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利用精密磁测对不同类已知断层的观测表明,可将断层磁异常简化为单极(monopole)磁场模型。而利用断层两侧磁场测值一阶导数波动强弱的比较,则能对断层位置及断层类型(正断层或逆断层)作出明确的判断。
The observation of different types of known faults using precision magnetometry shows that the fault magnetic anomalies can be simplified as the monopole magnetic field model. The use of magnetic field measurements on both sides of the magnetic field measured the first derivative of the strength of the comparison, the fault location and type of fault (normal or reverse fault) to make a clear judgment.