Assuming without evidence that magnetic sources are magnetised parallel to the
geomagnetic field can seriously mislead interpretation and can result in drill holes missing …

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 …

The presence of remanent magnetization has hindered the application of generalized 3D
magnetic inversion in exploration geophysics because of the unknown and variable …

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 …

摘要磁化方向的确定对磁异常处理, 反演及解释方面有着重要的参考价值. 然而,
目前常用的磁化方向估计方法易受计算窗口尺度, 化极或叠加异常等影响. 为此 …

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 …

Strong hydrothermal alteration modifies rock physical properties in iron oxide-copper-gold
deposits (IOCGs) and may result in characteristic signatures detectable in geophysical …

Three-dimensional cross-gradient joint inversion of gravity and magnetic data has the
potential to acquire improved density and magnetization distribution information. This …

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