首先概略地介绍了国内外具有较高理论价值的重磁勘探正反演理论前沿性研究成果，并给予了适当的对比评述。
The paper summarily introduces the advanced research results which are of theoretical importance in the forward and inverse problems in gravity magnetic exploration, and provides an adequate review.
提出了一种新的基于统计推断的重磁震联合反演方法。
A novel gravity magnetic seismic combination inversion method based on statistical inference was proposed.
因此，研究应力波与裂隙的相互作用，对于研究岩石爆破机理、应力波传播规律以及波的反演——材料的动态特性等有着十分重要的意义。
Therefore the study of interaction of stress waves with cracks will greatly contribute to the interpretation of blasting mechanism, the stress wave propagation and the dynamic behaviour of material.
地表粗糙度的标定对于利用微波辐射计数据反演地表参数而言是十分重要的工作。
Calibration for the soil roughness parameters is very important for land surface parameters retrieval with radiometer.
重磁线性反演最后都要归结于解数据方程。
The gravitational and magnetic linear inversion should be finally ended in the solution data equations.
本文采用重磁力联合反演方法，计算了民和盆地基底深度和视磁化强度。
In this paper, combined gravity and magnetic inversion method of potential field is applied to the calculation of the basement depth and apparent magnetization in the Minghe basin.
介绍一种重、磁界面计算的广义反演方法。
In this paper, the generalized inversion method on the computation of gravity and magnetic interfaces is presented.
本文主要介绍了作者所研制的人机联作重磁资料反演系统。
An interactive computer program for inversion of gravity and magnetic anomaly is presented.
沿剖面完成了重磁联合反演，获得了岩石圈二维密度结构与二维磁性结构。
Along the profile a joint inversion of gravity with geomagnetism has been carried out and 2-d density structure and 2-d geomagnetic structure have been obtained.
对于重磁力三维勘探而言，数据采集、地形改正和三维正反演法已逐步走向实用；
So far as 3D gravity and magnetic survey is concerned, the data acquisition, topographic correction and 3D forward and inversion methods are gradually practical;
对于重磁力三维勘探而言，数据采集、地形改正和三维正反演法已逐步走向实用；
So far as 3D gravity and magnetic survey is concerned, the data acquisition, topographic correction and 3D forward and inversion methods are gradually practical;
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