法效果良好,反演结果无边界振荡现象,优于其它近似的迭代反演方法,适用于实际生产.

关 键 词:重力反演  三度界面  反演方程  代数重建法  边界振荡  加权  平滑  
收稿时间:1994-10-17

Gravity inversion using weight-smoothed boundary element method
Mao Xiaoping,Wu Rongyuan. Gravity inversion using weight-smoothed boundary element method[J]. Oil Geophysical Prospecting, 1995, 30(4): 523-532
Authors:Mao Xiaoping  Wu Rongyuan
Affiliation:Department of Geophysical Exploration, China Geology University, Wuhan City, Hubei Province, Postcode:430074
Abstract:Boundary vibration phenomenon occurs in solving the gravity inversion of 3-D interfaces with the use of boundary element method(solving the gravity inversion equation by algebraic reconstruction technique). The origin of boundary vibration phenomenon is analysed here. Weight smoothing can be used to remove the boundary vibration phenoThenon and to cause fast convergence of iteration inversion. The inversion results of interfaces in both theoretical and real gravity fields show that the weight-smoothed boundary element method is better than other approximate iteration inversion methods and applies to practical work because it brings satisfactory inversion results without boundary vibration phenomenon.
Keywords:gravity inversion   three-dimensional interface   inversion equation  algebraic reconstruction technique   boundary vibration   weight  smooth
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