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磁模拟方法是勘探地球物理评价磁异常中的一种新方法。1981年治金部中南冶金地质研究所研制成功一套磁模拟系统投入使用后,来自生产、科研、大专院校的同志带着有关的科研项目在该所进行实验,从实践中寻求解决有关的地质和地球物理问题的新途径。当前主要是用以解释那些复杂形态、非均匀磁化三度地质体或多层地质体组合在一起所引起的复杂磁异常。有
Magnetic simulation method is a new method of exploration of geophysical evaluation of magnetic anomalies. After successfully completing a set of magnetic simulation system in 1981 by the Ministry of Metallurgical and Metallurgy of the Ministry of Metallurgy, comrades from production, scientific research and tertiary institutions took relevant scientific research projects to carry out experiments in the institute and sought to solve the problems in practice New Approaches to Geological and Geophysical Issues. At present, it is mainly used to explain the complex magnetic anomalies caused by the combination of complex shapes, heterogeneous magnetized tertiary geologic bodies or multi-layered geological bodies. Have