Remanent magnetization and self-demagnetization change the magnitude and direction of
the magnetization vector, which complicates the interpretation of magnetic data. To deal with …

We have developed an approach for the interpretation of magnetic field data that can be
used when measured anomalies are affected by significant remanent magnetization …

We present a new method to estimate the direction of the magnetization vector of geological
bodies based upon the correlation between the reduced‐to‐the‐pole field for tentative …

Remanent magnetization complicates the inversion of magnetic data due to altering the
strength and direction of the magnetization vector. To deal with the problem, we have …

The knowledge of total magnetization (magnitude and direction) makes it easier to interpret
magnetic anomalies. We have developed a simple crosscorrelation-based method to …

强剩磁, 强退磁改变了总磁化强度的大小和方向, 给磁测资料解释带来困难. 为此,
本文利用二维井中磁测数据反演磁化强度矢量的二维分布. 首先利用井中磁测的磁异常模量反演 …

We present a Matlab tool that calculates five magnitude magnetic transforms (MMTs) from an
input measured anomalous magnetic field. The MMTs are all based on the total magnitude …

Locating geologic contacts by mapping lateral magnetization changes provides a variety of
useful geologic information. Magnetic contacts will often correspond to lithologic boundaries …

Significant remanence and demagnetization alter the intensity and orientation of total
magnetization, which complicates interpretation of magnetic data. To deal with the problem …

磁异常转换模量(magnitude magnetic transforms, 简称MMTs) 相比传统的数据处理方法如化极,
总梯度模等, 其产生的异常更接近实际磁性异常体的水平位置, 以便进行磁法解释 …