The application of reduction to the pole magnetic anomaly approximation to determining the buried depth of isometric magnetic bodies
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摘要: 化极作为磁异常数据的处理方法在磁异常解释中已广泛应用,利用化极后异常极大值向北偏移的距离估算磁性体的埋深,方法简单,使用便利;对沿走向延伸不长的椭圆状异常,根据化极后异常极大值北移距离,结合实际地质条件确定综合剖面位置,可消除或减小斜磁化的影响,达到不同勘探方法的异常反映同一地质体的目的.Abstract: The reduction to the pole as a magnetic anomaly data processing method has been widely used in the magnetic anomaly explanation.It is simple and convenient to estimate the buried depth of magnetic bodies by using northward moving distance of reduction to the pole magnetic anomaly maximum value.As for the long elliptical magnetic anomalies that extend not very long along the strike,the author determined the position of the comprehensive profile in accordance with northward moving distance of reduction to the pole.The magnetic anomaly maximum and actual geological conditions can eliminate or reduce the influence of oblique magnetization,and can achieve the goals because the anomaly of different exploration methods reflects the same geological body.
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