理论模型和实际资料的反演结果表明，本方法是求解地球物理反问题的一种有效手段。
Theoretical model and real data inversion results show that the method is an effective means to solve geophysical inverse problem.
上述三种用于反演问题求解的算法已广泛地应用在地球物理求解中，已成为求解非线性反问题的有力数学工具。
The three algorithms mentioned above have been widely used in the solving of geo physical problems and are a powerful mathematical tool for nonlinear inversion problems.
分析了在理论模型、反演技术、综合解释上的成果与问题；指出了固体地球物理的复杂性。
The paper analyzes the results and problems in theoretical model, inverse technology and comprehensive interpretation, and points out the complexity of solid geophysics.
联合反演的优点就是比单一地球物理反演方法具有更高的分辨率，并且在一定程度上抑制了问题的多解性。
The joint inversion has better resolution and can more effectively resolve the problem of non-uniqueness than the inversion using only one geophysical method data.
尖锐边界反演是大地电磁及其他地球物理反演中的一个较难解决的问题，目前有不少专家正对这方面进行研究。
Sharp boundary inversion is a relatively difficult problem in magnetotelluric and other geophysical inversion , which has been studied by many researchers.
所得结果可应用于从地震表面波资料反演三维地球内部构造的地球物理问题。
The results can be applied in geophysics, used in 3-d earth's structure inv...
所得结果可应用于从地震表面波资料反演三维地球内部构造的地球物理问题。
The results can be applied in geophysics, used in 3-d earth's structure inversion from the seismic surface waves data.
所得结果可应用于从地震表面波资料反演三维地球内部构造的地球物理问题。
The results can be applied in geophysics, used in 3-d earth's structure inversion from the seismic surface waves data.
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