在磁法勘探解释和正反演计算,以及航磁数据(ΔT)换算三分量和磁化方向转换中,磁倾角是一个必不可少的重要参数。为了获取这个参数过去曾采用过不同的方法。例如:(1)采集大量的定向岩矿标本,经标本整形和精密测定,最后对测定结果进行计算、统计分析,得出有关的磁参数。(2)根据磁异常曲线计算出它们的理论值(有效磁化强度、有效磁倾角)。 Magnetic dip is an indispensable and important parameter in the interpretation and inversion of magnetic exploration, as well as the conversion of the three components of aeromagnetic data (ΔT) and the conversion of magnetization direction. In the past, different methods were used to get this parameter. For example: (1) Collect a large number of directional rock samples, the specimen shaping and precision measurement, the final calculation results of the calculation, statistical analysis, the relevant magnetic parameters. (2) According to the magnetic anomaly curve to calculate their theoretical value (effective magnetization, effective magnetic dip).