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任意密度分布复杂地质体重力异常快速三维正演方法

陈轻蕊 陈龙伟 戴世坤 张钱江 欧阳芳

物探化探计算技术2017,Vol.39Issue(2):176-182,7.
物探化探计算技术2017,Vol.39Issue(2):176-182,7.DOI:10.3969/j.issn.1001-1749.2017.02.04

任意密度分布复杂地质体重力异常快速三维正演方法

Three-dimensional forward modeling method for gravity anomalies of complex geological bodies with arbitrary density distribution

陈轻蕊 1陈龙伟 2戴世坤 1张钱江 1欧阳芳1

作者信息

  • 1. 中南大学 地球科学与信息物理学院,长沙 410083
  • 2. 桂林理工大学 地球科学学院,桂林 541006
  • 折叠

摘要

Abstract

Rapid three-dimensional (3D) forward modeling of gravity anomalies of complex geologic bodies with arbitrary density distribution plays an important role on 3D inversion of gravity and human-computer interaction modeling and interpretation.This paper proposes a wavenumber domain 3D forward modeling method.This new method has three key aspects: (1) prism based subdivision strategy.The research area is divided into many small regular prisms, density for each small prism can be given arbitrarily, in order to simulate complex geological body with arbitrary density distribution and undulating topography;(2) new wavenumber domain formula for computing gravity anomaly of combined prism model;(3) Gauss-FFT method.This paper uses Gauss-FFT method to transform the gravity anomaly from the wave number domain to the spatial domain.The Gauss-FFT method not only has high computational efficiency, but also suppresses the boundary effect and avoids the singular problem at zero wavenumber caused by the traditional FFT method.Numerical tests show that the proposed method is fast and accurate.It takes only a few seconds to calculate gravity anomaly for the combined 3D model with millions of prisms.

关键词

重力异常/三维正演/Gauss-FFT/积分方程

Key words

gravity anomalies/three-dimensional forward modeling/Gauss-FFT/integral equation

分类

天文与地球科学

引用本文复制引用

陈轻蕊,陈龙伟,戴世坤,张钱江,欧阳芳..任意密度分布复杂地质体重力异常快速三维正演方法[J].物探化探计算技术,2017,39(2):176-182,7.

基金项目

国家自然科学基金项目(41404106) (41404106)

物探化探计算技术

OACSCDCSTPCD

1001-1749

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