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以往有关重磁异常谱反演方法的文章重点多集中于讨论单个模型,研究组合磁异常谱反演方法的文章不多.但实际生产中经常遇到叠加矿体的情况,所以研究组合磁异常的反演方法是很有必要的.与空间域方法相比,波数域方法具有公式简洁明了,各参量易于分离等优点.本文在对二维组合磁异常波谱进行分析的基础上提出用伪波谱对组合磁异常进行反演的新方法.
In the past, the article focused on the inversion of gravity and magnetic anomaly mainly focus on the discussion of a single model, the study of composite magnetic anomaly spectrum inversion method is limited, but the actual production often encounter superimposed ore body, so the study of magnetic anomaly Compared with the space domain method, the wave number domain method has the advantages of concise formula, easy separation of each parameter, etc. Based on the analysis of the two-dimensional composite magnetic anomaly spectrum, A new method of inversion of composite magnetic anomalies.