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引言当前,在航磁数据处理工作中,化向磁极的处理比较普遍地得到应用,在某些地区取得了一定的地质效果. 采用化极这一计算方法,目的是想消除地磁场倾斜磁化的影响,使化极后的磁异常特征能和磁性体之间建立更直观的联系,简化定量解释工作.但几年来,大量数据处理结果表明,化向磁
INTRODUCTION At present, the processing of aeromagnetic data has been applied to the magnetic pole more generally, and some geological effects have been achieved in some areas. The purpose of this method is to eliminate the dipole magnetization of the geomagnetic field Influence, so that the magnetic anomaly after the pole can establish a more intuitive relationship between the magnetic body and simplify the quantitative interpretation work.But a few years, a large number of data processing results show that the direction of magnetic