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 …

Efficient and high-precision methods for performing large-scale numerical calculations
under high magnetic susceptibility conditions are essential for magnetic exploration …

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 …

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 …

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

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