Magnetization vector inversion is an useful approach to invert for magnetic anomaly in the
presence of significant remanent magnetization and self-demagnetization. However …

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

Natural remanent magnetization and self-demagnetization on high-susceptibility bodies are
two important factors affecting magnetic data inversion. We propose a framework for the …

摘要本文主要针对当前磁法勘探中高精度处理解释的需求, 对强磁性体Δ 犜异常计算存在的误差
进行分析研究. 我们首先通过理论模型计算试验, 证明常规计算采用的投影关系的Δ …

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 investigate self-demagnetization effects on magnetic data and develop a comparison of
two existing inversion methods as they apply to quantitative interpretation of such data in …

Unstructured grid generation is more suitable for finishing the joint inversion of gravity and
magnetic anomalies in the case of undulating observation surfaces and irregular field …

Self-demagnetization due to strongly magnetic bodies can seriously affect the interpretation
of magnetic anomalies. Conventional numerical methods often neglect the self …

Magnetic susceptibility and natural remanent magnetization of rocks are useful parameters
to study geological structures and geodynamic processes. Traditional widely used …

We have developed a case study on the use of constrained inversion of magnetic data for
recovering ore bodies quantitatively in the Macheng iron deposit, China. The inversion is …