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Dipole Correlation Method for Determination of Magnetization Directionunder the Influence of Remanent Magnetization

机译:剩磁影响下确定磁化方向的偶极相关法

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Processing and interpretation of magnetic data usually require information of total magnetization direction. However, under the effects of remanant magnetization, total magnetization direction is different from induced magnetization direction, which makes data processing and interpretation complexity. In this paper, we present a new method by cross-correlation of magnetic dipole source for determination of magnetization direction from relatively isolated and approximate equiaxial magnetic total field anomaly. This method calculates cross-correlation coefficient between observed magnetic total field anomaly and theoretical magnetic total field anomaly caused by a magnetic dipole source, by using a set of varying parameters of positions and total magnetization direction of dipole source for trial and error. The corresponding magnetization direction of maximum correlation coefficient is regarded as estimated total magnetization direction. Tests on both synthetic data and aeromagnetic data of a mineral exploration in northwestern China indicate this method reliably and effectively estimates the magnetization direction from relatively isolated and approximate equiaxial magnetic total field anomaly.
机译:磁数据的处理和解释通常需要总磁化方向的信息。然而,在剩余磁化的影响下,总磁化方向与感应磁化方向不同,这使得数据处理和解释变得复杂。在本文中,我们提出了一种通过磁偶极子源的互相关来从相对孤立和近似等轴的磁场总磁场异常确定磁化方向的新方法。该方法通过使用一组变化的位置参数和偶极源的总磁化方向来进行试验和计算,从而计算观察到的磁场全场异常与由磁偶极源引起的理论磁场全场异常之间的互相关系数。最大相关系数的相应磁化方向被视为估计的总磁化方向。对西北地区某矿产勘探的合成数据和航磁数据进行的测试表明,该方法可以根据相对孤立和近似等轴的磁场总场异常可靠而有效地估算出磁化方向。

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